Geometry and Kinematics - IGME

04/09/2015Quaternary Active Faults Database of Iberia v.3 (4/09/2015)

Refer to the Access file for a complete description of the record

ID: AT002 Fault Name: Portimao-Guadalquivir Bank

Segment Name:

Location X: -8.006

Location Y: 36.142

Name of Compiler(s): Álvarez-Gómez, J.A. and García-Mayordomo, J.

Filiation: UCM; IGME

Email: [email protected]

Last Update: 16/04/2015

Average Strike(º): 266 ± 5 LD Lima et al. (2010)

Dip (º): 55 + 15 / - 20 LD Lima et al. (2010)

Rake (º): 90 ± 20 LD Lima et al. (2010)

Sense of Movement: R LD Lima et al. (2010)

Length (km): 100.0 ± 5 LD Lima et al. (2010)

Min Depth (km): 0 + 0.5 LD Lima et al. (2010)

Max Depth (km): 40.0 ± 10 LD Lima et al. (2010)

Width (km): 48.8 AR

Area (km²): 5469.07 AR

Age of the youngestdeposits affected bythe fault:

Quaternary s.l. Pliocene-Quaternary

EJ Based on Zitellini et al. (2004).

Vertical Slip Rate(m/ka or mm/yr) :

0.100 EJ Based on Zitellini et al. (2004). Assuming a displacement of 1000 m (1 s TWT) since Middle Miocene times (Tortonian, 10 ma (Medialdea et al., 2004).

Horizontal Slip Rate(m/ka or mm/yr) :

Unknown

Net Slip Rate(m/ka or mm/yr) :

0.122 AR From rake, dip and VSR

MaxImum Slip Per Event (m):

Unknown

Number of SeismicEvents:

Unknown

Evidence of AseismicCreep:

Unknown

Identification

Geometry and KinematicsVariability Source Comment

Quaternary Activity

Variability Source

Comment

Seismic Potential

Prominent morphologic submarine topography with spatially associated seismicity, offset of recent reflectors.

Zitellini et al. (2004, 2009)

Geological Set: Atlantic Ocean (Offshore Southwest Iberia)

Identification Method: Geophysical methods

Comment

Quaternary activity evidence

B*Strength Class:

Slip Rate *Accuracy Class: C

Paleoearthquakes

Orden Visual: 282

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Maximun Magnitude(Mw):

7.35 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. Estimation following Scholz (2002) relations results in Mw 8.10.

RecurrenceInterval (years) :

5938 5938-79178 AR Preferred estimation considers Mw 7.35 and SR=0.122. Upper bound results from Mw 8.1.

Date of Last MaximumEarthquake (years) :

Unknown

Extended Information: EXTENDED_INFORMATION\AT001-AT003.rar

Lima, J. M. Miranda , M. A. Baptista, J. Catalao, M. Gonzalez, L. Otero, M. Olabarrieta, J. A. Alvarez-Gomez, and E. Carreño (2010): Impact of a 1755-like tsunami in Huelva, Spain. Natural Hazards and Earth System Science, 10: 1-10.

Medialdea, T., Vegas, R., Somoza, L., Vázquez, J. T., Maldonado, A., Dıaz-del-Rıo, V., ... & Fernández-Puga, M. C. (2004). Structure and evolution of the “Olistostrome” complex of the Gibraltar Arc in the Gulf of Cádiz (eastern Central Atlantic): evidence from two long seismic cross-sections. Marine Geology,209(1), 173-198.

Stirling, M., Rhoades, D. and Berryman K. (2002): Comparison of Earthquake Scaling Relations Derived from Data of the Instrumental and Preinstrumental Era. Bulletin of the Seismological Society of America, 92 (2): 812–830.

Zitellini, N., Rovere, M., Terrinha, P., Chierici, F., Matias, L., & Team, B. (2004). Neogene through Quaternary tectonic reactivation of SW Iberian passive margin.Pure and Applied Geophysics, 161(3), 565-587.

Zitellini, N., Gràcia, E., Matias, L., Terrinha, P., Abreu, M. A., DeAlteriis, G., … & Diez, S. (2009). The quest for the Africa–Eurasia plate boundary west of the Strait of Gibraltar. Earth and Planetary Science Letters, 280(1), 13-50.

Source Comment

Associated Seismicity

Extended Data and References

References

Variability

*Reliability rating: C


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ID: AT004 Fault Name: Marques de Pompal

Segment Name:

Location X: -10.203

Location Y: 36.653

Name of Compiler(s): Gràcia, E., Bartolomé, R., Martínez, S. and Lo Iacono, C.

Filiation: Unitat de Tecnologia Marina - CSIC



Average Strike(º): 021 ± 5 LD Measured on multibeam bathymetric data (Vizcaino, 2009; Gràcia et al., 2010).

Dip (º): 24 ± 5 LD Depth conversion of a MCS profile (Zitellini et al., 2001; 2004)

Rake (º): 90 ± 10 EJ Assumed pure reverse

Sense of Movement: R LD Displacement of reflectors on seismic data (Vizcaino, 2009; Gràcia et al., 2010).

Length (km): 47.6 ± 5 LD Measured on multibeam bathymetric data (Vizcaino, 2009; Gràcia et al., 2010).

Min Depth (km): 0 LD Vizcaino, 2009; Gràcia et al., 2010.

Max Depth (km): 50.0 - 10 LD From 40 to 50 km suggested by Geissler et al. (2010); Stich et al. (2010)

Width (km): 122.9 AR

Area (km²): 5851.45 AR


300 - 560 yr BP

LD Age of the last mass transport deposit associated to the fault. We relate it to the 1755 Lisbon Earthquake (Vizcaino, 2009; Gràcia et al., 2010)


Unknown


0 EJ The fault is mainly reverse. In addition, there are no evidences for calculating the horizontal component.

Net Slip Rate(m/ka or mm/yr) : Unknown


Unknown


4 LD We observe a total of 4 successive mass transport deposits associated to this fault (Vizcaino, 2009; Gràcia et al., 2010)


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Surface expression, offset Quaternary horizons, folds, landslides associated

Vizcaino, 2009; Gràcia et al., 2010



Comment


A+*Strength Class:

Slip Rate *Accuracy Class: Not rated

Paleoearthquakes

Orden Visual: 283

Página 3 de 632




7.04 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. The Mw is 7.76 if it is calculated according to Wells & Coppersmith (1994). A value of Mw 8.1 has been proposed by Lima et al. (2010).


2000 LD Based on the average recurrence of successive mass transport deposits associated to the Marques de Pombal Fault (Vizcaino, 2009; Gràcia et al., 2010).


Unknown


García-Orellana, J., Gràcia, E., Vizcaino, A., Masqué, P., Olid, C., Martínez Ruiz, F., Piñero, E., Sánchez-Cabeza, J.A, Dañobeitia, J.J (2006). Identifying instrumental and historical earthquake records in the SW Iberian Margin using 210Pb turbidite chronology. Geophys. Res. Lett., 33 (24), L24601, doi: 10.1029/2006GL028417.

Gràcia, E., Dañobeitia, J.J., Vergés, J., and PARSIFAL Team (2003). Mapping active faults offshore Portugal (38ºN-36ºN): Implications for seismic hazard assessment along the southwest Iberian Margin. Geology, 31, 83-86.

Gràcia, E., Vizcaino, A., Escutia, C., Asioli, A., Rodés, A., Pallàs, R., García Orellana, J., Lebreiro, S., Goldfinger, C (2010). Holocene earthquake record offshore Portugal (SW Iberia): Testing turbidite paleoseismology in a slow-convergence margin. Quaternary Science Reviews, 29, 1156–1172.

Gràcia, E., Bartolomé, R., Lo Iacono, C., Moreno, X., Martínez-Loriente, S., Perea, H., Masana, E., Pallàs, R., Díez, S., Dañobeitia, J.J., Terrinha, P., Zitellini, N. (2010). Characterizing active faults and associated mass transport deposits in the South Iberian Margin (Alboran Sea and Gulf of Cadiz): On-fault and off-fault paleoseismic evidence. En: Contribución de la Geología al Análisis de la Peligrosidad Sísmica (J.M. Insúa y F.Martín-González, eds.), pp. 163-166. IBERFAULT, Sigüenza (Guadalajara), 27-29 Octubre 2010.

V. V. Lima, J. M. Miranda , M. A. Baptista, J. Catalao, M. Gonzalez, L. Otero, M. Olabarrieta, J. A. Alvarez-Gomez, and E. Carreño (2010): Impact of a 1755-like tsunami in Huelva, Spain. Natural Hazards and Earth System Science, 10: 1-10.


Vizcaino, A., Gràcia, E., Pallàs, R., García-Orellana, J., Escutia, C., CASAS, D., WILLMOTT, V., Díez, S., AND Dañobeitia, J.J. (2006). Sedimentology, physical properties and ages of mass-transport deposits associated to the Marquês de Pombal Fault, Southwest Portuguese Margin. Norwegian Journal of Geology, 86, 173-182.

Vizcaino, A., 2009. “Processos sedimentaris d’edat Holocena al marge sud-oest de la Península Ibèrica: Aplicació a la paleosismologia marina”. Tesis Doctoral, Universitat de Barcelona, 281 pp.

Wells, D. L., and Coppersmith, K. J. (1994). New empirical relationships among magnitude, rupture length, rupture width, and surface displacement. Bulleting of the Seismological Society of America 84, 974-1002.

Geissler et al., 2010. Focal mechanisms for sub-crustal earthquakes in the Gulf of Cadiz from a dense OBS deployment. Geophys. Res. Lett., 37, L18309.

Stich, D., Mancilla, F., Morales, J., 2005. Crust-mantle coupling in the Gulf of Cadiz (SW Iberia). Geophys. Res. Lett., 32, L13306, doi:10.1029/2005GL023098.

Stich et al., 2010. Moment tensor inversion for Iberia-Maghreb earthquakes 2005-2008. Tectonophysics, 483, 390-398.

Zitellini, N., Mendes, L., Córdoba, D., Dañobeitia, J.J., Nicolich, R., Pellis, G., Ribeiro, A., Sartori, R., Torelli, L., and BIGSETS TEAM

Seismic PotentialSource Comment



References

Variability

*Reliability rating: A

*Reliability rating: Not rated

Database of Seismicity Associated to QAFI v.3 FaultsRefer to the Access file for a complete description of the record

ID_Event Event name Date Location XY Int./Mag. Source Association Comment

AT004

1755 Lisbon earthquake

1/11/1755 Mw>8 Lisbon event either associated to Horseshoe or Marques de Pombal faults (Gràcia et al., 2003; Zitellini et al., 2004).

730

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(2001). Source of the 1755 Lisbon Earthquake and Tsunami Investigated. EOS, Transactions of AGU, Vol 82 (26), p. 285-290-291.

Zitellini, N., Rovere, M., Terrinha, P., Chierici, F., Matias, L., and BIGSETS Team, 2004. Neogene through Quaternary tectonic reactivation of SW Iberian Passive Margin. Pure Appl. Geophys., 161, 565-587.

Página 5 de 632



ID: AT005 Fault Name: Horseshoe

Segment Name:

Location X: -10.477

Location Y: 35.803

Name of Compiler(s): Gràcia, E., Bartolomé, R., Martínez, S. and Lo Iacono, C.




Average Strike(º): 045 ± 5 LD Measured on multibeam bathymetric data (Gràcia et al., 2003, 2010).

Dip (º): 30 ± 10 LD Calculated from the SWIM-2006 MCS profiles, where we have performed pre-stack depth migration, so the profiles are in depth-section, not TWTT (Gràcia et al., 2003, 2010).

Rake (º): 90 ± 10 EJ Assumed pure reverse

Sense of Movement: R LD Displacement of reflectors on seismic data (Gràcia et al., 2003, 2010)

Length (km): 87.0 ± 5 LD Measured on multibeam bathymetric data (Gràcia et al., 2003, 2010)

Min Depth (km): 0 LD Gràcia et al., 2003, 2010.

Max Depth (km): 60.0 - 20 LD From 40 to 60 km suggested by Stich et al. (2007); Geissler et al. (2010); Stich et al. (2010)

Width (km): 120.0 AR

Area (km²): 10440.00 AR


Holocene LD The fault reaches up to the surface, as demonstrated by MCS and TOPAS profiles. The age of the seafloor sediments is of Holocene age based on sediment cores (Gràcia et al., 2003, 2010).


0.180 ± 0.01 LD Calculated from vertical displacement of seismic horizons in the depth-section profile (Gràcia et al., 2003, 2010). This is a long-range rate since the base of the Quaternary.


0 EJ The fault is mainly reverse. In addition, there are no evidences for calculating the horizontal component.


0.36 ± 0.01 AR Relationship between VSR, dip and rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Surface expression, offset Quaternary horizons, folds, landslides associated

Gràcia et al., 2003, 2010.



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 284

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7.29 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. The Mw is 8.01 if it is calculated according to Wells & Coppersmith (1994). A value of Mw 8.3 has been proposed by Lima et al. (2010).


864 234-3191 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): slip rate represents the rate at which maximum earthquakes are released by the fault. RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown


Gràcia, E., Dañobeitia, J.J., Vergés, J., and PARSIFAL Team (2003). Mapping active faults offshore Portugal (38ºN-36ºN): Implications for seismic hazard assessment along the southwest Iberian Margin. Geology, 31, 83-86.

Gràcia, E., Vizcaino, A., Escutia, C., Asioli, A., Rodés, A., Pallàs, R., García Orellana, J., Lebreiro, S., Goldfinger, C (2010). Holocene earthquake record offshore Portugal (SW Iberia): Testing turbidite paleoseismology in a slow-convergence margin. Quaternary Science Reviews, 29, 1156–1172.


V. V. Lima, J. M. Miranda , M. A. Baptista, J. Catalao, M. Gonzalez, L. Otero, M. Olabarrieta, J. A. Alvarez-Gomez, and E. Carreño (2010): Impact of a 1755-like tsunami in Huelva, Spain. Natural Hazards and Earth System Science, 10: 1-10.


Geissler et al., 2010. Focal mechanisms for sub-crustal earthquakes in the Gulf of Cadiz from a dense OBS deployment. Geophys. Res. Lett., 37, L18309.

Stich, D., Mancilla, F., Morales, J., 2005. Crust-mantle coupling in the Gulf of Cadiz (SW Iberia). Geophys. Res. Lett., 32, L13306, doi:10.1029/2005GL023098.




References

Variability





AT005

2007 Horseshoe event

12/02/2007 Mw=6.0 Stich et al., 2007

Stich et al., 2007728

AT005

1755 Lisbon earthquake

1/11/1755 Mw>8 Lisbon event either associated to Horseshoe or Marques de Pombal faults (Gràcia et al., 2003; Zitellini et al., 2004).

729

AT005

1969 Horseshoe earthquake

Mw=8.0 Gràcia et al. (2010)731

Página 7 de 632



Stich et al., 2007. Source analysis of the February 12th 2007, Mw 6.0 Horseshoe earthquake: Implications for the 1755 Lisbon earthquake. Geophys. Res. Lett., Vol 34, L12308.

Stich et al., 2010. Moment tensor inversion for Iberia-Maghreb earthquakes 2005-2008. Tectonophysics, 483, 390-398.


Wesnousky, S.G. (1986). Earthquakes, Quaternary faults, and seismic hazard in California. Journal of Geophysical Research. 91(B12), 12587-12631.

Zitellini, N., Rovere, M., Terrinha, P., Chierici, F., Matias, L. & BIGSETS TEAM (2004). Neogene through Quaternary tectonic reactivation of SW Iberian passive margin. Pure Appl. Geophys., 161, 565-587.

Página 8 de 632



ID: AT006 Fault Name: Coral Patch Ridge (1/2)

Segment Name: Western

Location X: -11.318

Location Y: 35.398

Name of Compiler(s): Gràcia, E., Martínez, S. and Bartolomé, R.




Average Strike(º): 085 ± 5 LD Measured on multibeam bathymetric data (Martínez-Loriente, 2008; Martínez-Loriente et al. 2009)

Dip (º): 90 LD Martínez-Loriente, 2008; Martínez-Loriente et al. 2009.

Rake (º): 90 EJ Assumed pure reverse

Sense of Movement: R LD Martínez-Loriente, 2008; Martínez-Loriente et al. 2009.

Length (km): 53.0 ± 5 LD Measured on multibeam bathymetric data (Martínez-Loriente, 2008; Martínez-Loriente et al. 2009).

Min Depth (km): Unknown

Max Depth (km): Unknown

Width (km): Unknown

Area (km²): Unknown


Holocene LD The fault reaches up to the surface, as demostrated by MCS and TOPAS profiles. Martínez-Loriente et al. (2009).


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Surface expression, offset Quaternary horizons Martínez-Loriente, 2008; Martínez-Loriente et al., 2009.



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 285

Página 9 de 632




7.09 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. The Mw is 7.08 if it is calculated according to Wells & Coppersmith (1994).


Not enough data for an estimation


Unknown



Martínez-Loriente, S., 2008. “Estratigrafia i estructura de la part externa del Golf de Cadis basades en dades de sísmica de reflexió multicanal migrades en profunditat pre-stack”. DEA Universitat de Barcelona.

Martínez-Loriente, S., Gràcia, E., Bartolomé, R., Sallarès, V., Terrinha, P. (2009). Active tectonics at the external part of the Gulf of Cadiz based on depth and time migrated MCS profiles. 6º Simposio sobre el Margen Ibérico Atlántico (MIA-09), Oviedo (Spain), 1-5 December 2009.

Martínez-Loriente, S., Sallarès, V., Bartolomé, R., Gràcia, E., NEAREST-SEIS CRUISE PARTY, 2009. Wide-angle reflection and refraction seismic profile from the outer part of the Gulf of Cadiz: NEAREST-SEIS cruise. Instrumentation Viewpoint, 8, 49, ISSN:1697-2562.



Source Comment



References

Variability



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ID: AT007 Fault Name: Coral Patch Ridge (2/2)

Segment Name: Eastern

Location X: -10.743

Location Y: 35.415

Name of Compiler(s): Gràcia, E., Martínez, S. and Bartolomé, R.




Average Strike(º): 056 ± 5 LD Measured on multibeam bathymetric data (Martínez-Loriente, 2008; Martínez-Loriente et al. 2009)

Dip (º): 90 LD Martínez-Loriente, 2008; Martínez-Loriente et al. 2009.


Sense of Movement: R LD Martínez-Loriente, 2008; Martínez-Loriente et al. 2009.

Length (km): 54.0 ± 5 LD Measured on multibeam bathymetric data



Width (km): Unknown



Holocene LD The fault reaches up to the surface, as demostrated by MCS and TOPAS profiles. Martínez-Loriente et al. (2009).


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Surface expression, offset Quaternary horizons Martínez-Loriente, 2008; Martínez-Loriente et al., 2009.



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 286

Página 11 de 632








Unknown





Martínez-Loriente, S., Sallarès, V., Bartolomé, R., Gràcia, E., NEAREST-SEIS CRUISE PARTY, 2009. Wide-angle reflection and refraction seismic profile from the outer part of the Gulf of Cadiz: NEAREST-SEIS cruise. Instrumentation Viewpoint, 8, 49, ISSN:1697-2562.



Source Comment



References

Variability



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ID: AT008 Fault Name: Lineament N

Segment Name:

Location X: -9.456

Location Y: 35.962

Name of Compiler(s): Gràcia, E., Bartolomé, R. and Martínez, S.




Average Strike(º): 100 ± 2 LD Measured on multibeam bathymetric data (Zitellini et al., 2009).

Dip (º): 90 ± 10 LD Calculated from the SWIM-2006 MCS profiles, where we have performed pre-stack depth migration, so the profiles are in depth-section, not TWTT (Zitellini et al., 2009).

Rake (º): 180 ± 10 EJ Assumed pure dextral strike-slip

Sense of Movement: D LD Zitellini et al., 2009.

Length (km): 130.0 ± 5 LD Measured on multibeam bathymetric data (Zitellini et al., 2009).



Width (km): Unknown



Holocene LD Zitellini et al., 2009.


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Surface expression, flower structures, offset quaternary horizons Zitellini et al., 2009.



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 287

Página 13 de 632








Unknown



Bartolomé, R., Gràcia, E., Stich, D., MARTÍNEZ–LORIENTE, S., Klaeschen, D., Masana, E., Díez, S., Lo Iacono, C., Moreno, X., Zitellini, N., Mànuel, A., Dañobeitia, J.J. (2009). Seismic evidence of active strike-slip faulting in the external Gulf of Cadiz (SW Iberian Margin). EOS Trans AGU, Fall meeting Suppl., San Francisco (USA), 14-18 Dec. 2009.





Zitellini, N., Gràcia, E., MATIAS, L., Terrinha, P., ABREU, M.A., DE ALTERIIS, G., HENRIET, J.P., Dañobeitia, J.J., MASSON, D.G., MULDER, T., RAMELLA, R., SOMOZA, L., Díez, S. (2009). The Quest for the Africa-Eurasia plate boundary west of the Strait of Gibraltar. Earth Planet Sci. Lett., 280, 13-50.

Source Comment



References

Variability



Página 14 de 632



ID: AT009 Fault Name: Lineament S

Segment Name:

Location X: -10.858

Location Y: 35.866

Name of Compiler(s): Gràcia, E., Bartolomé, R.and Martínez, S.




Average Strike(º): 105 ± 2 LD Measured on multibeam bathymetric data (Zitellini et al., 2009).

Dip (º): 90 ± 10 LD Calculated from the SWIM-2006 MCS profiles, where we have performed pre-stack depth migration, so the profiles are in depth-section, not TWTT (Zitellini et al., 2009).

Rake (º): 180 ± 10 EJ Assumed pure dextral strike-slip

Sense of Movement: D LD Evidenced by earthquake focal mechanisms (Stich et al., 2010)

Length (km): 170.0 ± 5 LD Measured on multibeam bathymetric data (Zitellini et al., 2009).

Min Depth (km): 0 LD Zitellini et al., 2009.

Max Depth (km): 55.0 LD Lower depth of the instrumental seismicity according to recent earthquake focal mechanisms along this fault (Geissler et al., 2010; Stich et al., 2010)

Width (km): 55.0 AR

Area (km²): 9350.00 AR


Holocene LD The fault reaches up to the surface, as demonstrated by MCS and TOPAS profiles (Zitellini et al., 2009).


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Surface expression, flower structures, offset quaternary horizons Zitellini et al., 2009.



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 288

Página 15 de 632








Unknown


Bartolomé, R., Gràcia, E., Stich, D., Martínez-Loriente, S., Klaeschen, D., Masana, E., Díez, S., Lo Iacono, C., Moreno, X., Zitellini, N., Mànuel, A., Dañobeitia, J.J. (2009). Seismic evidence of active strike-slip faulting in the external Gulf of Cadiz (SW Iberian Margin). EOS Trans AGU, Fall meeting Suppl., San Francisco (USA), 14-18 Dec. 2009.

Geissler et al., 2010. Focal mechanisms from sub-crustal earthquakes in the Gulf of Cadiz from a dense OBS deployment. Geohys. Res. Lett., 37, L18309.




Stich et al., 2010. Moment tension inversion for Iberia-Maghreb earthquakes 2005-2008. Tectonophysics, 483, 390-398.



Zitellini, N., Gràcia, E., MATIAS, L., Terrinha, P., ABREU, M.A., DE ALTERIIS, G., HENRIET, J.P., Dañobeitia, J.J., MASSON, D.G., MULDER, T., RAMELLA, R., SOMOZA, L., Díez, S. (2009). The Quest for the Africa-Eurasia plate boundary west of the Strait of Gibraltar. Earth Planet Sci. Lett., 280, 13-50.




References

Variability



Página 16 de 632



ID: ES001 Fault Name: North Maladeta Fault (1/2)

Segment Name: Western-Central

Location X: 0.6759

Location Y: 42.6645

Name of Compiler(s): Ortuño Candela, M.

Filiation: Universidad Nacional Autónoma de México-UNAM



Average Strike(º): 100 ± 5 LD Observed in the field (fault trace) and obtained by using the Boxer (Gasperini et al., 1999) for the central part (Ortuño,2008).

Dip (º): 80 ± 10 LD 80º to the N. Observed in the field and in the audiomagnetotelluric surveys (Ortuño et al., 2008) performed in the other segment (Ortuño,2008).

Rake (º): -90 LD Only based in geomorphologic observations. The fault could have some lateral component that is not reflected in the present day geomorphology of the area (Ortuño,2008).

Sense of Movement: N LD Ortuño,2008.

Length (km): 13.5 LD Surface length. Length at depth: 9,2 km from the macroseismic analysis made by Ortuño et al. (2008).

Min Depth (km): 0 - 1.55 LD There is a fault trace in the surface. However, the 1923 earthquake did not rupture the surface, and has a minimum estimated depth of 1.55 km as derived from the Boxer (Gasperini et al., 1999) analysis of

Max Depth (km): 10.0 + 2 / - 1.15 ER Maximum value (12 km) comes from the seismogenic depth inferred to the area by Souriau and Pauchet (1998) by analyzing the instrumental seismicity. Minimum value (8,45 km) comes from the

Width (km): 10.2 AR

Area (km²): 137.08 AR


Last glacial maximum

LD Not deposits but erosive surfaces of probable Last Glacial Maximum age (see Ortuño, 2008 for explanation; Rodés, 2008 for exposure ages).


0.090 0.04 - 0.09 EJ We can assume a similar value that the one determined for the easternmost segment


Unknown


0.07 0.04 - 0.09 EJ Unknown. The scarps interpreted as parts of the fault trace have a clear erosive or/and gravitational component, so that the neotectonic component cannot be measured (see Ortuño, 2008 for explanation).


0.66 0.27 - 0.44 ER Using Wells and Coppersmith (1994) relationships and Mw= 5.8 assigned to the 1923 Vielha earthquake

Identification


Quaternary Activity

Variability Source

Comment

Any clear direct evidence of Quaternary activity. Some features of composite origin (erosive, topographic and tectonic) have been considered to define the fault trace.

Some well preserved triangular facets in the glaciated slopes of the Nere valley and the Conangles valley could correspond to the fault plane exposure or to a different fault plane with a gravitational (topographic) component (Ortuño,2008).

Geological Set: Pyrenees (Lleida)

Identification Method: Geological/Geomorphological field mapping

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 11

Página 17 de 632




1 19th November 1923


OD No


6.52 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset.


23798 5157-149476 AR Considering the Maximum Earthquake Model (Wesnousky, 1986). It can also be 30,8 - 69,4 ka using the Brune (1968) relationships, Stirling et al. (2002) SRL derived magnitudes and the SR inferred for the other segment (Ortuño, 2008).


1923 LD Historic earthquake, see Susagna et al. (1994) and Ortuño et al. (2008).

Extended Information: EXTENDED_INFORMATION\ES001-ES002.rar

Brune, J.N., 1968. Seismic moment, seismicity, and rate of slip along major fault zones. Journal of Geophysical Research 73, 777-784.

Ortuño, M. (2008). Deformación activa en el Pirineo Central: la falla Norte de la Maladeta y otras fallas activas. Tesis doctoral, Univ. De Barcelona, 346 pp.

Ortuño, M., Queralt, P., Martí, A., Ledo, J., Masana, E., Perea, H. & Santanach, P. (2008). The North Maladeta fault (Spanish Central Pyrenees) as the Vielha 1923 earthquakeseismic source: recent activity revealed by geomorphological and geophysical research. Tectonophysics (453), 246-262.

Ortuño and Perea, (2010). El terremoto de Vielha de 1923 (Pirineos Centrales): fuente sismogenética, variación del esfuerzo de Coulomb y distribución de la sismicidad posterior .In: Contribución de la Geología al Análisis de la Peligrosidad Sísmica (J.M. Insua y F. Martín‐González, eds.), pp.15‐18. Sigüenza (Guadalajara, Spain).

Rodés, A. (2008). La última deglaciación en los Pirineos: datación de superficies de exposición mediante 10Be, y modelado numérico de paleoglaciares. Tesis doctoral, Universitat de Barcelona. 238 pp.


Susagna, T., Roca, A., Goula, X. & Batlló, J. (1994). Analysis of Macroseismic and Instrumental Data for the Study of the 19 November 1923 Earthquake in the Aran Valley (Central Pyrenees). Natural Hazards, 10, 7-17.

Wells, D.L. y Coppersmith, K.J., 1994; Empirical relationships among magnitude, rupture length, rupture area, and surface displacement. Bull. Seismol. Soc. Am., 82, 974-1002.





References

Variability

*Reliability rating: D




ES001

Vielha earthquake 19th of November

1923

(0.7, 42.67) Imax = VIII; ML = 5.6

Susagna et al. (1994)

isoseist analysis and spacial correlation

5 km hipocenter, Susagna et al. (1994), Ortuño et al (2008) for seismogenesis. The epicentre obtained using the Gasperini et al. (1999) method slightly differs from this: (42.7 N, 0.778 E); having an associated Mw (from source dimensions) = 5,77

595

Página 18 de 632



ID: ES002 Fault Name: North Maladeta fault (2/2)


Location X: 0.836

Location Y: 42.668





Average Strike(º): 100 ± 5 LD Observed in the field (fault trace) (Ortuño,2008).

Dip (º): 80 ± 5 LD 80º to the N. Observed in the field and in the audiomagnetotelluric surveys (Ortuño et al., 2008)

Rake (º): -90 ± 5 LD Only based in geomorphologic observations. The fault could have some lateral component that is not reflected in the present day geomorphology of the area (Ortuño,2008).


Length (km): 14.3 ± 0.010 LD Ortuño,2008.

Min Depth (km): 0 EJ Inferred from the surface displacement

Max Depth (km): 12.0 LD Maximum value (12 km) comes from the seismogenic depth inferred to the area by Souriau and Pauchet (1998) by analyzing the instrumental seismicity (Ortuño,2008).

Width (km): 12.2 AR

Area (km²): 149.43 AR


Late Neogene LD The Prüedo lacustrine deposits (Late Miocene, most probably vallesian age: 11.1 - 8. 7 Ma) were formed in a tectonic basin generated by the activity of this fault (Ortuño,2008).


0.090 0.04 - 0.09 LD Triangular facets, erosion surfaces displaced and dated by lacustrine deposits on top (489 m/11.1 - 8,7 Ma)((Ortuño,2008)). The maximum value is preferred because it is more conservative.


Unknown


0.07 0.04 - 0.09 EJ Unknown, the fault could have some lateral component that is not reflected in the present day geomorphology of the area. No free surface have been observed.


0.463 +0.145/-0.111 ER Using Wells and Coppersmith (1994) and a Mw = 6.2, estimated for the Ribagorça (1373) earthquake, possibly generated by this fault segment (among other possible sources).


1 LD The Ribagorça (1373) earthquake, possibly generated by this fault segment (among other possible sources) (Ortuño,2008).

Identification


Quaternary Activity

Variability Source

Comment

Any clear direct evidence of Quaternary activity. Some features of composite origin (erosive, topographic and tectonic) have been considered to define the fault trace.

Ortuño (2008).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 12

Página 19 de 632




Unknown


6.55 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. The Mw is 6.30 using Wells and Coppersmith (1994) and a surface length of 12.263 km


Unknown, although a rough estimate using the Brune (1968) relationships and indirect data leads to values between (35,2 - 79,2) ka, using Stirling et al. (2002) SRL derived magnitudes and the slip rate inferred for the other segment (Ortuño, 2008).


1373 Historic earthquake (Olivera et al., 2006) that might be produced by this fault (Ortuño, 2008)


Brune, J.N., 1968. Seismic moment, seismicity, and rate of slip along major fault zones. Journal of Geophysical Research 73, 777-784.

Olivera, C., Redondo, E., Lambert, J., Riera Melis, A. y Roca, A., 2006. Els terratrèmols dels segles XIV i XV a Catalunya. Institut Cartogràfic de Catalunya, Monografies nº30,407 pp.

Ortuño, M. (2008). Deformación activa en el Pirineo Central: la falla Norte de la Maladeta y otras fallas activas. Tesis doctoral, Univ. De Barcelona, 346 pp.

Ortuño, M., Queralt, P., Martí, A., Ledo, J., Masana, E., Perea, H. & Santanach, P. (2008). The North Maladeta fault (Spanish Central Pyrenees) as the Vielha 1923 earthquakeseismic source: recent activity revealed by geomorphological and geophysical research. Tectonophysics (453), 246-262.






References

Variability





ES002

The Ribagorça earthquake

3th March 1373

(0.683 , 42,633)

Imax = VIII - IX; M = 6.2

Olivera et al. (2006)

epicentral area and spacial correlation

This segment of the North Maladeta fault is among the possible seismic sources of this event. Other possible sources are the Coronas fault and faults in the Rius-Cabanes fault system (see Ortuño, 2008 for further information)

596

Página 20 de 632



ID: ES003 Fault Name: Coronas

Segment Name:

Location X: 0.60394462

Location Y: 42.66733179





Average Strike(º): 140 ± 5 LD Ortuño, 2008

Dip (º): 80 ± 10 LD 80º to the N. Geologic data (Ortuño,2008).

Rake (º): -80 ± 5 LD A left-lateral minor component is inferred from the analysis of the geodynamical features observed in other associated secondary faults (Ortuño, 2008).


Length (km): 10.2 LD Ortuño,2008.

Min Depth (km): 0 LD Inferred from the displacement of the surface (Ortuño,2008).

Max Depth (km): 12.0 LD Maximum value (12 km) comes from the seismogenic depth inferred to the area by Souriau and Pauchet (1998) by analyzing the instrumental seismicity (Ortuño,2008).

Width (km): 12.2 AR

Area (km²): 124.65 AR


20 ky ± 3 ky EJ Last Glacial Maximum (see Ortuño,2008).


0.090 0.04 to 0.09 LD Estimation from proximity and similarities to North Maladeta Fault. 1.2 m/ka is a overestimation considering the maximum offset (150m) accumulated since 125 ka ago, although it could be longer ago. Part of this slip is expected to be gravitational.


0.016 0.007 to 0.016 AR Relationship between NSR and rake


0.093 0.041 to 0.093 AR Relationship between VSR, dip and rake


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Offset of glacial erosion surfaces at the Ballibierna valley (Huesca)

This fault has probably displaced the northern slope of the Ballibierna valley (Huesca) by some meters. The present day offset (almost 200 m at some parts) seem to have a gravitational component. See Ortuño (2008) for further information.

Geological Set: Pyrenees (Huesca-Lleida)


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 13

Página 21 de 632




LD There are several evidences of aseismic creep. This creep, however, is not tectonic by due to a topographic instability. The Aneto massif seems to be collapsing towards the north along part of a tectonic fault. See Ortuño (2008) for further information.


6.41 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. The Mw is 6.3 using Wells and Coppersmith (1994) and a surface length of 10.23 km




1373 LD Historic earthquake (Olivera et al., 2006) that might be produced by this fault (Ortuño, 2008)

Extended Information: EXTENDED_INFORMATION\ES003.rar

Olivera, C., Redondo, E., Lambert, J., Riera Melis, A. y Roca, A., 2006. Els terratrèmols dels segles XIV i XV a Catalunya. Institut Cartogràfic de Catalunya, Monografies nº30, 407 pp.

Ortuño, M. (2008). Deformación activa en el Pirineo Central: la falla Norte de la Maladeta y otras fallas activas. Tesis doctoral, Univ. de Barcelona, 346 pp.







References

Variability





ES003


3th March 1373

(0.683 , 42,633)



epicentral area and spacial correlation

This fault is among the possible seismic sources of this event. Other possible sources are the North Maladeta fault and faults in the Rius-Cabanes fault system (see Ortuño, 2008 for further information).

597

Página 22 de 632



ID: ES004 Fault Name: Sud de la Tet-Cerdanya

Segment Name:

Location X: 2.5879

Location Y: 42.6475

Name of Compiler(s): Perea, H. and García-Mayordomo, J.

Filiation: ICM-CSIC and IGME



Average Strike(º): 243 LD Briais et al. (1990); Carozza and Baize (2004). Strike changes from north being 236 until (2.368, 42.533), 259 until (2.174, 42.505), 236 until (1.852, 42.341), 270 until (1.684, 42.341).

Dip (º): 60 ± 10 LD Roca (1992 and 1996); Roca and Guimerà (1992)

Rake (º): -90 ± 10 LD Roca (1992 and 1996); Roca and Guimerà (1992)

Sense of Movement: N LD Roca (1992 and 1996); Roca and Guimerà (1992)

Length (km): 80.0 ± 5 LD Briais et al. (1990); Carozza and Baize (2004)

Min Depth (km): 1.5 ± 1 EJ

Max Depth (km): 15.0 ± 5 LD Roca and Guimerà (1992); Sàbat et al. (1997). The maximum depth is also established by expert judgement (EJ) from the analysis of the earthquake focal depth (Perea, 2006 and 2009; Perea et al.,2006)

Width (km): 15.6 AR

Area (km²): 1247.08 AR


Unknown


0.070 0.070-0.300 LD Miocene surface displaced: 3000m and 1700m/10Ma and 15Ma (Briais et al.,1990); 1000m/10Ma and 15Ma (Carozza and Baize,2004; Perea, 2006).


0 EJ HSR=0, assumed pure dip-slip faulting.


0.081 0.081-0.346 AR Relationship between VSR, dip and rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Triangular facets, wine glass basin shape, low space index. Briais et al. (1990); Carozza and Baize (2004); Perea (2006)

Geological Set: Pyrenees (Francia-Girona-Lleida)


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 14

Página 23 de 632




7.26 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. The Mw is 7.40 calculated using Wells and Coppersmith (1994) surface rupture length relationship for normal faults (Perea, 2006; Perea et al., 2006).


28538 102431-1861 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Perea (2006) obtained 54000 yrs considering Mw 7.40 from W&C'94 and 0.07 m/ka. The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown


Briais, A., Armijo, R., Winter, T., Tapponnier, P., Herbecq, A. (1990): Morphological evidence for Quaternary normal faulting and seismic hazard in the Eastern Pyrenees. Annales Tectonicae, 4(1), 19-42.

Carozza, J.-M., Baize, S. (2004): L'escarpement de la Têt est-il le résultat de la tectonique active Plio-Pléistocène? C.R.Geoscience, 336, 217-226.

Perea, H. (2006): Falles actives i perillositat sísmica al marge nord-occidental del solc de València, PhD Thesis Universitat de Barcelona, Barcelona, 382 pp.

Perea, H. (2009): The Catalan seismic crisis (1427 and 1428; NE Iberian Peninsula): Geological sources and earthquake triggering. Journal of Geodynamics, 47, 259-270.

Perea, H., Masana, E., Santanach, P. (2006): A pragmatic approach to seismic parameters in a region with low seismicity: The case of eastern Iberia. Natural Hazards, 39(3): 451-477.

Roca, E. (1992): L'estructura de la Conca Catalano-Balear: paper de la compressió i de la distensió en la seva gènesi. PhD thesis, Universitat de Barcelona, pp. 330.

Roca, E. (1996): La evolución geodinámica de la Cuenca Catalano-Balear y áreas adyacentes desde el Mesozoico hasta la actualidad. Acta Geol. Hispanica 29(1994), 3-26.

Roca, E., Guimerà, J. (1992): The Neogene structure of the eastern Iberian margin: structural constrains on the crustal evolution of the València trough (western Mediterranean). Tectonophysics 203, 203-218.

Sàbat, F., Roca, E., Muñoz, J.A., Vergés, J., Sans, M., Masana, E., Santanach, P. Estévez, A., Santisteban, C. (1997): Role of extension and compression in the evolution of the eastern margin of Iberia: the ESCI-València Trough seismic profile. Rev. Soc. Geol. España 8 (1995), 431-448.

Simón, J.L. (1984): Compresión y distensión alpinas en la Cadena Ibérica oriental. Instituto de Estudios Turolenses-CSIC, pp. 172.


Wells, D.L., Coppersmith, K.J. (1994): New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bulletin of the Seismological Society of America 84 (4), 974–1002.

Wesnousky, S. G. (1986): Earthquakes, quaternary faults and seismic hazard in California. J. Geophys. Res. 91(B12), 12587–12631.




References

Variability



Página 24 de 632



ID: ES005 Fault Name: Amer (complete)

Segment Name:

Location X: 2.608

Location Y: 41.991

Name of Compiler(s): Perea, H.

Filiation: ICM-CSIC



Average Strike(º): 321 LD Saula et al. (1996); Ferrer et al. (1999). The strike of the fault is given following the direction that connects its tips. Note that the fault changes its direction at its middle point.

Dip (º): 60 ± 10 LD Saula et al. (1996)

Rake (º): -90 ± 10 LD Saula et al. (1996)

Sense of Movement: N LD Saula et al. (1996)

Length (km): 35.4 ± 0.5 LD Ferrer et al. (1999); Perea (2006); Perea et al. (2006)


Max Depth (km): 15.0 ± 5 LD The maximum depth is also established by expert judgement (EJ) from the analysis of the earthquake focal depth (Perea, 2006 and 2009; Perea et al.,2006)

Width (km): 15.6 AR

Area (km²): 551.83 AR


Unknown


0.055 0.045-0.138 LD Triangular facets and alluvial fan surface: 275m/5Ma and 2Ma (Ferrer et al., 1999; Perea, 2006; Perea et al., 2006)






Unknown


2 in last 573 yr

2-3 LD Fault responsible of at least 2, but probable, of the 3 earthquakes of the Catalan Seismic Crisis between 1427-1428 (Goula et al., 1992; Ferrer et al, 1999; Fleta et al., 2001; Perea, 2006; Perea et al., 2006; Perea, 2009)

Identification


Quaternary Activity

Variability Source

Comment

Triangular facets, wine glass basin shape, low space index Ferrer et al. (1999); Perea (2006); Perea et al. (2010)

Geological Set: Pyrenees (Girona)


Comment


C+*Strength Class:


Paleoearthquakes

Orden Visual: 15

Página 25 de 632




Unknown






573 LD Source of the Catalan Seismic Crisis 1427-1428 (Fontserè and Iglésies, 1971; Cadiot, 1979; Goula et al, 1992; Olivera et al, 1992; Lambert, 1993; Ferrer et al, 1999; Fleta et al, 2001; Olivera et al, 2006; Perea, 2006; Perea et al, 2006; Perea, 2009)


Cadiot, B. (1979): Les effets en France du séisme Catalan de 1428. In: J. Vogt (Editor), Les tremblements de terre en France. BRGM, Orleans, pp. 166-172.

Ferrer, P., Masana, E., Santanach, P. (1999): Expresión geomorfológica de la actividad reciente de la falla de Amer (NE de la Península Ibérica). Acta Geol.Hispanica, 31(1996): 17-24.

Fleta, J., Santanach, P., Goula, X., Martínez, P., Grellet, B., Masana, E. (2001): Preliminary geologic, geomorphologic and geophysical studies for the paleoseismological analysis of the Amer fault (NE Spain). Netherlands Journal of Geosciences / Geologie en Mijnbouw, 80(3-4): 243-253.

Fontserè, E., Iglésies, J. (1971): Recopilació de dades sísmiques de les terres catalanes entre 1100 i 1906. Fundació Salvador Vives Casajuana, Barcelona, 548 pp.

Goula, X., Olivera, C., Escuer, J., Fleta, J., Grellet, B., Bousquet, J.C. (1992): Neotectonics and seismicity of the area of the seismic crisis of 1427-28 in Catalonia. Proceedings of the 22nd General Assembly of the European Seismological Comission, Barcelona: 333-338.




References

Variability





ES005

Amer earthquake 19/03/1427 2.5833, 41.9833

IEMS98 = VIII / Mw = 5.9

ICC Spatial correlation and macroseismic data

analysis

1st event of the Catalan Seismic Crisis 1427-1428 (Fontserè and Iglésies, 1972; Cadiot, 1979; Goula et al, 1992; Olivera et al, 1992; Lambert, 1993; Ferrer et al, 1999; Fleta et al, 2001; Olivera et al, 2006; Perea, 2006; Perea et al, 2006; Perea, 2009)

598

ES005

Olot earthquake 15/05/1427 2.4333, 41.1667



analysis

2nd event of the Catalan Seismic Crisis 1427-1428 (Fontserè and Iglésies, 1972; Cadiot, 1979; Goula et al, 1992; Olivera et al, 1992; Lambert, 1993; Ferrer et al, 1999; Fleta et al, 2001; Olivera et al, 2006; Perea, 2006; Perea et al, 2006; Perea, 2009)

599

ES005

Camprodon earthquake

02/02/1428 2.3333, 42.3000


ICC Macroseismic data and Coulomb stress

analyses

3rd event of the Catalan Seismic Crisis 1427-1428 (Fontserè and Iglésies, 1972; Cadiot, 1979; Goula et al, 1992; Olivera et al, 1992; Lambert, 1993; Ferrer et al, 1999; Fleta et al, 2001; Olivera et al, 2006; Perea, 2006; Perea et al, 2006; Perea, 2009)

600

Página 26 de 632



Lambert, J. (1993): The Catalonian (1428) and Alpine (1564, 1644) earthquakes: review of research in France. In: M. Stucchi (Editor), Historical investigation of european earthquakes. CNR, Milano, pp. 145-159.

Olivera, C., Redondo, E., Lambert, J., Riera Melis, A., Roca, A. (2006): Els terratrèmols dels segles XIV i XV a Catalunya. Monografies nº 30. Institur Cartogràfic de Catalunya, Barcelona, 407 pp.

Olivera, C., Susagna, T., Roca, A., Goula, X. (1992): Seismicity of the Valencia trough and surrounding areas. Tectonophysics, 203: 99-109.




Perea, H., Masana, E. and Santanach, P. (2010): Geomorphological features of mountain fronts controlled by low slip extensional faults: the northweastern margin of the València trough. In: Contribución de la geología al análisis de la peligrosidad sísmica (Insua, J.M. and Martín-González, F., eds.). 19-22.

Saula, E., Picart, J., Mató, E., Llenas, M., Losantos, M., Berástegui, X., Agustí, J. (1996): Evolución geodinámica de la fosa del Empordà y las Sierras Transversales. Acta Geológica Hispánica 29 (2–4 (1994)), 55–75.




Página 27 de 632



ID: ES006 Fault Name: Amer (1/2)

Segment Name: Amer norte

Location X: 2.467

Location Y: 42.088


Filiation: ICM-CSIC



Average Strike(º): 335 LD Saula et al. (1996); Ferrer et al. (1999). Note that the fault changes its strike at (2.4337,42.1177) from 321 (to the south) to 357 (to the north).







Width (km): 15.6 AR

Area (km²): 205.86 AR


Unknown








Unknown


1 in last 573 yr

1-2 LD Fault responsible of at least 1, an probable 2, of the 3 earthquakes of the Catalan Seismic Crisis between 1427-1428 (Goula et al., 1992; Ferrer et al, 1999; Fleta et al., 2001; Perea, 2006; Perea et al., 2006; Perea, 2009)


Unknown

Identification


Quaternary Activity

Variability Source

Comment




Comment


C+*Strength Class:


Paleoearthquakes

Orden Visual: 16

Página 28 de 632








573 LD Source of the Catalan Seismic Crisis 1427-1428 (Fontserè and Iglésies, 1971; Cadiot, 1979; Goula et al, 1992; Olivera et al, 1992; Lambert, 1993; Ferrer et al, 1999; Fleta et al, 2001; Olivera et al, 2006; Perea, 2006; Perea et al, 2006; Perea, 2009).


Cadiot, B. (1979): Les effets en France du séisme Catalan de 1428. In: J. Vogt (Editor), Les tremblements de terre en France. BRGM, Orleans, pp. 166-172.




Goula, X., Olivera, C., Escuer, J., Fleta, J., Grellet, B., Bousquet, J.C. (1992): Neotectonics and seismicity of the area of the seismic crisis of 1427-28 in Catalonia. Proceedings of the 22nd General Assembly of the European Seismological Comission, Barcelona: 333-338.

Lambert, J. (1993): The Catalonian (1428) and Alpine (1564, 1644) earthquakes: review of research in France. In: M. Stucchi (Editor), Historical investigation of european earthquakes. CNR, Milano, pp. 145-159.







References

Variability





ES006

Olot earthquake 15/05/1427 2.4333, 41.1667



analysis

2nd event of the Catalan Seismic Crisis 1427-1428 (Fontserè and Iglésies, 1972; Cadiot, 1979; Goula et al, 1992; Olivera et al, 1992; Lambert, 1993; Ferrer et al, 1999; Fleta et al, 2001; Olivera et al, 2006; Perea, 2006; Perea et al, 2006; Perea, 2009)

601

ES006

Camprodon earthquake

02/02/1428 2.3333, 42.3000


ICC Macroseismic data and Coulomb stress

analyses

3rd event of the Catalan Seismic Crisis 1427-1428 (Fontserè and Iglésies, 1972; Cadiot, 1979; Goula et al, 1992; Olivera et al, 1992; Lambert, 1993; Ferrer et al, 1999; Fleta et al, 2001; Olivera et al, 2006; Perea, 2006; Perea et al, 2006; Perea, 2009)

602

Página 29 de 632






Saula, E., Picart, J., Mató, E., Llenas, M., Losantos, M., Berástegui, X., Agustí, J. (1996): Evolución geodinámica de la fosa del Empordà y las Sierras Transversales. Acta Geológica Hispánica 29 (2–4 (1994)), 55–75.




Página 30 de 632



ID: ES007 Fault Name: Amer (2/2)

Segment Name: Amer sur

Location X: 2.624

Location Y: 41.968

Name of Compiler(s): Perea, H., Bach, J. and Linares, R.

Filiation: IDL-U. de Lisboa and Grupo Geodinámica Externa-UAB



Average Strike(º): 315 LD Saula et al. (1996); Ferrer et al. (1999). Note that the fault changes its strike at (2.5268,42.0499) from 318 (to the south) to 310 (to the north).







Width (km): 15.6 AR

Area (km²): 250.97 AR


Unknown








Unknown


1 in last 573 yr

LD Fault responsible of ´May 15ty earthquake of the Catalan Seismic Crisis between 1427-1428 (Goula et al., 1992; Ferrer et al, 1999; Fleta et al., 2001; Perea, 2006; Perea et al., 2006; Perea, 2009)


Unknown

Identification


Quaternary Activity

Variability Source

Comment




Comment


C+*Strength Class:


Paleoearthquakes

Orden Visual: 17

Página 31 de 632








573 LD Source of the Catalan Seismic Crisis 1427-1428 (Fontserè and Iglésies, 1971; Cadiot, 1979; Goula et al, 1992; Olivera et al, 1992; Lambert, 1993; Ferrer et al, 1999; Fleta et al, 2001; Olivera et al, 2006; Perea, 2006; Perea et al, 2006; Perea, 2009).

Extended Information:

Cadiot, B. (1979): Les effects en France du séisme Catalan de 1428. In: J. Vogt (Editor), Les tremblements de terre en France. BRGM, Orleans, pp. 166-172.




Goula, X., Olivera, C., Escuer, J., Fleta, J., Grellet, B., Bousquet, J.C. (1992): Neotectonics and seismicity of the area of the seismic crisis of 1427-28 in Catalonia. Proceedings of the 22nd General Assembly of the European Seismological Comission, Barcelona: 333-338.Lambert, J. (1993): The Catalonian (1428) and Alpine (1564, 1644) earthquakes: review of research in France. In: M. Stucchi (Editor), Historical investigation of european earthquakes. CNR, Milano, pp. 145-159.







Saula, E., Picart, J., Mató, E., Llenas, M., Losantos, M., Berástegui, X., Agustí, J. (1996): Evolución geodinámica de la fosa del Empordà




References

Variability





ES007

Amer earthquake 19/03/1427 2.5833, 41.9833



analysis

1st event of the Catalan Seismic Crisis 1427-1428 (Fontserè and Iglésies, 1972; Cadiot, 1979; Goula et al, 1992; Olivera et al, 1992; Lambert, 1993; Ferrer et al, 1999; Fleta et al, 2001; Olivera et al, 2006; Perea, 2006; Perea et al, 2006; Perea, 2009)

603

Página 32 de 632



y las Sierras Transversales. Acta Geológica Hispánica 29 (2–4 (1994)), 55–75.




Página 33 de 632



ID: ES008 Fault Name: El Camp (complete)

Segment Name:

Location X: 0.8764

Location Y: 40.9735


Filiation: ICM-CSIC



Average Strike(º): 035 LD Masana (1994, 1995 and 1996); Perea (2006); Perea et al. (2006). Note that the fault changes its strike at (1.1032, 41.1798) from 060 (to the south) to 030 (to the north) and at (0.9748, 41.1258) from 025 (to the south) to 060 (to the north).




Length (km): 41.1 ± 0.5 LD Masana (1994, 1995 and 1996); Perea (2006); Perea et al. (2006)



Width (km): 15.6 AR

Area (km²): 640.69 AR


<125ka LD Masana et al. (2001a) See El Camp 3/3: L'Hospitalet segment.


0.020 0.020-0.080 LD Masana et al. (2001a and 2001b); Santanach et al. (2001 and 2010). See El Camp 3/3: L'Hospitalet segment.






Unknown


5-6 in 300ka

5-6 LD Masana et al. (2001a and 2001b); Santanach et al. (2001 and 2010); Perea et al (2003 and 2006).


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Triangular facets, low sinuosity, wine glass basin shape, low space index, low valley-floor-to-height ratio.

Masana (1994, 1995 and 1996); Perea (2006); Perea et al. (2006); Perea et al. (2010)

Geological Set: Catalan Coastal Ranges (Tarragona)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 38

Página 34 de 632








3000 805 AD-30000

LD Masana et al. (2001a and 2001b); Santanach et al. (2001 and 2010); Perea et al (2003 and 2006).


Masana, E. (1994): Neotectonic features in the Catalan Coastal Ranges, Northeastern Spain. Acta Geol. Hispanica 29 (2-4), 107-121.

Masana, E. (1995): L'activitat neotectònica a les Cadenes Costaneres Catalanes. PhD thesis, Universitat de Barcelona, pp. 444.

Masana, E. (1996): Evidence for past earthquakes in an area of low historical seismicity: the Catalan coastal ranges, NE Spain. Anali di Geofisica XXXIX, 689-704.

Masana, E., Villamarín, J.A., Sánchez Cabañero, J., Plaza, J., Santanach, P. (2001a): Seismogenic faulting in an area of low seismic activity: Paleoseismicity of the El Camp fault (Northeast Spain). Geol. Mijnbouw/Netherlands J. Geosciences 80 (3-4), 29-41.

Masana, E., Villamarín, J.A., Santanach, P. (2001b): Paleoseismic results from multiple trenching analysis along a silent fault: The El Camp fault (Tarragona, northeastern Iberian Peninsula). Acta Geol. Hispanica 36 (3-4), 329-354.



Perea, H., Figueiredo, P.M., Carner, J., Gambini, S., Boydell, K. (2003): Paleoseismological data from a new trench across the El Camp Fault (Catalan Coastal Ranges, NE Iberian Peninsula). Annals of Geophysics 46, 763-774.







Santanach, P., Masana, E., Villamarín, J.A. (2001): Proyecto Datación. CSN-Consejo de Seguridad Nuclear, Madrid, pp. 159.

Santanach, P., Masana, E. and Perea, H. (2010): The El Camp fault revisited: A 300 ka long paleoseismic history of a low-slip normal fault in northeastern Iberia. In: Contribución de la geología al análisis de la peligrosidad sísmica (Insua, J.M. and Martín-González, F., eds.). 23-26.






References

Variability



Página 35 de 632




Página 36 de 632



ID: ES009 Fault Name: El Camp (1/3)

Segment Name: La Selva

Location X: 1.0889

Location Y: 41.1738


Filiation: ICM-CSIC



Average Strike(º): 030 LD Masana (1994, 1995 and 1996); Perea (2006); Perea et al. (2006)







Width (km): 15.6 AR

Area (km²): 262.70 AR


Unknown


0.030 0.018-0.045 LD Triangular facets and alluvial fan surface: 90m/5Ma and 2Ma (Masana, 1994, 1995 and 1996; Perea, 2006; Perea et al., 2006).






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential


Masana (1994, 1995 and 1996); Perea (2006); Perea et al. (2006)); Perea et al. (2010)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 39

Página 37 de 632








Unknown
















Source Comment



References

Variability



Página 38 de 632




Segment Name: Vilavella

Location X: 0.937

Location Y: 41.0925


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 207.25 AR


Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 40

Página 39 de 632








Unknown
















Source Comment



References

Variability



Página 40 de 632




Segment Name: L'Hospitalet

Location X: 0.8764

Location Y: 40.9735


Filiation: ICM-CSIC



Average Strike(º): 025 LD Masana (1994, 1995 and 1996); Santanach et al. (2001); Perea (2006); Perea et al. (2006)




Length (km): 18.2 ± 0.5 LD Masana (1994, 1995 and 1996); Perea (2006); Perea et al. (2006). The faults enters into the sea and its length could be around 24 km (Santanach et al., 2001).



Width (km): 15.6 AR

Area (km²): 282.99 AR


<125ka LD Masana et al. (2001a)


0.020 0.020-0.080 LD Masana et al. (2001a and 2001b); Santanach et al. (2001 and 2010).






Unknown


5-6 in 300 ka

5-6 LD Masana et al. (2001a and 2001b); Santanach et al. (2001 and 2010).


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Triangular facets, low sinuosity, wine glass basin shape, low space index, low valley-floor-to-height ratio, fault escarpment.




Comment


A+*Strength Class:

Slip Rate *Accuracy Class: A

Paleoearthquakes

Orden Visual: 41

Página 41 de 632




6.65 ± 0.37 ER Mw using Stirling et al. (2002) equation. Mw 6.50 calculated using Wells and Coppersmith (1994) surface rupture length relationship for normal faults (Masana et al., 2001a and 2001b; Santanach et al. 2001 and 2010; Perea, 2006, Perea et al 2003 and 2006)


30000 25000-50000 LD Paleoseismic data from Masana et al. (2001a and 2001b); Santanach et al. (2001 and 2010); Perea et al (2003 and 2006). Considering the Maximum Earthquake Model (Wesnousky, 1986) and an average slip rate of 0.05 m/ka results 24702 yrs.


3000 805 AD-30000

LD Masana et al. (2001a and 2001b); Santanach et al. (2001 and 2010); Perea et al (2003 and 2006).





Masana, E., Villamarín, J.A., Sánchez Cabañero, J., Plaza, J., Santanach, P. (2001a): Seismogenic faulting in an area of low seismic activity: Paleoseismicity of the El Camp fault (Northeast Spain). Geol. Mijnbouw/Netherlands J. Geosciences 80 (3-4), 29-41.

Masana, E., Villamarín, J.A., Santanach, P. (2001b): Paleoseismic results from multiple trenching analysis along a silent fault: The El Camp fault (Tarragona, northeastern Iberian Peninsula). Acta Geol. Hispanica 36 (3-4), 329-354.



Perea, H., Figueiredo, P.M., Carner, J., Gambini, S., Boydell, K. (2003): Paleoseismological data from a new trench across the El Camp Fault (Catalan Coastal Ranges, NE Iberian Peninsula). Annals of Geophysics 46, 763-774.







Santanach, P., Masana, E., Villamarín, J.A. (2001): Proyecto Datación. CSN-Consejo de Seguridad Nuclear, Madrid, pp. 159.

Santanach, P., Masana, E. and Perea, H. (2010): The El Camp fault revisited: A 300 ka long paleoseismic history of a low-slip normal fault in northeastern Iberia. In: Contribución de la geología al análisis de la peligrosidad sísmica (Insua, J.M. and Martín-González, F., eds.). 23-26.






References

Variability



Página 42 de 632




Página 43 de 632



ID: ES012 Fault Name: Montseny

Segment Name:

Location X: 2.2953

Location Y: 41.69


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 360.09 AR


Quaternary Pliocene-Quaternary

EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential



Geological Set: Catalan Coastal Ranges (Barcelona)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 42

Página 44 de 632








Unknown


Fontboté, J.M. (1954): Las relaciones tectónicas de la depresión del Vallès-Penedès con la Cordillera Prelitoral y con la depresión del Ebro.Tomo homenaje al profesor E. Hernández Pacheco. Rev. Soc. Esp. Hist. Nat., 281-310.

Fontserè, E. (1927): El temblor de tierra del 12 de Marzo del 1927. Revista Ibérica, 23-IV-1327, -675.

Gasperini, P., Bernardini, F., Valensise, G., Boschi, E. (1999): Defining seismogenic sources from historical earthquake felt report. Bulletin of the Seismological Society of America, 89(1), 94-110.












Stirling, M., Rhoades, D. and Berryman K. (2002): Comparison of Earthquake Scaling Relations Derived from Data of the Instrumental

Source Comment



References

Variability





ES012

Sant Celoni earthquake

12/03/1927 2.4840, 41.7398

IMSK = VII / Mw = 5.0


analysis

Mw estimated from Boxer (Gasperini, 1999). Intensity coming from Fontserè (1927) and Susagna and Goula (1999). Fontboté (1954) associate this earthquake to the fault.

604

Página 45 de 632



and Preinstrumental Era. Bulletin of the Seismological Society of America, 92 (2): 812–830.

Susagna, T., Goula, X. (1999): Atlas sísmic de Catalunya. Volum 1: Catàleg de sismicitat. Institut Cartogràfic de Catalunya, p. 436.Wells, D.L., Coppersmith, K.J. (1994): New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bulletin of the Seismological Society of America 84 (4), 974–1002.


Página 46 de 632



ID: ES013 Fault Name: Pla de Barcelona

Segment Name:

Location X: 1.9574

Location Y: 41.2654


Filiation: ICM-CSIC



Average Strike(º): 040 LD Perea (2006); Perea et al. (2006)




Length (km): 32.1 ± 0.5 LD Perea (2006); Perea et al. (2006)



Width (km): 15.6 AR

Area (km²): 500.87 AR



EJ Unknown


0.020 0.015-0.038 LD Triangular facets and alluvial fan surface: 75m/5Ma and 2Ma (Perea, 2006; Perea et al., 2006).






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential


Perea (2006); Perea et al. (2006)); Perea et al. (2010)

Geological Set: Catalan Coastal Ranges (Barcelona-Girona)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 43

Página 47 de 632








Unknown













Source Comment



References

Variability



Página 48 de 632



ID: ES014 Fault Name: Pla de Burgar

Segment Name:

Location X: 0.6382

Location Y: 40.9342


Filiation: ICM-CSIC



Average Strike(º): 350 LD Masana (1994, 1995 and 1996); Perea (2006); Perea et al. (2006). Note that the fault changes its strike at (0.5992, 41.0500) from 356 (to the south) to 026 (to the north) and at (0.6038, 41.0001) from 334 (to the south) to 356 (to the north).







Width (km): 15.6 AR

Area (km²): 264.43 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 44

Página 49 de 632




6.62 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. A Mw 6.40 results from using Wells and Coppersmith (1994) surface rupture length relationship for normal faults (Perea, 2006; Perea et al., 2006).




Unknown



















References

Variability



Página 50 de 632



ID: ES015 Fault Name: Baix Ebre (complete)

Segment Name:

Location X: 0.01646

Location Y: 40.3868


Filiation: ICM-CSIC



Average Strike(º): 032 LD Masana (1994, 1995, 1996); Perea (2006); Perea et al. (2006). Strike changes from north being 014 until (0.400, 40.754), 036 until (0.326, 40.684), 061 until (0.241, 40.648), 023 until (0.156, 40.495), 052 until (0.088, 40.455), 033 until (0.040, 40.398).







Width (km): 15.6 AR

Area (km²): 1247.08 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment



Geological Set: Catalan Coastal Ranges (Castellón-Tarragona)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 45

Página 51 de 632








Unknown



















References

Variability



Página 52 de 632



ID: ES016 Fault Name: Baix Ebre (1/5)

Segment Name: La Caramella

Location X: 0.3968

Location Y: 40.7516


Filiation: ICM-CSIC



Average Strike(º): 014 LD Masana (1994, 1995 and 1996); Perea (2006); Perea et al. (2006).







Width (km): 15.6 AR

Area (km²): 341.39 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 46

Página 53 de 632








Unknown
















Source Comment



References

Variability



Página 54 de 632




Segment Name: La Sénia norte

Location X: 0.3251

Location Y: 40.6838


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 169.91 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 47

Página 55 de 632








Unknown
















Source Comment



References

Variability



Página 56 de 632




Segment Name: La Sénia sur

Location X: 0.235

Location Y: 40.6475


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 169.91 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 48

Página 57 de 632








Unknown
















Source Comment



References

Variability



Página 58 de 632




Segment Name: Tirig norte

Location X: 0.07733

Location Y: 40.452487


Filiation: ICM-CSIC



Average Strike(º): 042 LD Perea (2006); Perea et al. (2006).







Width (km): 15.6 AR

Area (km²): 221.18 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential


Perea (2006); Perea et al. (2006); Perea et al. (2010)

Geological Set: Catalan Coastal Ranges (Castellón)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 49

Página 59 de 632








Unknown













Source Comment



References

Variability



Página 60 de 632




Segment Name: Tirig sur

Location X: 0.0165

Location Y: 40.3868


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 134.06 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 50

Página 61 de 632








Unknown













Source Comment



References

Variability



Página 62 de 632



ID: ES021 Fault Name: Montsiá

Segment Name:

Location X: 0.5298

Location Y: 40.5641


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 171.47 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 51

Página 63 de 632








Unknown













Source Comment



References

Variability



Página 64 de 632



ID: ES022 Fault Name: Salsadella (complete)

Segment Name:

Location X: 0.2058

Location Y: 40.4672


Filiation: ICM-CSIC



Average Strike(º): 203 LD Perea (2006); Perea et al. (2006). Strike changes from north being 198 until (0.186, 40.419), 133 until (0.192, 40.414), 121 until (0.132, 40.340), 157 until (0.136, 40.334), 205 until (0.096, 40.270).

Dip (º): 60 ± 10 LD Roca (1992 and 1996); Roca and Guimerà (1992); Simón (1984)

Rake (º): -90 ± 10 LD Roca (1992 and 1996); Roca and Guimerà (1992)); Simón (1984)

Sense of Movement: N LD Roca (1992 and 1996); Roca and Guimerà (1992)); Simón (1984)




Width (km): 15.6 AR

Area (km²): 366.33 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 52

Página 65 de 632








Unknown

















References

Variability



Página 66 de 632



ID: ES023 Fault Name: Salsadella (1/3)

Segment Name: Salsadella norte

Location X: 0.2058

Location Y: 0.4672


Filiation: ICM-CSIC




Dip (º): 60 ± 10 LD Roca (1992 and 1996); Roca and Guimerà (1992)); Simón (1984)






Width (km): 15.6 AR

Area (km²): 90.41 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 53

Página 67 de 632








Unknown














Source Comment



References

Variability



Página 68 de 632




Segment Name: Salsadella central

Location X: 0.1891

Location Y: 40.4123


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 148.09 AR



EJ Unknown


0.020 0.014-0.035 LD Triangular facets and alluvial fan surface:70m/5Ma and 2Ma (Perea, 2006; Perea et al., 2006).






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 54

Página 69 de 632






40633 209647-6510 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Perea (2006) obtained 26000 yrs considering Mw6.20 from W&C'94 and 0.020 m/ka. The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown














Source Comment



References

Variability



Página 70 de 632




Segment Name: Salsadella sur

Location X: 0.134



Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 124.71 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 55

Página 71 de 632








Unknown














Source Comment



References

Variability



Página 72 de 632



ID: ES026 Fault Name: Alcalá de Xivert (complete)

Segment Name:

Location X: 0.3545

Location Y: 40.3915


Filiation: ICM-CSIC



Average Strike(º): 222 LD Perea (2006); Perea et al. (2006). Strike changes from north being 227 until (0.272, 40.333), 211 until (0.241, 40.295).







Width (km): 15.6 AR

Area (km²): 226.03 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 56

Página 73 de 632








Unknown

















References

Variability



Página 74 de 632



ID: ES027 Fault Name: Alcalá de Xivert (1/2)

Segment Name: Alcalá de Xivert norte

Location X: 0.3545

Location Y: 40.392


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 137.18 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 57

Página 75 de 632








Unknown














Source Comment



References

Variability



Página 76 de 632



ID: ES028 Fault Name: Alcalá de Xivert (2/2)

Segment Name: Alcalá de Xivert sur

Location X: 0.2735

Location Y: 40.3334


Filiation: ICM-CSIC










Width (km): 15.6 AR




EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 58

Página 77 de 632








Unknown














Source Comment



References

Variability



Página 78 de 632



ID: ES029 Fault Name: Serra d'Irta

Segment Name:

Location X: 0.2806

Location Y: 40.3101


Filiation: ICM-CSIC










Width (km): 15.6 AR




EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 59

Página 79 de 632








Unknown














Source Comment



References

Variability



Página 80 de 632



ID: ES030 Fault Name: Vall d'Angel

Segment Name:

Location X: 0.19927

Location Y: 40.3351


Filiation: ICM-CSIC










Width (km): 15.6 AR




EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 60

Página 81 de 632








Unknown














Source Comment



References

Variability



Página 82 de 632



ID: ES031 Fault Name: Catí (complete)

Segment Name:

Location X: -0.0749

Location Y: 40.3593


Filiation: ICM-CSIC



Average Strike(º): 025 LD Perea (2006); Perea et al. (2006). Strike changes from north being 021 until (0.000, 40.466), 028 until (-0.074, 40.361).







Width (km): 15.6 AR

Area (km²): 296.18 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 61

Página 83 de 632








Unknown

















References

Variability



Página 84 de 632



ID: ES032 Fault Name: Catí (1/2)

Segment Name: Segmento de Catí norte

Location X: 0.0025

Location Y: 40.4619


Filiation: ICM-CSIC










Width (km): 15.6 AR




EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 62

Página 85 de 632








Unknown














Source Comment



References

Variability



Página 86 de 632



ID: ES033 Fault Name: Catí (2/2)

Segment Name: Segmento de Catí sur

Location X: -0.0749

Location Y: 40.3593


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 194.86 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 63

Página 87 de 632








Unknown














Source Comment



References

Variability



Página 88 de 632



ID: ES034 Fault Name: Albocásser (complete)

Segment Name:

Location X: -0.0997

Location Y: 40.2685


Filiation: ICM-CSIC



Average Strike(º): 027 LD Perea (2006); Perea et al. (2006). Strike changes from north being 013 until (0.000, 40.392), 024 until (-0.040, 40.325), 039 until (-0.096, 40.270).







Width (km): 15.6 AR

Area (km²): 318.00 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 64

Página 89 de 632








Unknown

















References

Variability



Página 90 de 632



ID: ES035 Fault Name: Albocásser (1/3)

Segment Name: Segmento Albocásser norte

Location X: -0.00136

Location Y: 40.3881


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 106.42 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 65

Página 91 de 632








Unknown














Source Comment



References

Variability



Página 92 de 632




Segment Name: Segmento Albocásser central


Location Y: 40.2685


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 100.61 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 66

Página 93 de 632








Unknown














Source Comment



References

Variability



Página 94 de 632




Segment Name: Segmento Albocásser sur

Location X: -0.0997

Location Y: 40.2685


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 132.50 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 67

Página 95 de 632








Unknown














Source Comment



References

Variability



Página 96 de 632



ID: ES038 Fault Name: Atzeneta oriental (complete)

Segment Name:

Location X: -0.0565

Location Y: 40.3367


Filiation: ICM-CSIC



Average Strike(º): 212 LD Perea (2006); Perea et al. (2006). Strike changes from north being 218 until (-0.099, 40.297), 208 until (-0.130, 40.253), 190 until (-0.132, 40.242), 216 until (-0.172, 40.201).







Width (km): 15.6 AR

Area (km²): 280.59 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 68

Página 97 de 632








Unknown

















References

Variability



Página 98 de 632



ID: ES039 Fault Name: Atzeneta oriental (1/2)

Segment Name: Atzeneta oriental norte

Location X: -0.0565

Location Y: 40.3367


Filiation: ICM-CSIC



Average Strike(º): 214 LD Perea (2006); Perea et al. (2006). Strike changes from north being 218 until (-0.099, 40.297), 208 until (-0.130, 40.253).







Width (km): 15.6 AR

Area (km²): 174.59 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 69

Página 99 de 632








Unknown

















References

Variability



Página 100 de 632



ID: ES040 Fault Name: Atzeneta oriental (2/2)

Segment Name: Atzeneta oriental sur


Location Y: 40.2501


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 101.32 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 70

Página 101 de 632








Unknown














Source Comment



References

Variability



Página 102 de 632



ID: ES041 Fault Name: Atzeneta occidental

Segment Name:

Location X: -0.1475

Location Y: 40.273


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 148.09 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 71

Página 103 de 632








Unknown

















References

Variability



Página 104 de 632



ID: ES042 Fault Name: Els Ivarsos (complete)

Segment Name:

Location X: -0.02630762

Location Y: 40.31302949

Name of Compiler(s): Perea, H.; García-Mayordomo, J. and Martín-Banda, R.

Filiation: Instituto de Ciencias del Mar-CSIC



Average Strike(º): 190 LD Perea (2006); Perea et al. (2006). Strike changes from north being 210 until (-0.073, 40.234), 166 until (-0.060, 40.194), 185 until (-0.063, 40.169).




Length (km): 24.2 ± 0.5 LD Perea (2006) and Perea et al. (2006); Simon et al. (2012) considers an additional southwestern segment (Els Ivarsos 3/3).



Width (km): 15.6 AR

Area (km²): 236.94 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 72

Página 105 de 632




6.76 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. The Mw is 6.70 calculated using Wells and Coppersmith (1994) surface rupture length relationship for normal faults, according to the length of 3 segments.




Unknown











Simón, J.L., Arlegui, L.E., Lafuente, P., Liesa, C.L. (2012): Active extensional faults in the central-eastern Iberian Chain, Spain. Journal of Iberian Geology, 38 (1), 127-144.


Wells, D.L., Coppersmith, K.J. (1994): New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bulletin of the Seismological Society of America 84 (4), 974–1002.Wesnousky, S. G. (1986): Earthquakes, quaternary faults and seismic hazard in California. J. Geophys. Res. 91(B12), 12587–12631.




References

Variability



Página 106 de 632



ID: ES043 Fault Name: Els Ivarsos (1/3)

Segment Name: Els Ivarsos norte

Location X: -0.0263

Location Y: 40.313


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 127.83 AR



EJ Unknown








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 73

Página 107 de 632








Unknown














Source Comment



References

Variability



Página 108 de 632




Segment Name: Els Ivarsos central

Location X: -0.06979341

Location Y: 40.23540124


Filiation: ICM-CSIC







Length (km): 6.8 ± 0.5 LD Perea (2006) and Perea et al. (2006).



Width (km): 15.6 AR

Area (km²): 106.00 AR



EJ








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 74

Página 109 de 632




6.24 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw is 6 using Wells and Coppersmith (1994) surface rupture length relationship for normal faults and length and area of Perea (2006) and Perea et al (2006).




Unknown











Simón, J.L., Arlegui, L.E., Lafuente, P., Liesa, C.L. (2012): Active extensional faults in the central-eastern Iberian Chain, Spain. Journal of Iberian Geology, 38 (1), 127-144.







References

Variability



Página 110 de 632



ID: ES045 Fault Name: Vall d'Uixó

Segment Name:

Location X: -0.316

Location Y: 39.7852


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 113.16 AR



EJ








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential



Geological Set: Catalan Coastal Ranges (Castellón-Valencia)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 76

Página 111 de 632








Unknown














Source Comment



References

Variability



Página 112 de 632



ID: ES201 Fault Name: Ventaniella

Segment Name: Suroriental

Location X: -4.744

Location Y: 42.894

Name of Compiler(s): Martín Banda, R. and García Mayordomo, J.

Filiation: Universidad Complutense de Madrid and IGME

Email: [email protected]; Julian.


Average Strike(º): 117 ± 3 LD Compiler's measurement based Nozal and Gracia (1990), IGME y ENRESA (1998), Tavani et al. (2011). According to Tavani et al (2011) Ubierna and Ventaniella faults form part of the same shear zone, about 15 km wide, and called it the Ubierna Fault System.

Dip (º): 85 80-90 LD Sub-vertical. Nozal and Gracia (1990), IGME y ENRESA (1998), Tavani et al. (2011).

Rake (º): 180 to 135 LD Tavani et al. (2011). Slightly transpressive.

Sense of Movement: D to DR LD Tavani et al. (2011). Slightly transpressive.

Length (km): 39.0 25-40 EJ Compiler's measurement based on Mapa Neotectónico de España, for the Quaternary trace of the Ventaniella fault (IGME y ENRESA, 1998) . Fault may extend further to the SE according to Tavani et al. (2011).

Min Depth (km): 0 0-1 LD Nozal y Gracia (1990), IGME y ENRESA (1998), Tavani et al. (2011).

Max Depth (km): 16.0 to 14 LD Tavani et al. (2011) based on seismicity depth distribution.

Width (km): 16.1 AR

Area (km²): 626.38 AR


Lower Pleistocene

LD According to Nozal and Gracia (1990) the fault is sealed by younger fans, Middle to Upper Pleistocene in age. There are no radiometric dating for the Quaternary formations in the area.


0.000 EJ VSR=0, assumed pure strike-slip faulting.


0.05 0.1- 0.01 EJ 0.1 and 0.01 are extreme values assumed by Villamor et al. (2012) for a seismic hazard calculation (Villamor, 2002).


0.05 0.1- 0.01 EJ 0.1 and 0.01 are extreme values assumed by Villamor et al. (2012) for a seismic hazard calculation (Villamor, 2002).


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Morphologic lineament 2) It offsets early Pleistocene alluvial fan deposits 3) Possible association to seismic epicentres.

Nozal and Gracia (1990), IGME y ENRESA (1998), Tavani et al. (2011).

Geological Set: Basque-Cantabrian Basin and Duero Basin (Palencia a


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 1

Página 113 de 632




Unknown


6.96 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. Considering uncertainty in length (25-40 km) results: 6.78-6.97.


33420 599766-4656 AR Considering the MEM (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter. Villamor et al. (2012) estimated for Ventaniella segments 5 and 6: 50-10 kyr.


Unknown

Extended Information: EXTENDED INFORMATION\

IGME and ENRESA (1998a): Neotectonic Map of Spain, scale 1:1.000.000.

IGME and ENRESA (1998b): Memory of the Neotectonic and Seismotectonic Map of Spain, scale 1:1.000.000. Vol.1

Nozal, F., and Gracia , F.J. (1990): El piedemonte de la Sierra del Brezo (Montes Palentinos). Primera Reunión Nacional de Geomorfología, Teruel: 763-772.


Tavani, S., Quintà, A., and Granado, P. (2011): Cenozoic right-lateral wrench tectonics in the Western Pyrenees (Spain): The Ubierna Fault System. Tectonophysics, 509, 238–253.

Villamor, P. (2002) "Cinemática terciaria y cuaternaria de la falla de Alentejo Plasencia y su influencia en la peligrosidad sísmica del interior de la Peninsula Ibérica" PhD Thesis. UCM. 343p

Villamor, P., Capote, R., Stirling, M.W., Tsige, M., Berryman, K.R., Martínez-Díaz, J.J., and Martín-González, F (2012): Contribution of active faults in the intraplate area of Iberia to seismic hazard: The Alentejo-Plasencia Fault. Journal of Iberian Geology, 38 (1), 85-111.




References

Variability



Página 114 de 632



ID: ES204 Fault Name: Plasencia (1/4)

Segment Name: Cañaveral

Location X: -6.45666666666667

Location Y: 39.7366666666667

Name of Compiler(s): Martín-Banda, R. and García-Mayordomo, J.




Average Strike(º): 050 LD Villamor et al. (2012)

Dip (º): 90 LD Villamor et al. (2012)

Rake (º): 2 LD Villamor et al. (2012)

Sense of Movement: S LD Villamor et al. (2012)

Length (km): 43.2 ± 0.5 LD Villamor et al. (2012)

Min Depth (km): 0 LD Villamor et al. (2012)

Max Depth (km): 20.0 EJ

Width (km): 20.0 AR

Area (km²): 863.00 AR


Middle Pleistocene

LD Villamor et al. (2012)


0.002 ± 0.001 AR Relationship between NSR, dip and rake


0.07 ± 0.02 AR Relationship between NSR and rake


0.07 ± 0.02 LD Associated with pull-apart formation (16 Ma) (Villamor et al., 2012)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Pull-apart basin of Plasencia. In Moro pull-apart basin, two fault scarps resemble recent and a shutter ridge. A Middle Pleistocene fluvial terrace is faulted.

Villamor (2002), p. 114 y 116; Villamor et al. (2012)

Geological Set: Iberian Massif - Central Iberian Zone (Cáceres)


Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 4

Página 115 de 632




7.00 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw from rupture length (Wells and Coppersmith, 1994) is 6.95 and from Anderson et al. (1996) assuming a SR 0.05 m/ka is 7.32 (Villamor et al., 2012).


19798 99482-4290 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Villamor et al. (2012) obtained 25635 yrs considering Mw 6.95 from W&C'94 and 0.05 m/ka. The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown


Anderson, J.G., Wesnousky, S.G., Stirling, M.W. (1996): Earthquake size as a function of fault slip rate. Bull. Seis. Soc. America 86, 683-690.




Wells, D.L.; Coppersmith, K.J. (1994): New empirical relationships among magnitude, rupture length, rupture area, and surface displacement. Bull. Seis. Soc. of America 84, 974-1002.

Source Comment



References

Variability

*Reliability rating: B


Página 116 de 632




Segment Name: Brozas

Location X: -6.65333333333333

Location Y: 39.5483333333333












Width (km): 20.0 AR

Area (km²): 536.00 AR


Middle Pleistocene

LD Villamor (2002), p.166; Villamor et al. (2012)






0.09 ± 0.03 LD Associated with pull-apart formation (16 Ma) (Villamor et al., 2012)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Deformation of at least 1 m vertical thrown in a Middle Pleistocene terrace in Cañaveral pull-apart basin. Fault scarp.

Villamor (2002), p. 166; Villamor et al. (2012)

Geological Set: Iberian Massif - Central Iberian Zone (Cáceres)


Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 5

Página 117 de 632




6.81 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw from rupture length (Wells and Coppersmith, 1994) is 6.74 and from Anderson et al. (1996) assuming a SR 0.05 m/ka is 7.08 (Villamor et al. (2012)




Unknown







Source Comment



References

Variability



Página 118 de 632




Segment Name: Aliseda

Location X: -6.86666666666667

Location Y: 39.29












Width (km): 20.0 AR

Area (km²): 682.60 AR


Plio-Quaternary

LD Villamor et al. (2012).






0.1 ± 0.03 LD Total Slip Rate for 16 Ma. SR 0.04 +/- 0.01 for 35 Ma (Villamor et al., 2012).


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Fault scarp. Neogene series sediments are also found at Ribera de Araya pull-apart basins but the detailed relationships with faulting are not exposed.

Villamor et al. (2012).

Geological Set: Iberian Massif - Central Iberian Zone (Cáceres-Badajoz


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 6

Página 119 de 632








Unknown







Source Comment



References

Variability



Página 120 de 632




Segment Name: Alburquerque

Location X: -6.9864

Location Y: 39.1122












Width (km): 20.0 AR

Area (km²): 417.40 AR


Lower Pleistocene

LD Villamor (2002), p.167






0.03 ± 0.02 LD Associated with Raña surface (for 2 Ma) and 0.012 +/- 0.008 for > 5 Ma (Villamor et al., 2012).


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Syncline deformation in a Lower Pleistocene terrace at Ribera de Albarragena

Villamor (2002), p. 167

Geological Set: Iberian Massif - Central System Zone (Badajoz)


Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 7

Página 121 de 632








Unknown







Source Comment



References

Variability



Página 122 de 632



ID: ES208 Fault Name: Plasencia (complete)

Segment Name: Alburquerque-Aliseda-Brozas-Cañaveral

Location X: -6.9864

Location Y: 39.1122









Length (km): 125.0 OD Sum of the lengths of the four segments



Width (km): 20.0 AR

Area (km²): 2500.00 AR


Middle Pleistocene

LD Villamor (2002). See segments for more information.


0.000 AR Relationship between NSR, dip and rake


0.05 0.01-0.10 AR Relationship between NSR and rake


0.05 0.01-0.10 LD Villamor et al. (2012)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

At least 1 m vertical thrown in a Middle Pleistocene terrace (see Brozas). Syncline deformation in a Lower Pleistocene terrace at Ribera de Albarragena (see Alburquerque). Drainage-relief relations and scarps in Moro basin (see Cañaverales).

Villamor (2002)

Geological Set: Iberian Massif - Central Iberian Zone (Cáceres-Badajoz


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 8

Página 123 de 632






43558 781692-6068 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Villamor et al. (2012) obtained 81079 yrs. The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown






Source Comment



References

Variability



Página 124 de 632



ID: ES214 Fault Name: Vilachá-Baralla

Segment Name:

Location X: -7.1022

Location Y: 43.1022

Name of Compiler(s): Martín-González, F.

Filiation: ESCET. Universidad Rey Juan Carlos



Average Strike(º): 210 LD Martín-González et al. (2012)

Dip (º): 70 LD Martín-González et al. (2012)

Rake (º): 175 LD Martín-González et al. (2012)

Sense of Movement: S LD Martín-González et al. (2012)

Length (km): 36.0 LD Martín-González et al. (2012)

Min Depth (km): 0 LD Martín-González et al. (2012)


Width (km): 21.3 AR

Area (km²): 766.21 AR


Pleistocene Pliocene-Pleistocene

LD Martín-González et al. (2012)


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Drainage affections in Sarria depression, displacement of the latest alluvial fans “Raña” Pliocene-Pleistocene in age (not dated)

Martín-González et al. (2012)

Geological Set: Iberian Massif - Asturoccidental-Leonesa Zone (Lugo-A


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 9

Página 125 de 632




6.93 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. It is 6.90 using the magnitude-rupture length scaling relation from Wells and Coppersmith (1994).




Unknown


Martín-González, F., 2005. Tectónica Alpina, Neotectónica y Sismotectónica en la terminación occidental de los relieves cantábricos (Noroeste del Macizo Ibérico): Marco tectónico de las crisis sísmicas de Lugo. Tesis Doctoral, Univ. Complutense, 313 p.

Martínez-Díaz, J.J., Capote R., Tsige M., Villamor P., Martín-González F., Insua-Arévalo, J .M., 2006. Seismic triggering in a stable continental area: The Lugo1995-1997 seismic sequences (NW Spain). Journal of Geodynamics 41, 440-449.

Martín-González, F., 2009. Cenozoic tectonic activity in a Variscan basement: Evidence from geomorphological markers and structural mapping (NW Iberian Massif). Geomorphology 107, 210-225. doi: 10.1016/j.geomorph.2008.12.008

Martín-González, F., Antón, L., Insua, J.M., De Vicente, G., Martínez- Díaz, J.J., Muñoz-Martín, A., Heredia, N., Olaiz, A. 2012. Seismicityand potentially active faults in the Northwest and Central-West Iberian Peninsula. Journal of Iberian Geology 38, 53–69. DOI: 10.5209/ rev_JIGE.2012.v38.n1.39205.


Source Comment



References

Variability


*Reliability rating: Not Rated



ES214

Sarria-Triacastela-Becerreá

29 nov and 24

december 1995

4.6 IGN607

ES214

Sarria-Triacastela-Becerreá

May 1997 5.1 IGN608

Página 126 de 632



ID: ES401 Fault Name: Bañón

Segment Name:



Name of Compiler(s): González, Álvaro

Filiation: Universidad de Zaragoza



Average Strike(º): 205 OD Compiler's measurement, based on the cartographies by Olivé & Gutiérrez (1983) and Portero et al. (1983).

Dip (º): 60 45-90 EJ Typical dip of normal faults.

Rake (º): -90 EJ No evidence of strike-slip displacement suggests purely dip-slip, normal displacement.

Sense of Movement: N LD Gracia (1990); Gracia and Gutiérrez (1996); Rubio and Simón (2007); Gutiérrez et al. (2008).

Length (km): 3.7 OD Compiler's measurement of end-to-end distance, based on the cartographies by Olivé & Gutiérrez (1983) and Portero et al. (1983).

Min Depth (km): 0 LD The fault crops out at the surface (e.g. Gracia and Gutiérrez, 1996; Rubio and Simón, 2007; Gutiérrez et al., 2008).

Max Depth (km): 15.0 EJ Depths assigned to the seismicity in the region typically range between 5 and 15 km, and are always less than 25 km (IGN, 2010). That's consistent to the brittle layer above a basal detachment level ,

Width (km): 17.3 AR



Pleistocene Pleistocene-Holocene

LD Gracia and Gutiérrez (1996) show that the fault offsets Pleistocene alluvial deposits, and probably Holocene soil.


0.040 0.01-0.05 EJ There are no published estimates of slip rate for this fault. If the 50-cm-high scarp is Holocene in age (12000 yr old at most), the slip rate is ca. 0.04 m/ky. This is slightly smaller than the slip rate of the adjacent Calamocha Fault (0.05 m/ky).


0 EJ No evidences for horizontal slip during the Quaternary have been reported.


0.05 0.01-0.07 EJ Compiler's crude estimate, taking into account the assumed range of vertical slip rate and the assumed range of fault dips.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Faulted Quaternary alluvial deposits. Continuous fault scarp, about 50 cm high.

As reviewed by Gutiérrez et al. (2008). Previous works by Moissenet (1980); Olivé & Gutiérrez (1983); Portero et al. (1983); Gracia (1990) and Gracia and Gutiérrez (1996). The scarp height is mentioned by Gracia and Gutiérrez (1996).

Geological Set: Iberian Range (Teruel)


Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 91

Página 127 de 632




Unknown


5.99 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. Using equation derived from the preinstrumental dataset, Mw is higher (6.3, 6.2-6.5).




Unknown


Gracia, J. (1990): Geomorfología de la región de Gallocanta (Cordillera Ibérica Central). PhD Thesis. Universidad de Zaragoza (Spain). 660 p.

Gracia, F.J. & Gutiérrez, F. (1996): Neotectónica y sismicidad del valle del Jiloca y sus alrededores. Xiloca, 17: 165–206.

Gracia, F.J.; Gutiérrez, F. & Gutiérrez, M. (2003): The Jiloca karst polje-tectonic graben (Iberian Range, NE Spain). Geomorphology, 52: 215-231.

Gutiérrez, F.; Gutiérrez, M.; Gracia, F.J.; McCalpin, J.P.; Lucha, P. & Guerrero, J. (2008): Plio-Quaternary extensional seismotectonics and drainage network development in the central sector of the Iberian Chain (NE Spain). Geomorphology, 102: 21-42.

IGN (2010). Http://www.ign.es/ign/es/IGN/SisCatalogo.jsp

Moissenet, É. (1980): Relief et déformations récentes: trois transversales dans les fossés internes des chaînes ibériques orientales. Revue Géographique des Pyrénées et du Sud-Ouest, 51: 315–344.

Olivé, A. & Gutiérrez, M. (1983): Geomorfología. In: Mapa geológico de España E. 1:50.000, Monreal del Campo (516). Instituto Geológico y Minero de España, Madrid. pp 40-44 + map.

Portero, J.M.; Olivé, A. & Gutiérrez, M. (1983): Geomorfología. In: Mapa geológico de España E. 1:50.000, Calamocha (491). Instituto Geológico y Minero de España, Madrid. pp 48-64 + map.

Roca, E., Guimerà, J. (1992): The Neogene structure of the eastern Iberian margin: structural constraints on the crustal evolution of the Valencia trough (western Mediterranean). Tectonophys, 203: 203-218.

Rubio, J.C. & Simón, J.L. (2007): Tectonic subsidence v. erosional lowering in a controversial intramontane depression: the Jiloca basin (Iberian Chain, Spain). Geological Magazine, 144: 127-141.

Stirling, M.; Rhoades, D. & Berryman, K. (2002): Comparison of earthquake scaling relations derived from data of the instrumental and preinstrumental era. Bulletin of the Seismological Society of America, 92: 812-830.





References

Variability



Página 128 de 632



ID: ES402 Fault Name: Calamocha

Segment Name:







Average Strike(º): 149 OD Compiler's measurement, based on the cartographies by Portero et al. (1983); Gracia & Gutiérrez (1996); Gracia et al. (2003) and Rubio & Simón (2007).



Sense of Movement: N LD As reviewed by Gutiérrez et al. (2008).

Length (km): 15.0 OD Compiler's measurement of end-to-end distance, based on the cartographies by Portero et al. (1983); Gracia & Gutiérrez (1996); Gracia et al. (2003) and Rubio & Simón (2007).

Min Depth (km): 0 LD The fault crops out at the surface (e.g. Rubio and Simón, 2007; Gutiérrez et al., 2008).


Width (km): 17.3 AR

Area (km²): 259.81 AR


Quaternary LD As reviewed by Gutiérrez et al. (2008).


0.050 LD Minimum vertical offset since Early Pliocene: 250 m (Olivé et al., 1983) or 160-180 m (Rubio and Simón, 2007). The 250 m and a maximum age of 5.3 Ma (base of the Pliocene) yield a minimum vertical slip rate of 0.05 m/ky (Gutiérrez et al., 2008).




0.06 0.05-0.07 EJ Compiler's calculation, taking into account the minimum vertical slip rate of 0.05 m/ky and the assumed range of fault dips.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Early Pliocene limestone sediments displaced vertically more than 250 m. Faulted Quaternary alluvial deposits. Thick Plio-Quaternary sequence beneath the valley bottom. Triangular facets.

As reviewed by Gutiérrez et al. (2008). Previous works include those of Moissenet (1980); Portero et al. (1983); Simón (1983); Colomer (1987); Gracia (1990); Gracia & Gutiérrez (1996); Arlegui et al. (2005) and Rubio and Simón (2007).



Comment


A+*Strength Class:

Slip Rate *Accuracy Class: B

Paleoearthquakes

Orden Visual: 92

Página 129 de 632




Unknown


6.57 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. Using equation derived from the preinstrumental earthquakes, Mw is higher (6.8, 6.6-7.0).




Unknown.


Arlegui, L.E.; Simón, J.L.; Lisle, R.J. & Orife, T. (2005) Late Pliocene–Pleistocene stress field in the Teruel and Jiloca grabens (eastern Spain): contribution of a new method of stress inversion. Journal of Structural Geology, 27: 693-705.

Colomer, M. (1987): Estudi geològic de la vora sud-oest de la Fossa de Calataiud-Daroca entre Villafeliche i Calamocha. MSc Thesis, Universitat de Barcelona (Spain). 99 p.


Gracia, F.J. & Gutiérrez, F. (1996) Neotectónica y sismicidad del valle del Jiloca y sus alrededores. Xiloca, 17: 165-206.




Olivé, A.; Hernández, A.; Portero, J.M.; Moissenet, É.; Gutiérrez, M.; Aguilar, M.J. & Leal, M.C. (1983) Memoria. In: Mapa geológico de España E. 1:50.000, Calamocha (491). Instituto Geológico y Minero de España, Madrid.


Portero, J.M.; Olivé, A. & Gutiérrez, M. (1983): Geomorfología. In: Mapa geológico de España E. 1:50.000, Calamocha (491). Instituto Geológico y Minero de España, Madrid. p. 48-64 + map.

Roca, E., Guimerà, J. (1992): The Neogene structure of the eastern Iberian margin: structural constraints on the crustal evolution of the Valencia trough (western Mediterranean). Tectonophys, 203: 203-218.v


Simón, J.L. (1983): Tectónica y neotectónica del sistema de fosas de Teruel. Teruel 69: 21-97.






References

Variability



Página 130 de 632



ID: ES403 Fault Name: Daroca

Segment Name:







Average Strike(º): 142 OD Compiler's measurement, based on the cartographies by Olivé & Gutiérrez (1983) and Gracia (1992).



Sense of Movement: N LD e.g. Gracia (1992), Gutiérrez et al. (2008).

Length (km): 24.8 OD Compiler's measurement of end-to-end distance, based on the cartographies by Olivé & Gutiérrez (1983) and Gracia (1992).

Min Depth (km): 0 LD The fault crops out at the surface (e.g. Gracia, 1992).


Width (km): 17.3 AR

Area (km²): 429.55 AR


112855 yr BP ± 9145 yr LD OSL age (+/- 1-sigma range) of the youngest dated colluvial deposits offset by the fault (Gutiérrez et al., 2008, Fig. 14).


0.020 LD Minimum vertical slip rate (Gutiérrez et al., 2008), based on the displacement of Upper-Pliocene to Quaternary markers (Gracia, 1992).






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Fault scarp with triangular facets. >100 m thick Upper Pliocene-Pleistocene sequence deposited in the hangingwall basin. Faulted Upper Pleistocene mantled pediment deposits. Anomalously large alluvial fans.

As reviewed by Gutiérrez et al. (2008), based on previous work by Julivert (1954); Colomer (1987); Colomer and Santanach (1998) and Gracia (1990, 1992). The fault is part of the "Jiloca seismotectonic line" depicted by Rey Pastor and Bonelli Rubio (1957).

Geological Set: Iberian Range (Zaragoza-Teruel)


Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 93

Página 131 de 632








Unknown.


Colomer, M. (1987): Estudi geològic de la vora sud-oest de la Fossa de Calataiud-Daroca entre Villafeliche i Calamocha. MSc Thesis, Universitat de Barcelona (Spain). 99 p.

Colomer, M. & Santanach, P. (1988) Estructura y evolución del borde sur-occidental de la Fosa de Calatayud-Daroca. Geogaceta, 4: 29-31.


Gracia, J. (1992): Tectónica pliocena de la Fosa de Daroca (prov. de Zaragoza). Geogaceta, 11: 127-129.


Gutiérrez, F.; Masana, E.; González, Á.; Lucha, P.; Guerrero, J. & McCalpin, J.P. (2009): Late Quaternary paleoseismic evidence on the Munébrega half-graben fault (Iberian Range, Spain). International Journal of Earth Sciences, 98: 1691-1703.


Olivé, A. & Gutiérrez, M. (1983): Geomorfología. In: Mapa geológico de España E. 1:50.000, Daroca (465). Instituto Geológico y Minero de España, Madrid. p. 54-58 + map.

Julivert, M. (1954) Observaciones sobre la tectónica de la Depresión de Calatayud. Arrahona (Museo de Sabadell), 3-18.

Mezcua, J. & Martínez Solares, J.M. (1983): Sismicidad del área Iberomogrebi. Instituto Geográfico Nacional (Madrid). Publicación 203. 301 p.

Mezcua, J.; Rueda, J. & García Blanco, M. (2004): Reevaluation of historic earthquakes in Spain. Seismological Research Letters, 75 (1): 75-81.

Rey Pastor, A. & Bonelli Rubio, J. (1957): El sismo de Daroca-Used de 28 de septiembre de 1953 y su relación con la línea sismotectónica del Jiloca. Instituto Geográfico y Catastral, Madrid, 16 p + map.




References

Variability





ES403

Daroca-Used Earthquake or

Used Earthquake

September 28th, 1953

-1.57, 41.25 Magnitudes : MD=4.7;

Mw=5.0. Max. intensity VII

IGN catalog & Mezcua et al. (2004).

Spatial correlation with epicentre and isoseists.

Association noted by Rey Pastor & Bonelli Rubio (1957). See also Gracia (1992) and Gutiérrez et al. (2009). MD by Mezcua & Martínez Solares (1983). Mw by Mezcua et al. (2004). Focal depth might be about 15 km (Samardjieva et al., 1999).

609

ES403

Daroca earthquake September 11th, 1917

-1.4, 41.1 Maximum intensity IV

Instituto Geográfico

Nacional

Spatial correlation. The macroseismic epicentre is located on the fault trace.

612

Página 132 de 632




Samardjieva, E.; Payo, G. & Badal, J. (1999): Magnitude formulae and intensity-magnitude relations for early instrumental earthquakes in the Iberian Region. Natural Hazards, 19 (2-3): 189-204.



Página 133 de 632



ID: ES404 Fault Name: El Pobo Range

Segment Name:







Average Strike(º): 171 OD Compiler's measurement, based on the cartographies by Moissenet (1983) and Olivé et al. (1983).



Sense of Movement: N LD e.g. Moissenet (1983); Gutiérrez et al. (2008) and Lafuente et al. (2008).

Length (km): 13.7 10.4 - 13.7 OD Compiler's measurement, based on maps by Moissenet (1983) and Olivé et al. (1983). Fault trace assumed continuous (e.g. Gutiérrez Elorza, 1983); Quaternary mantled pediments with synsedimentary deformations (Moissenet, 1983) obscure part of it.

Min Depth (km): 0 LD The fault crops out at the surface (e.g. Moissenet, 1983).


Width (km): 17.3 AR

Area (km²): 237.29 AR


Plio-Quaternary

LD As reviewed by Gutiérrez et al. (2008).


0.120 LD Minimum vertical slip rate (Gutiérrez et al., 2008), based on 500 m of vertical Plio-Quaternary offset, and a maximum time interval of 4.2 million years for the deformation (base of the MN15 biozone).






Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Linear mountain front. Tectonically-controlled deposition of Upper Pliocene limestones and alluvial fan units. Eastward tilting of Lower Pliocene limestones and the Plio-Quaternary Perales mantled pediment.

As reviewed by Gutiérrez et al. (2008). Previous works include those of Moissenet (1980, 1982, 1983); Peña et al. (1981); Olivé et al. (1983); Simón (1983) and Gutiérrez (1998).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 94

Página 134 de 632




Unknown


6.53 ± 0.37 ER Mw from continuous trace length (13.7 km) using Stirling et al. (2002) equation derived from the instrumental dataset. Considering dashed trace (10.4 km) Mw is 6.42. Using equation derived from the preinstrumental dataset Mw is higher (6.8, 6.6-7.0).




Unknown.


Gutiérrez, F. (1998): Fenómenos de subsidencia por disolución de formaciones evaporíticas en las fosas neógenas de Teruel y Calatayud. PhD Thesis, Universidad de Zaragoza (Spain). 569 p.


Gutiérrez Elorza, M. (1983) Geomorfología. In: Mapa geológico de España, E. 1:50.000, Alfambra (542). Instituto Geológico y Minero de España, Madrid.


Lafuente, P.; Rodríguez-Pascua, M.A.; Simón, J.L.; Arlegui, L.E. & Liesa, C.L. (2008): Sismitas en los depósitos pliocenos y pleistocenos de la Fosa de Teruel. Revista de la Sociedad Geológica de España, 21: 133-149.


Moissenet, É. (1982): Le Villafranchien de la région de Teruel (Espagne), stratigraphie-déformations-milieux. In: Actes du Colloque "Le Villafranchien méditerranéen", p. 229–253. Lille (France).

Moissenet, É. (1983): Aspectos de la neotectónica en la Fosa de Teruel. In: Geología de España, vol. II. Instituto Geológico y Minero de España, Madrid. p. 423–446.

Olivé, A.; Godoy, A. & Moissenet, E. (1983): Cartografía. In: Mapa geológico de España, E. 1:50.000, Alfambra (542). Instituto Geológico y Minero de España, Madrid.

Peña, J.L.; Sánchez, M. & Simón, J.L. (1981) Algunos aspectos de la tectónica cuaternaria en el margen oriental de la fosa de Alfambra-Teruel. Teruel, 66: 31-48.


Simón, J.L. (1983): Tectónica y neotectónica del sistema de fosas de Teruel. Teruel, 69: 21-97.





References

Variability





ES404

Alfambra earthquake

June 16th, 1927

-1.0333, 40.5333

Maximum intensity V

Instituto Geográfico

Nacional

Spatial correlation The epicentre is located on the hanging wall of the fault.

611

Página 135 de 632



Página 136 de 632



ID: ES405 Fault Name: Munébrega E

Segment Name:







Average Strike(º): 322 OD Compiler's measurement, based on the cartography by Gutiérrez et al. (2009).



Sense of Movement: N LD Gutiérrez et al. (2008, 2009).

Length (km): 9.1 OD Compiler's measurement of end-to-end distance, based on the cartography by Gutiérrez et al. (2009).

Min Depth (km): 0 LD The fault crops out at the surface (e.g. Gutiérrez et al., 2009).


Width (km): 17.3 AR

Area (km²): 157.62 AR


Miocene LD The geomorphic expression of the fault and the associated Plio-Quaternary alluvial fan (interpreted as tectonically-induced) suggest recent activity, but the youngest sediments faulted in exposures are Miocene in age (Gutiérrez et al., 2009).


0.050 0.01-0.1 EJ Unknown. The weaker geomorphic expression than the Munébrega E Fault suggests that the slip rate may be smaller than in the nearby Munébrega W Fault (Gutiérrez et al., 2009).




0.05 0.01-0.1 EJ Unknown. The weaker geomorphic expression than the Munébrega E Fault suggests that the slip rate may be smaller than in the nearby Munébrega W Fault (Gutiérrez et al., 2009).


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Topographic lineament, reflected by a conspicuous break in slope. Exposures show faulted Miocene sediments. Plio-Quaternary alluvial fan (Valgalindo Fan) inset into the basin fill. Stream deflections controlled by the fault.

Detailed by Gutiérrez et al. (2009). The fault was previously studied by Hoyos et al. (1977); Gracia & Gutiérrez (1996); Gutiérrez (1996, 1998) and Gutiérrez et al. (2008).

Geological Set: Iberian Range (Zaragoza)


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 95

Página 137 de 632




Unknown






>7921 yr BP +/-587 LD In the exposure of a road cutting, the fault is covered by an undeformed mantled pediment; a sample taken from the base of the pediment deposits had an OSL age of 7921+/-587 yr BP (Gutiérrez et al., 2009).



Gutiérrez, F. (1996): Gypsum karstification induced subsidence: effects on alluvial systems and derived geohazards (Calatayud Graben, Iberian Range, Spain). Geomorphology 16: 277–293.




Hoyos, M., Zazo, C., Goy, J.L. & Aguirre, E. (1977): Estudio geomorfológico en los alrededores de Calatayud. Actas de la III Reunión Nacional (El Cuaternario en medios semiáridos), p. 149–160.







References

Variability



Página 138 de 632



ID: ES406 Fault Name: Munébrega W

Segment Name:







Average Strike(º): 144 ± 20 OD Compiler's measurement, based on the cartography by Gutiérrez et al. (2009). The range accounts for the sinuosity of the fault trace.



Sense of Movement: N LD del Olmo et al. (1983); Gutiérrez (1996, 1998); Gutiérrez et al. (2008); Gutiérrez et al. (2009).

Length (km): 18.2 18.2-20 LD The compiler's measurement of end-to-end distance is ca. 18.2 km. The total fault length (Gutiérrez et al., 2009) is 20 km. The difference is due to the sinuosity of the fault trace.

Min Depth (km): 0 LD The fault crops out at the surface (e.g. Gutiérrez et al., 2009).


Width (km): 17.3 AR

Area (km²): 315.23 AR


32567 yr BP ± 2467 yr LD OSL age (+/- 1-sigma range) of the youngest dated alluvial deposits clearly affected by the fault in a trench exposure (Gutiérrez et al., 2009).


0.100 +/-0.01 LD Calculated by Gutiérrez et al. (2009), from 7.4 m of vertical displacement (measured in a trench) of a stratigraphic marker dated by OSL at 71,809 +/- 5,555 yr BP (1-sigma range).




0.12 0.09-0.16 EJ Compiler's calculation, taking into account the vertical slip rate of 0.10 +/-0.01 m/ky and the assumed range of fault dips.


2.5 LD Inferred from a total of 7.4 m of displacement produced by three surface-rupturing earthquakes interpreted from a trench exposure, occurred after 71,809 ± 5,555 OSL yr BP (1-sigma range, Gutiérrez et al., 2009).

Identification


Quaternary Activity

Variability Source

Comment

Fault scarp offsetting Pleistocene sediments at least 7.4 m vertically. Linear range front with triangular and trapezoidal fault facets. Originates a half-graben partially filled with Plio-Quaternary sediments.

Detailed by Gutiérrez et al. (2009). The fault had been previously studied by del Olmo et al. (1983); Gracia & Gutiérrez (1996); Gutiérrez (1996, 1998) and Gutiérrez et al. (2008).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 96

Página 139 de 632




3 LD Three surface-rupturing earthquakes have been interpreted from a trench exposure, occurred after 71,809 ± 5,555 OSL yr BP (1-sigma range, Gutiérrez et al., 2009).


Unknown


6.65 ± 0.37 ER Magnitude from compiler's length (18.2 km) using Stirling et al. (2002) equation derived from the instrumental dataset. Considering total length (20 km), Mw is 6.69. Using equation derived from the preinstrumental earthquakes, Mw is higher (6.9, 6.7-7.1).


24000 ± 2000 LD Based on the identification of three surface-rupturing events occurred after 71,809 ± 5,555 OSL yr BP (Gutiérrez et al., 2009). The range reported here takes into account this 1-sigma range of age uncertainty.From Wesnousky'86 approach results 9240 yrs.


35000-18000 yr BP

LD The last surface-rupturing event (Gutiérrez et al. 2009) is younger than 32,567 ± 2,467 OSL yr BP (1-sigma range); and it is and probably older than 19,021 +/- 1,191 OSL yrs BP (1-sigma range), since sediments of this age may be undeformed.


del Olmo, P.; Aragonés, E. & Gutiérrez, M. (1983): Geomorfología. In: Mapa Geológico de España E. 1:50.000, Ateca (437). Instituto Geológico y Minero de España, Madrid. p. 45-48 + map.


Gutiérrez, F. (1996): Gypsum karstification induced subsidence: effects on alluvial systems and derived geohazards (Calatayud Graben, Iberian Range, Spain). Geomorphology, 16: 277–293.










References

Variability



Página 140 de 632



ID: ES407 Fault Name: Palomera Range

Segment Name:







Average Strike(º): 150 OD Compiler's measurement, based on the cartographies by Olivé & Gutiérrez (1983) and Gracia et al. (2003).



Sense of Movement: N LD e.g. Olivé & Gutiérrez (1983); Gracia et al. (2003); Rubio and Simón (2007) and Gutiérrez et al. (2008).

Length (km): 15.8 OD Compiler's measurement of end-to-end distance, based on the cartographies by Olivé & Gutiérrez (1983) and Gracia et al. (2003).

Min Depth (km): 0 LD The fault crops out at the surface (e.g. Rubio & Simón, 2007; Gutiérrez et al., 2008).


Width (km): 17.3 AR

Area (km²): 273.66 AR


Quaternary Upper Pliocene-Quaternary

LD e.g. Gutiérrez et al. (2008).


0.040 0.02-0.2 EJ Compiler's estimate, based on a variety of estimates of vertical throw (Cortés and Casas, 2000; Gracia et al., 2003, 2008; Rubio and Simón, 2007; Gutiérrez et al., 2008). See "Extended Data" section for details.




0.04 0.02-0.2 EJ Compiler's estimate, based on a variety of estimates of vertical throw (Cortés and Casas, 2000; Gracia et al., 2003, 2008; Rubio and Simón, 2007; Gutiérrez et al., 2008), and the assumed range of fault dips. See "Extended Data" section for details.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Linear mountain front. Faulted Upper Pliocene–Quaternary alluvial deposits with angular unconformities and cumulative wedge outs. Anomalously steep fans. Triangular and trapezoidal fault facets. Hanging canyons.

As reviewed by Gutiérrez et al. (2008). Other works: Moissenet (1980); Olivé & Gutiérrez (1983); Simón (1983); Cortés (1999); Cortés and Casas (2000); Casas-Sainz and Cortés-Gracia (2002); Gracia et al. (2003, 2008) and Rubio and Simón (2007).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 97

Página 141 de 632




Unknown






Unknown.


Casas-Sainz, A. & Cortés-Gracia, A. (2002): Cenozoic landscape development within the Central Iberian Chain, Spain. Geomorphology, 44: 19-46.

Cortés, A.L. (1999): Evolución tectónica reciente de la Cordillera Ibérica, Cuenca del Ebro y Pirineo centro-occidental. PhD Thesis, Universidad de Zaragoza (Spain). 406 p.

Cortés, A.L. & Casas, A.M. (2000): ¿Tiene el sistema de fosas de Teruel origen extensional? Revista de la Sociedad Geológica de España, 13: 445-470.


Gracia, F.J.; Gutiérrez, F.; Gutiérrez, M.; Rubio, J.C. & Simón, J.L. (2008): Discussion of 'Tectonic subsidence v. erosional lowering in a controversial intramontane depression: the Jiloca basin (Iberian Chain, Spain)'. Geological Magazine, 145: 591-597.




Olivé, A. & Gutiérrez, M. (1983) Geomorfología. In: Mapa geológico de España, E 1:50000, Monreal del Campo (516). Instituto Geológico y Minero de España, Madrid. p. 40-44 + map.



Simón, J.L. (1983): Tectónica y neotectónica del sistema de fosas de Teruel. Teruel, 69: 21-97.





References

Variability





ES407

Bueña earthquake September 14th, 1972

-1.2683, 40.6967

Magnitude 3.8 Instituto Geográfico

Nacional

Spatial correlation. The epicentre is on the fault trace, as noted by Gracia et al. (2003).

613

Página 142 de 632



Página 143 de 632



ID: ES408 Fault Name: Rubielos de la Cérida

Segment Name:







Average Strike(º): 173 ± 20 OD Compiler's measurement, based on the cartography by Gutiérrez et al. (2008). The range accounts for the different orientations of the fault traces within the system.

Dip (º): 75 60-90 EJ To the compiler, the narrowness of the graben suggests that the faults may merge into a subvertical fault at depth, with overall down-to-the-W displacement. In an outcrop, one of the main fault strands dips 75-80 degrees to the W (Gutiérrez et al., 2008).


Sense of Movement: N LD e.g. Gutiérrez et al. (2008).

Length (km): 9.7 OD Compiler's measurement of end-to-end distance of the whole graben, based on the cartography by Gutiérrez et al. (2008). Individual fault strands are up to ca. 3.2 km long.

Min Depth (km): 0 LD Several fault strands crop out at the surface (e.g. Gutiérrez et al., 2008).


Width (km): 15.5 AR

Area (km²): 150.63 ER


43070 yr BP ± 1200 yr LD 14C age (+/- 1-sigma range) of the youngest colluvial deposits affected by a fault strand in an artificial outcrop (Gutiérrez et al., 2008, Fig. 13).


0.050 LD Gutiérrez et al. (2008) estimated a vertical slip rate of ca. 0.05 m/ky for a fault strand (assuming that it equals the sedimentation rate on the hanging wall) from 2.1 m of sediment thickness accumulated since 43,070 +/-1200 14C yr BP (1-sigma range).




0.05 0.05-0.06 EJ Compiler's calculation, taking into account the vertical slip rate of ca. 0.05 m/yr (Gutiérrez et al., 2008) and the assumed range of fault dips.


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Narrow graben formed by a set of subparallel valleys bounded by fault scarps, which offset Upper Pleistocene and maybe even Holocene colluvial deposits.

As described by Gutiérrez et al. (2008). The fault system was previously studied by Capote et al. (1981) and Gutiérrez et al. (1983a,b).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 98

Página 144 de 632




Unknown


Unknown






Unknown.


Capote, R.; Gutiérrez, M.; Hernández, A. & Olivé, A. (1981): Movimientos recientes en la Fosa del Jiloca (Cordillera Ibérica). In: Actas de la V Reunión del Grupo Español de Trabajo del Cuaternario, Sevilla (Spain), p. 245–257.

Gutiérrez, M., Peña, J.L., Rodríguez, J. & Simón, J.L. (1983a): Criterios geomorfológicos aplicados al estudio de la neotectónica en áreas continentales (ejemplos en la Cadena Ibérica, Depresión del Ebro y Pirineos). In: Actas de las primeras jornadas sobre neotectónica y su aplicación al análisis de riesgos de emplazamientos energéticos e industriales. Junta de Energía Nuclear, Madrid, p. 158–213.

Gutiérrez, M., Peña, J.L. & Simón, J.L. (1983b): Los valles tectónicos recientes de Rubielos de la Cérida (Teruel). In: Actas de la VI Reunión Nacional Grupo Español de Trabajo del Cuaternario, Vigo-Santiago de Compostela (Spain), p. 449–459.









References

Variability



Página 145 de 632



ID: ES409 Fault Name: Valdecebro

Segment Name:

Location X: -1.04373257






Average Strike(º): 098 078-107 OD Compiler's measurement of the strands along the main trace, based on the cartographies by Godoy et al. (1983) and Moissenet (1983). Other nearby faults with smaller displacements and diverse strikes were mapped by Peña et al. (1981) and Moissenet (1983).



Sense of Movement: N LD Moissenet (1980, 1983); Peña et al. (1981); Gutiérrez (1998); Gutiérrez et al. (2008).

Length (km): 4.1 OD Compiler's measurement of end-to-end distance of the main trace, based on the cartographies by Godoy et al. (1983) and Moissenet (1983). To the SE, other fault traces with smaller displacements were mapped by Peña et al. (1981) and Moissenet (1983).

Min Depth (km): 0 LD The fault crops out at the surface (Moissenet, 1980, 1983; Peña et al., 1981; Gutiérrez, 1998; Gutiérrez et al., 2008).


Width (km): 17.3 AR



Pleistocene LD Moissenet (1983); Gutiérrez et al. (2008).


0.040 LD Minimum vertical slip rate (Gutiérrez, 1998; Gutiérrez et al., 2008), from a vertical offset of 150 m since the Early Pliocene.






Unknown

Identification


Quaternary Activity

Variability Source

Comment

Linear mountain front. Uplifted Lower Pliocene planation surface and faulted Pleistocene pediment deposits.

As reviewed by Gutiérrez et al. (2008). Previous work by Moissenet (1980, 1983); Peña et al. (1981); Godoy et al. (1983); Gutiérrez (1998) and Arlegui et al. (2005).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 99

Página 146 de 632




Unknown


Unknown






Unknown.



Godoy, A.; Olivé, A. & Moissenet, E. (1983) Cartografía. In: Mapa geológico de España, E: 1:50000, Teruel (567). Instituto Geológico y Minero de España, Madrid.

Gutiérrez, F. (1998) Fenómenos de subsidencia por disolución de formaciones evaporíticas en las fosas neógenas de Teruel y Calatayud. PhD Thesis, Universidad de Zaragoza (Spain). 569 p.

Gutiérrez, F.; Gutiérrez, M.; Gracia, F.J.; McCalpin, J.P.; Lucha, P. & Guerrero, J. (2008) Plio-Quaternary extensional seismotectonics and drainage network development in the central sector of the Iberian Chain (NE Spain). Geomorphology, 102, 21-42.




Peña, J.L.; Sánchez, M. & Simón, J.L. (1981) Algunos aspectos de la tectónica cuaternaria en el margen oriental de la fosa de Alfambra-Teruel. Teruel, 66: 31-48.






References

Variability



Página 147 de 632



ID: ES410 Fault Name: Villar del Salz

Segment Name:







Average Strike(º): 275 OD Compiler's measurement, based on the geomorphological cartographies by Simón-Gómez (1989) and Gracia et al. (2003), and the geological cartography by Olivé et al. (1983).



Sense of Movement: N LD e.g. Simón-Gómez (1989); Gracia et al. (2003); Rubio and Simón (2007) and Gutiérrez et al. (2008).

Length (km): 5.8 OD Compiler's measurement of end-to-end distance, based on the geomorphological cartographies by Simón-Gómez (1989) and Gracia et al. (2003), and the geological cartography by Olivé et al. (1983).

Min Depth (km): 0 LD The fault crops out at the surface (e.g. Simón-Gómez, 1989; Gracia et al., 2003; Rubio and Simón, 2007; Gutiérrez et al., 2008).


Width (km): 17.3 AR

Area (km²): 100.46 ER


Pleistocene LD As reviewed by Gutiérrez et al. (2008), based on Gracia et al. (1987, 2003) and Gracia (1990).


0.030 0.01-0.05 EJ Unknown. The assumed range expresses the slip rates of other faults in the region with comparable geomorphic expression.




0.03 0.01-0.06 EJ Unknown. The assumed range expresses the slip rates of other faults in the region with comparable geomorphic expression.


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Linear fault scarp. Quaternary alluvial fans with 1) normal faults with metre-scale throws, 2) extensional gashes and 3) anomalous dips in the proximity of the fault scarp.

Simón-Gómez (1989); Gracia (1990); Gracia et al. (2003) and Gutiérrez et al. (2008). Also mapped, e.g., by Rubio and Simón (2007).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 100

Página 148 de 632




Unknown


Unknown






Unknown.




Gracia, F.J.; Gutiérrez, M. & Sancho, C. (1987): Las costras calcáreas pliocuaternarias de Villafranca (Fosa de Calamocha-Teruel). Actas VII Reun. sobre Cuaternario. AEQUA. Santander, p. 279–282.

Gutiérrez, F.; Gutiérrez, M.; Gracia, F.J.; McCalpin, J.P.; Lucha, P. & Guerrero, J. (2008) Plio-Quaternary extensional seismotectonics and drainage network development in the central sector of the Iberian Chain (NE Spain). Geomorphology, 102, 21-42.


Olivé, A.; Hernández, A.; Pardo, G., Villena, J. & Moissenet, É. (1983) Cartografía. In: Mapa geológico de España, E 1:50000, Monreal del Campo (516). Instituto Geológico y Minero de España, Madrid. p. 40-44 + map.



Simón-Gómez, J.L. (1989): Late Cenozoic stress field and fracturing in the Iberian Chain and Ebro Basin (Spain). Journal of Structural Geology, 11: 285-294.





References

Variability



Página 149 de 632



ID: ES411 Fault Name: Aldehuela

Segment Name:







Average Strike(º): 194 ± 10 OD Compiler's measurement, based on the cartographies by Moissenet (1980) and Godoy et al. (1983). The range accounts for the sinuosity of the fault trace.



Sense of Movement: N LD e.g. Moissenet (1980) and Gutiérrez et al. (2008).

Length (km): 3.7 OD Compiler's measurement of end-to-end distance, based on the cartographies by Moissenet (1980) and Godoy et al. (1983).

Min Depth (km): 0 LD The fault crops out at the surface (e.g. Godoy et al., 1983; Moissenet, 1983).


Width (km): 17.3 AR



Plio-Quaternary

LD Gutiérrez et al. (2008) and references therein. The vertical Plio-Quaternary offset exceeds several tens of meters (Moissenet, 1983; Gutiérrez et al., 2008).


0.010 EJ Compiler's estimate, based on ca. 30 m of vertical throw of deposits from the terminal Pliocene (Moissenet, 1983, Fig. IV.1.16), which may be Quaternary, according to the new convention. Their assumed age is 2.6 million years (base of the Quaternary).




0.01 0.01-0.02 EJ Compiler's estimate, taking into account the vertical slip rate of ca. 0.01 m/ky and the assumed range of fault dips.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Faulted alluvial fan deposits with cumulative wedge outs and angular unconformities.

As reviewed by Gutiérrez et al. (2008). Previous work by Adrover et al. (1978); Moissenet (1980, 1982, 1983, 1989); Simón (1983) and Arlegui et al. (2005).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 101

Página 150 de 632




Unknown






Unknown.



Adrover, R.; Mein, P. & Moissenet, É. (1978): Nuevos datos sobre la edad de las formaciones continentales neógenas de los alrededores de Teruel. Estudios Geológicos, 34: 205-214.

Godoy, A.; Ramírez, J.I.; Moissenet, É. & Olivé, A. (1983): Cartografía. In: Mapa geológico de España, E: 1:50000, La Puebla de Valverde (590). Instituto Geológico y Minero de España, Madrid.



Moissenet, É. (1982): Le Villafranchien de la région de Teruel (Espagne), stratigraphie-déformations-milieux. In: Actes du Colloque "Le Villafranchien méditerranéen", p. 229–253. Lille (France).


Moissenet, É. (1989): L'age et les deformations des terrases alluviales du Fosse de Teruel. II Reunión del Cuaternario Ibérico. Madrid, p. 267–279.


Simón, J.L. (1983): Tectónica y neotectónica del sistema de fosas de Teruel. Teruel 69: 21-97.





References

Variability



Página 151 de 632



ID: ES412 Fault Name: Concud

Segment Name:

Location X: -1.208

Location Y: 40.441

Name of Compiler(s): Lafuente, P., Simón, J.L., Arlegui, L.E. and Liesa, C.L.

Filiation: Zaragoza University



Average Strike(º): 130 113-170 OD Field and cartography measurements.

Dip (º): 68 ± 3 OD Field measurements.

Rake (º): -75 ± 17 OD Field measurements.

Sense of Movement: N OD

Length (km): 14.5 ± 1 km LD From cartography (Lafuente et al., 2010)

Min Depth (km): 0 EJ


Width (km): 16.2 AR

Area (km²): 234.58 AR


15.6 ky ± 1 ky LD River terrace affected by a minor branch fault of the Concud fault (Lafuente et al., 2010). Discussion by Gutiérrez et al. (2011) attributes the most likely cause of deformation to a landslide or collapse structure.


0.216 0.066-0.310 LD Values for the whole activity period: 240m/3.6 Ma, for Pleistocene: 36m/116-169 ky, best estimate: 36m/169 ky (Simón et al., 2005; Lafuente et al., 2010). Gutiérrez et al. (2011) discuss these displacement and age values; SR might be higher.


0.058 0.018-0.084 AR Relationship between NSR and rake


0.225 0.069-0.323 AR From vertical slip rate, considering fault dip and rake.


1.9 LD Lafuente et al. (2011). Gutiérrez et al. (2011) consider this value an overestimation when considering the length of the fault and because the measurement was taken close to the tip of the fault.


6-7 in 81 ka > 4 in 72 ka OD Los Baños trench (Lafuente et al., 2010). For the same site Gutiérrez et al. (2008) interpreted a minimum of 4 events in the las 72 ka (cf. Gutiérrez et al., 2011)


OD No evidences.

Identification


Quaternary Activity

Variability Source

Comment

Fault-generated mountain front, triangular facets, deformed fluvial terraces, drainage pattern partially controlled by fault, non-incised alluvial fans, geomorphic indices

Values of geomorphic indices, together with qualitative features of the escarpment and piedmont landscape, indicate at least a moderate activity of the fault ( Lafuente et al., 2008).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 102

Página 152 de 632






7300 6700-7900 LD Los Baños trench (Lafuente et al., 2010). For the same site Gutiérrez et al. (2011) estimates for the same time period a RI of 9900 yrs considering just 4 events (cf. Gutiérrez et al., 2011). From Wesnousky'86 approach results 4790 yrs.


15300 15000-15600 LD Based on the age of a faulted terrace exposed at N420-A226 road cut and attributed by Lafuente et al. (2010) to the Concud Fault. Gutiérrez et al. (2011) points out a non-tectonic origin, that would imply a date of the last event older than 15 ka.


Gutiérrez F., Gutiérrez M., Gracia F.J., McCalpin J.P., Lucha P., Guerrero J. (2008) Plio-Quaternary extensional seismotectonics and drainage network development in the central sector of the IberianChain (NE Spain). Geomorphology 102:21–42

Gutiérrez, F., Lucha, P., Guerrero, J., Gutiérrez, M. and Carbonel, D. (2011) Discussion on the article "Paleoseismological analysis of an intraplate extensional structure: the Concud fault" (Iberian Chain, Eastern Spain)" by P. Lafuente, L.E. Arlegui, C.L. Liesa, and J.L. Simón (Int J Earth Sci), Internationa Journal of Earth Sciences, DOI 10.1007/s00531-011-0660-4


Lafuente, P., Lamelas, T., Soriano, M.A. (2008). Caracterización morfotectónica de la actividad de la falla de Concud (Cordillera Ibérica, Teruel). Geo-Temas, 10: 1027-1030.

Lafuente, P., Arlegui, L.E., Liesa, C.L., Simón, J.L. (2010): Paleoseismological analysis of an intraplate extensional structure: the Concud fault (Iberian Chain, eastern Spain). International Journal of Earth Sciences. DOI 10.1007/s00531-010-0542-1

Lafuente, P., Arlegui, L.E., Liesa, C.L., Simón, J.L. (2010): Nuevo estudio paleosismológico en el sector central de la falla de Concud (Fosa del Jiloca, Teruel): resultados preliminares. Resúmenes de la 1ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Sigüenza, España, 2010: 67-70.


Simón, J.L., Lafuente, P., Arlegui, L.E., Liesa, C.L., Soriano, M.A. (2005): Caracterización paleosísmica preliminar de la falla de Concud (fosa del Jiloca, Teruel). Geogaceta, 38: 63-66.

Stirling, M., Rhoades, D., Berryman, K. (2002): Comparison of Earthquake Scaling Relations Derived from Data of the Instrumental and Preinstrumental Era. Bulletin of the Seismological Society of America, 92 (2): 812-830.




References

Variability



Página 153 de 632



ID: ES413 Fault Name: Vicort

Segment Name:



Name of Compiler(s): Gutiérrez, F.

Filiation: University of Zaragoza



Average Strike(º): 315 ± 10 OD Based on detailed morpho-structural map produced by the compiler at 1:10,000 scale

Dip (º): 70 ± 15 OD Estimated from fault contact observed at the margin of transverse drainage

Rake (º): -90 EJ


Length (km): 15.5 OD Measured on detailed morphostructural map



Width (km): 16.0 AR

Area (km²): 247.42 AR


Quaternary OD Presumably, late Pleistocene


0.105 0.01-0.2 EJ




0.112 0.01-0.21 AR From VSR, dip and rake.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Controls prominent mountain front with conspicuous triangular facets up to 230 m high. In the hanging-wall, antithetic secondary fault expressed as upslope-facing scarp on alluvial fan surfaces. GPR profile shows faulted young (Holocene?)

Master fault at the SW margin of the Río Grío Graben. Juxtaposes Plio-Quaternary alluvial fan deposits, more than 90 m thick, against Paleozoic rocks.



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 103

Página 154 de 632








Unknown


Gutiérrez, F.; Lucha, P. and Jordá, L. (2009). The Río Grío depression (Iberian Range, NE Spain). Neotectonic graben vs. fluvial valley. En: Pérez-López, R.; Grützner, C.; Lario, J.; Reicherter, K. y Silva, P. (Eds.). Archeoseismology and Palaeoseismology in the Alpine-Himalayan collisional zone. 1st INQUA-IGCP-567 International Workshop on Earthquake Archaeology and Palaeoseismology, Baelo Claudia, Spain, 43-46.



Stirling, M.; Rhoades, D. & Berryman, K. (2002) Comparison of earthquake scaling relations derived from data of the instrumental and preinstrumental era. Bulletin of the Seismological Society of America, 92, 812-830.





References

Variability



Página 155 de 632



ID: ES414 Fault Name: Modorra

Segment Name:








Dip (º): 70 ± 15 OD Preferred based on dip of faults measured in the area

Rake (º): -90 EJ

Sense of Movement: N

Length (km): 5.9 OD Measured on detailed morpho-structural map



Width (km): 16.0 AR





0.105 0.01-0.2 EJ






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Controls prominent mountain front with conspicuous triangular facets up to 140 m high. Separated from the Vicort Fault by a transverse graben (gap) controlled by cross faults. Different seismogenic segments?

Juxtaposes Plio-Quaternary alluvial fan deposits against Paleozoic rocks. In the hanging-wall, sympathetic fault expressed as downslope-facing scarp on alluvial fan surfaces.



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 104

Página 156 de 632








Unknown


Gutiérrez, F.; Lucha, P. and Jordá, L. (2009). The Río Grío depression (Iberian Range, NE Spain). Neotectonic graben vs. fluvial valley. En: Pérez-López, R.; Grützner, C.; Lario, J.; Reicherter, K. y Silva, P. (Eds.). Archeoseismology and Palaeoseismology in the Alpine-Himalayan collisional zone. 1st INQUA-IGCP-567 International Workshop on Earthquake Archaeology and Palaeoseismology, Baelo Claudia, Spain, 43-46.








References

Variability



Página 157 de 632



ID: ES415 Fault Name: Río Grío Graben (1/3)

Segment Name: Fault F3

Location X: -1.4376

Location Y: 41.407





Average Strike(º): 327 ± 10 OD Based on detailed morpho-structural map produced by the compiler at 1:10,000 scale.


Rake (º): -90 EJ





Width (km): 16.0 AR

Area (km²): 103.76 AR




0.105 0.01-0.2 EJ






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Linear front with triangular fault facets up to 60 m high. Offsets alluvial fan deposits developed in the graben depression controlled by faults F3 and F4 at their distal edge.



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 105

Página 158 de 632








Unknown


Gutiérrez, F.; Lucha, P.; Jordá, L. (2013). The Río Grío depression (Iberian Chain, NE Spain). Neotectonic graben vs. Fluvial valley. Cuaternario y Geomorfología, 27, 63-71.

Gutiérrez, F.; Lucha, P. and Jordá, L. (2009). The Río Grío depression (Iberian Range, NE Spain). Neotectonic graben vs. Fluvial valley. En: Pérez-López, R.; Grützner, C.; Lario, J.; Reicherter, K. y Silva, P. (Eds.). Archeoseismology and Palaeoseismology in the Alpine-Himalayan collisional zone. 1st INQUA-IGCP-567 International Workshop on Earthquake Archaeology and Palaeoseismology, Baelo Claudia, Spain, 43-46.








References

Variability



Página 159 de 632













Rake (º): -90 EJ





Width (km): 16.0 AR





0.105 0.01-0.2 EJ






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Triangular fault facets up to 60 m high. Small right-stepping step-over NE of Monte Blanco Peak.

Juxtaposes Plio-Quaternary alluvial fan deposits against Paleozoic rocks.



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 106

Página 160 de 632








Unknown











References

Variability



Página 161 de 632





Location X: -1.455

Location Y: 41.3985







Rake (º): -90 EJ





Width (km): 16.0 AR



Quaternary EJ No recent stratigraphic markers associated to the inferred Quaternary fault


0.105 0.01-0.2 EJ






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Mapped as active fault based on its prominent geomorphic expression; linear mountain front with truncated divides and triangular facets.

Very limited Quaternary deposits along the fault trace zone



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 107

Página 162 de 632








Unknown










References

Variability



Página 163 de 632



ID: ES599 Fault Name: Crevillente (Sector Alicante) (2/3)

Segment Name: Río Vinalopó - Torrellano

Location X: -0.597

Location Y: 38.315

Name of Compiler(s): Martin-Rojas, I., Alfaro, P., Estévez, A., García-Mayordomo, J.

Filiation: Universidad de Alicante, IGME



Average Strike(º): 270 + 3 / - 2 LD Martín-Rojas et al. (2014ab, 2015)

Dip (º): 65 40-90 EJ Dip varies along strike, probably lower than Crevillente (Sector Alicante) 1/3. Martín-Rojas et al. (2014ab, 2015)

Rake (º): 80 80-90 EJ Reverse kinematics with a minor sinistral component. Martín-Rojas et al. (2014ab, 2015)

Sense of Movement: R SR-ANT LD Anticline-sincline par (Martín-Rojas et al., 2014ab, 2015).

Length (km): 16.5 LD Martín-Rojas et al., 2014ab, 2015

Min Depth (km): 0.5 0.5-1 EJ Blind fault. Martín-Rojas et al. (2014ab, 2015)

Max Depth (km): 15.0 LD Fragile section of the fault, the fault depht is mantelic. Table 4.21 in García-Mayordomo (2005). See explanation in p. 306.

Width (km): 16.0 AR

Area (km²): 263.98 AR


Lower Pleistocene

Pleistocene LD Indirect evidence from alluvial fan relationships by Goy and Zazo (1989)


0.050 0.03-0.07 EJ Unknown. Assumed to be similar to Crevillente (Sector Alicante) 1/3, Abanilla-Río Vinalopó segment.


0.01 0.006-0.014 AR From NSR and rake. Alfaro et al. (2014ab) and Sánchez-Alzola et al. (2014) indicate 0.44-0.75 mm/yr from GPS data. Considering that the main fault kinematics is reverse, this value may be an overestimation.


0.056 0.034-0.078 AR From assumed values for VSR, dip and rake.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Apparent linear topography. Mountain front uplift linked to Lower Pleistocene alluvial fan development. Probable relationship with seismites in Early-Middle Pleistocene deposits.

Goy y Zazo (1989) in García-Mayordomo (2005) p.146; Alfaro et al. (1999); Martin-Rojas et al. (2014ab).

Geological Set: Betic Range (Alicante)

Identification Method: Geological/Geomorphological field mapping and modelling

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 119

Página 164 de 632




6.61 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset and considering 40 km length.




Unknown


Alfaro, P., Martín-Rojas, I., Estévez, A., García-Tortosa, F.J., Sánchez-Alzola, A., Borque, M.J., Rodríguez-Caderot, G., de Lacy. C., García-Armenteros, J.A., Avilés, M., Herrera-Olmo, A., Molina, S., Rosa-Cintas, S., and Gil, A.J. (2014). Red GPS de la Cuenca del Bajo Segura (Cordillera Bética Oriental). Implicaciones sobre las tasas de desplazamiento de las fallas del Bajo Segura y de Crevillente. Resúmenes de la 2ª Reunión Ibérica sobre Falls Activas y Paleosismología, Lorca, España, 205-208.

Bisbal Cervelló, L. (1984). Estudio de la distribución de intensidades sísmicas en el ámbito valenciano. Su incidencia en las obras públicas. Tesis Doctoral, Universidad de Valencia.

Garcia-Mayordomo, J. (2005). Caracterización y Análisis de la Peligrosidad Sísmica en el Sureste de España. Tesis Doctoral, Universidad Complutense de Madrid, 373 pp.

I.T.G.E. (1993). Mapa neotectónico, sismotectónico y de actividad de fallas de la Región de Murcia (escalas 1:200.000 y 1:100.000). Conserjería de Política Territorial y Obras Públicas de la Región de Murcia, 6 mapas, 99 pp. Record 65 of the data-file.

Martín-Rojas, I., Alfaro, P., and Estévez, A. (2014a). Caracterización estructural y actividad tectónica reciente de la Falla de Crevillente. Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España, 39-42.

Martín-Rojas, I., Alfaro, P., and Estévez, A. (2014b). Evolución tectónica del borde norte de la cuenca del Bajo Segura. Implicaciones en la evolución de la falla de Crevillente (sector Abanilla-Alicante). Cuaternario y Geomorfología: 28 (3-4), 85-94.

Martín-Rojas, I., Alfaro, P. and Estévez, A. (2015) 3D geometry of growth strata in a fault‑propagation fold: insights into space–time evolution of the Crevillente Fault (Abanilla‑Alicante sector), Betic Cordillera, Spain. Int J Earth Sci (Geol Rundsch) DOI 10.1007/s00531-015-1143-9

Rey, J., Fumanal, M.P., Ferrer, C., Viñals, M.J. y Yébenes, A. (1993). Correlación de las unidades morfológicas cuaternarias (dominio continental y plataforma submarina) del sector Altea-Villa Joiosa, País Valenciano, España. Cuadernos de Geografía de la Universidad de Valencia, 54, 249-267.

Sánchez-Alzola, A.,Borque, M.J., Martín-Rojas, I., García- Tortosa, F.J., Alfaro, P., Estévez, A., Molina, S., Rodríguez-Caderot, G., de Lacy, C., García-Armenteros, J.A., Avilés, M., Herrera-Olmo, A., Rosa, S. & Gil, A.J. (2014). Tasas de deformación GPS en la cuenca del Bajo Segura (Cordillera Bética oriental). Geogaceta, 54, 3-6.

Silva, P.G., Goy, J.L., Zazo, C. y Bardají T. (2003). Fault-generated mountain fronts in southeast Spain: geomorphologic assessment of tectonic and seismic activity. Geomorphology, 50, 203-225.






References

Variability



Página 165 de 632




Segment Name: Torrellano - Mar Mediterráneo

Location X: -0.155

Location Y: 38.471






Dip (º): 65 40-90 EJ Dip varies along strike, probably lower than Crevillente (Sector Alicante) 1/3. Martín-Rojas et al. (2014ab, 2015)

Rake (º): 80 90-75 EJ Reverse kinematics with a minor sinistral component. Martín-Rojas et al. (2014ab, 2015)

Sense of Movement: R SR-ANT LD Anticline-sincline par, clearly reverse onshore (Martín-Rojas et al., 2014ab, 2015). Contrastingly, in offshore studies it is classified as a normal fault (ITGE, 1994) (cf. García-Mayordomo, 2005, p.153, for discussion).

Length (km): 40.0 14-60 EJ 14 km is the length of the inferred trace onshore (Martín-Rojas et al, 2014ab, 2015). Considering its offshore extension length reaches at least 40 km and it could be much longer (García Mayordomo, 2005).

Min Depth (km): 0.5 0-1 km EJ Blind fault. Martín-Rojas et al. (2014ab, 2015)

Max Depth (km): 15.0 LD Fragile section of the fault, the fault depht is mantelic. Table 4.21 in García-Mayordomo (2005). See explanation in p. 306.

Width (km): 16.0 AR

Area (km²): 639.96 AR


Pleistocene PlioQuaternary - Pleistocene

LD According to ITGE (1994) the offshore fault is sealed by Plio-Quaternary deposits (G.-Mayordomo (2005), p.153). Martin-Rojas et al. (2014b) describes Thyrrenian terraces affected by the fault based on Goy et al. (1993). Well located deep seismicity.


0.050 0.03-0.07 EJ Unknown. Assumed to be similar to Crevillente (Sector Alicante) 1/3, Abanilla-Río Vinalopó segment.




0.056 0.034-0.078 AR From assumed values for VSR, dip and rake.


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Uplifted and tilted Thyrrenian marine terraces. Likely association to seismites. Very likely association to seismicity (see associated seismicity)

García-Mayordomo (2005), p.153. Alfaro et al. (1999). Goy et al. (1993), Martin-Rojas et al. (2014ab, 2015).

Geological Set: Betic Range (Alicante and offshore)

Identification Method: Trace inferred from Geological/Geomorphological mapping, modelling and by spatial association to seismic hypocentres (offshore extension).

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 120

Página 166 de 632




Unknown


Unknown


6.97 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset and considering 40 km length.




Unknown


Alfaro, P., Estévez, A., Moretti, M. y Soria, J.M. (1999). Structures sédimentaires de déformation interprétés comme séismites dans le Quaternaire du bassin du Bas Segura (Cordillère bétique orientale). C.R. Acad. Sci. Paris, 328, 17-22.



Goy, J.L., Zazo C., Bardaji T., Somoza L., Causse C., Hillaire-Marcel, C. (1993). Elements d'une chronostratigraphie du Tyrrhenien des regions d'Alicante-Murcia, Sud-Est de l'Espagne. Geodinamica Acta 6 (2): 103-119.

I.T.G.E. (1994). Mapa Geológico de la Plataforma Continental Española y Zonas Adyacentes a escala 1:200.000. Hoja nº 72-73, Elche-Alicante.









References

Variability





ES600

Seismic cluster in Alicante onshore-

offshore area

1981 onwards

mbLg=1.7-4.9 IGN catalogue from 1985

to 2002

Relationship of focal depht and tectonic

structure

Along and close to inferred fault-trace a number of events located at dephts 12-27km (ERZ<=2 km) are associated to current fault activity as it is the only tectonic structure that could reach that depth in the area (G-M, 2005, p. 272-273, fig.4.17).

678

Página 167 de 632




Yébenes, A., Alfaro, P., Delgado, J., Estévez, A. y Soria, J.M. (2002). Sea cliffs resulting from late Miocene extensional tectonics: the Serra Gelada case study (Betic Cordillera, Spain). Geomorphology, 42, 197-211.


Página 168 de 632



ID: ES601 Fault Name: Crevillente (Sector Murcia) (1/3)

Segment Name: La Cañada - Campo Coy

Location X: -1.93566944


Name of Compiler(s): García-Mayordomo, J., Martínez-Díaz, J.J. and Martín Banda, R.

Filiation: IGME and UCM



Average Strike(º): 252 + 7 / - 5 OD Based on cartographic trace of the fault provided by J.J. Martínez-Díaz (Pers. Com.)

Dip (º): 90 LD To apply right hand rule dip is considered towards N

Rake (º): 30 EJ Sinistral-reverse kinematics assumed.

Sense of Movement: SR S to R LD At Present it is sinistral reverse, although in earlier times it was very different. Estévez et al., (1976); Sanz de Galdeano (1983); García-Mayordomo (2005); Sanz de Galdeano and Buforn (2005); Canora Catalán (2005)

Length (km): 30.0 Segment length coincides with fault trace length. Table 3.12 in García-Mayordomo (2005)

Min Depth (km): 0 LD Outcrops at the surface

Max Depth (km): 15.0 LD Table 4.21 in García-Mayordomo (2005)

Width (km): 15.0 AR

Area (km²): 449.91 AR


Middle-Lower Pleistocene

LD García-Mayordomo (2005)


0.058 >0.058 AR Relationship between NSR, dip and 30º rake


0.1 >0.1m/ka EJ Minimum value estimated by comparison to other active faults in the area (Table 3.30 y Fig. 3.29 in García-Mayordomo, 2005)


0.115 >0.115 AR Relationship between HSR and 30º rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformed Lower-Middle Pleistocene deposits. Geomorphic anomalies (see ITGE, 1993).

ITGE (1993)

Geological Set: Betic Range (Murcia)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 115

Página 169 de 632




6.85 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset.


13771 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): slip rate represents the rate at which maximum earthquakes are released by the fault. RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown


Buforn, E. y Sanz de Galdeano, C. (2001). Focal mechanism of Mula (Murcia, Spain) earthquake of February 2, (1999). Journal of Seismology, 5, 277-280.

Canora Catalán, C. (2005). Evolución Neotéctónica de la Zona de Falla de Crevillente (Sector Occidental). Implicaciones Sismotectónicas. Tesina. Universidad Complutense de Madrid. 132 pp.

Estévez, A., López Garrido, A.C. y Sanz de Galdeano, C. (1976). Estudio de las deformaciones recientes en el sector del Negretín (Depresión de Guadix-Baza). En: Reunión sobre la Geodinámica de la Cordillera Bética y Mar de Alborán, Granada,12-14 de Mayo de 1976, Universidad de Granada, España, pp. 165-192.


I.T.G.E. (1993). Mapa neotectónico, sismotectónico y de actividad de fallas de la Región de Murcia (escalas 1:200.000 y 1:100.000). Conserjería de Política Territorial y Obras Públicas de la Región de Murcia, 6 mapas, 99 pp.

Martínez-Díaz, J.J., Rigo, A., Louis, L., Capote, R., Hernández-Enrile, J.L., Carreño, E. y Tsige, M. (2002). Caracterización geológica y sismotectónica del terremoto de Mula (febrero de 1999, Mb: 4.8) mediante la utilización de datos geológicos, sismológicos y de interferometría de RADAR (INSAR). Boletín Geológico y Minero, 113(1), 23-33.

Mezcua, J. y Lopez Arroyo, A. (1975). Ca racterísticas espacio-temporal de la serie de réplicas en Orce-Galera. En: Comunicaciones de la 1ª Asamblea Nacional de Geodesia y Geofísica, Madrid, 16-19 de Diciembre de 1974.

Sanz de Galdeano, C. (1983). Los accidentes y fracturas principales de las Cordilleras Béticas. Estudios Geológicos, 39, 157-165.

Sanz de Galdeano, C. y Buforn, E. (2005). From strike-slip to reverse reactivation: The Crevillente Fault system and seismicity in the Bullas-Mula area (Betic Cordillera, SE Spain). Geologica Acta, 3, 241-250.


Wells, D.L. y Coppersmith, K.J. (1994). New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bulletin of the Seismological Society of America, 84(4), 974-1002.




References

Variability



Página 170 de 632




Segment Name: Campo Coy - Sierra Ricote

Location X: -1.48260999

Location Y: 38.10853771






Dip (º): 90 LD To apply right hand rule criteria dip is considered towards N


Sense of Movement: SR S to R LD Quaternary period, in earlier times it was very different. Estévez et al., (1976); Sanz de Galdeano (1983); García-Mayordomo (2005); Sanz de Galdeano and Buforn (2005); Canora Catalán (2005)

Length (km): 43.7 LD Segment length coincides with fault trace length. Table 3.12 in García-Mayordomo (2005)



Width (km): 15.0 AR

Area (km²): 655.22 AR











Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformed Lower-Middle Pleistocene deposits. Geomorphic anomalies (see IGTE, 1993).

ITGE (1993)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 116

Página 171 de 632








Unknown




Estévez, A., López Garrido, A.C. y Sanz de Galdeano, C. (1976). Estudio de las deformaciones recientes en el sector del Negretín (Depresión de Guadix-Baza). En: Reunión sobre la Geodinámica de la Cordillera Bética y Mar de Alborán, Granada,12-14 de Mayo de 1976, Universidad de Granada, España, pp. 165-192.



Martínez-Díaz, J.J., Rigo, A., Louis, L., Capote, R., Hernández-Enrile, J.L., Carreño, E. y Tsige, M. (2002). Caracterización geológica y sismotectónica del terremoto de Mula (febrero de 1999, Mb: 4.8) mediante la utilización de datos geológicos, sismológicos y de interferometría de RADAR (INSAR). Boletín Geológico y Minero, 113(1), 23-33.

Mezcua, J. y Lopez Arroyo, A. (1975). Ca racterísticas espacio-temporal de la serie de réplicas en Orce-Galera. En: Comunicaciones de la 1ª Asamblea Nacional de Geodesia y Geofísica, Madrid, 16-19 de Diciembre de 1974.

Sanz de Galdeano, C. (1983). Los accidentes y fracturas principales de las Cordilleras Béticas. Estudios Geológicos, 39, 157-165.







References

Variability



Página 172 de 632




Segment Name: Sierra Ricote - Río Segura

Location X: -1.27188012

Location Y: 38.16322157






Dip (º): 90 LD To apply right hand rule criteria dip is considered towards N


Sense of Movement: SR S to R LD Quaternary period, in earlier times it was very different. Estévez et al., (1976); Sanz de Galdeano (1983); García-Mayordomo (2005); Sanz de Galdeano and Buforn (2005); Canora Catalán (2005)

Length (km): 17.8 LD Segment length coincides with fault trace length. Table 3.12 in García-Mayordomo (2005)



Width (km): 15.0 AR

Area (km²): 266.91 AR











Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformed Lower-Middle Pleistocene deposits. Geomorphic anomalies (see IGTE, 1993).

ITGE (1993)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 117

Página 173 de 632






11032 Unstated AR Considering the Maximum Earthquake Model (Wesnousky, 1986): slip rate represents the rate at which maximum earthquakes are released by the fault. RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown











References

Variability





ES603

Agrupación - Serie Sísmica de Mula

1999 MSK: VI; M: 4.8 IGN Spatial correlation, focal mechanism

García-Mayordomo, J. (2005) fig. 3.15 and p.129; Martínez-Díaz et al. 2002; Buforn y Sanz de Galdeano, 2001.

641

Página 174 de 632




Segment Name: Abanilla - Río Vinalopó

Location X: -0.752

Location Y: 38.324






Dip (º): 65 40-90 LD Dip varies along strike. Martín-Rojas et al. (2014ab, 2015)

Rake (º): 80 LD Reverse kinematics with a minor sinistral component. Martín-Rojas et al. (2014ab, 2015)

Sense of Movement: R SR - ANT LD Anticline-syncline par. Martín-Rojas et al. (2014ab, 2015)

Length (km): 30.0 LD Martín-Rojas et al. (2014ab, 2015)

Min Depth (km): 0 LD Outcrops at the surface, though it is blind in its eastern end. Martín-Rojas et al. (2014ab, 2015)


Width (km): 16.6 AR

Area (km²): 496.52 AR


Upper Pleistocene

LD ITGE (1993), Goy y Zazo (1989) in García-Mayordomo (2005) p.146. Martín-Rojas et al (2014ab,2015) argue that during the Quaternary activity migrates southwards to the Bajo Segura Fault Zone.


0.050 0.03-0.07 LD Silva et al. (2003) mountain front classification in García-Mayordomo (2005)




0.056 0.034-0.078 AR From dip, rake and VSR.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Affects Upper and Middle Pleistocene alluvial fans. Folded travertine in Abanilla village and folded alluvial fan deposits in Rambla de la Lima (N of La Murada village).

ITGE (1993, record 65), Goy y Zazo (1989) in García-Mayordomo (2005) p.146, and Martin-Rojas et al. (2014ab).

Geological Set: Betic Range (Alicante-Murcia)

Identification Method: Geological/Geomorphological field mapping and modelling

Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 118

Página 175 de 632




6.85 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw is 6.79 (6.67-6.79) according to García Mayordomo (2005) based on: SRL(30km) vs Mw and RA vs. Mw from Wells and Coppersmith (1994) and sample "All".


25625 151488-5126 AR Considering the MEM (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter. García-Mayordomo (2005) estimated previously 45-20 ky.


Unknown



Bisbal Cervelló, L. (1984). Estudio de la distribución de intensidades sísmicas en el ámbito valenciano. Su incidencia en las obras públicas. Tesis Doctoral, Universidad de Valencia.


I.T.G.E. (1993). Mapa neotectónico, sismotectónico y de actividad de fallas de la Región de Murcia (escalas 1:200.000 y 1:100.000). Conserjería de Política Territorial y Obras Públicas de la Región de Murcia, 6 mapas, 99 pp. Record 65 of the data-file.









References

Variability





ES604

Fortuna 1958 22/12/1958 -1.11667, 38.18333

MSK: VI; M: 4.0 IGN Catalogue before 2002

Spatial correlation (Weak)

García-Mayordomo, J. (2005) p.144 and fig. 317. Additionally, relatively deep earthquakes (h>16km) seem to be related to the current activity of this deep tectonic fault (p. 273).

624

ES604

Elche 1787 MSK: VI IGN Catalogue

Spatial correlation Bisbal Cervelló (1984) in García-Mayordomo, J. (2005)

625

Página 176 de 632






Página 177 de 632



ID: ES605 Fault Name: Jumilla (Sector Murcia) (1/3)

Segment Name: Calasparra - Jumilla

Location X: -1.71284157

Location Y: 38.26675464

Name of Compiler(s): García-Mayordomo, J. and Jiménez-Díaz, A.


Email: [email protected]; ajime


Average Strike(º): 053 + 15 / - 10 LD García-Mayordomo (2005), fig. 3.29.

Dip (º): 90 LD García-Mayordomo (2005) To apply right hand rule criteria dip is considered towards S

Rake (º): 30 EJ Unknown.

Sense of Movement: SR EJ García-Mayordomo (2005)

Length (km): 35.0 5-10 to 35 km LD 35 km is the total length of the segment. Note that 5-10 km is the length of single faults included in the shear zone of the segment (García-Mayordomo, 2005 -Table 3.12; Van Balen et al., 2013).

Min Depth (km): 0 LD García-Mayordomo (2005)

Max Depth (km): 11.0 LD García-Mayordomo (2005)

Width (km): 11.0 AR

Area (km²): 385.00 AR


Quaternary LD ITGE (1993) in García-Mayordomo (2005)


0.010 <0.01 EJ By comparison with other active faults in the area (Table 3.30 y Fig. 3.29 in García-Mayordomo, 2005)


0.017 <0.017 AR From NRS and 30º rake


0.02 <0.02 AR From VRS, dip and 30º rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformed Lower-Middle Pleistocene alluvial fans ITGE (1993) in García-Mayordomo (2005)



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 121

Página 178 de 632




6.40 ± 0.37 ER Mw from maximum single fault length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw is 6.01 (5.89-6.24) according to García Mayordomo (2005) based on: SRL(5-10 km) vs Mw from Wells and Coppersmith (1994) and sample "All".




Unknown



I.G.M.E. (1978b). Mapa geológico de España a escala 1/50.000. Serie MAGNA Hoja nº 819 Caudete.



Van Balen, R.T. , Forzoni, A.,Van Dam, J., available online. Active faulting and folding along Jumilla Fault Zone, northeastern Betics, Spain. Geomorphology, doi: 10.1016/j.geomorph.2013.12.001





References

Variability



Página 179 de 632




Segment Name: Jumilla - Yecla

Location X: -1.38632185

Location Y: 38.49489016

Name of Compiler(s): Van Balen, R.T., García-Mayordomo, J., Jiménez-Díaz, A. and Martín-Banda R.

Filiation: Vrije Universiteit Amsterdam, IGME and UCM

Email: R.T.van. [email protected]


Average Strike(º): 057 + 15 / - 10 LD García-Mayordomo (2005), fig. 3.29. Van Balen et al. (2013)

Dip (º): 90 LD García-Mayordomo, J. (2005). To apply right hand rule criteria dip is considered towards S


Sense of Movement: SR LD García-Mayordomo (2005) and Van Balen et al. (2013).

Length (km): 30.0 10 to 30 LD 30 km is the total length of the segment. Note that 10 km is the length of single faults included in the shear zone of the segment. García-Mayordomo (2005) Table 3.12

Min Depth (km): 0 LD García-Mayordomo (2005) and Van Balen et al. (2013).


Width (km): 11.0 AR

Area (km²): 330.00 AR


< 500 ka LD Age evidenced by numerical forward modelling of scarp degradation using a diffusion approach (Van Balen et al., 2013).




0.014 <0.014 AR From NSR and rake


0.017 <0.017 AR From VSR, dip and rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Fault scarps, drainage network, pop-up hills, lineaments Van Balen et al. (2013)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 122

Página 180 de 632




6.40 ± 0.37 ER Mw from maximum single fault length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw is 6.22 (5.94-6.5) according to García Mayordomo (2005) based on: SRL(10 km) vs Mw from Wells and Coppersmith (1994) and sample "All".




Unknown






Van Balen, R.T. , Forzoni, A.,Van Dam, J., available online. Active faulting and folding along Jumilla Fault Zone, northeastern Betics, Spain. Geomorphology, doi: 10.1016/j.geomorph.2013.12.001

Van Dam, J., Furió, M., Van Balen, R., accepted. Re-interpreting the biochronology of the La Celia and Los Gargantones mammal sites (late Miocene, Murcia, Spain). Geobios, doi: 10.1016/j.geobios.2014.03.002





References

Variability





ES606

Agrupación de Yecla

1985-2002 IGN Catalogue

Spatial correlation García-Mayordomo, J. (2005)626

Página 181 de 632




Segment Name: Yecla - Caudete


Location Y: 38.63166946






Dip (º): 90 LD García-Mayordomo, J. (2005) To apply right hand rule criteria dip is considered towards S



Length (km): 15.0 10 to 15 LD 15 km is the total length of the segment. Note that 10 km is the length of single faults included in the shear zone of the segment. García-Mayordomo (2005) Table 3.12



Width (km): 11.0 AR

Area (km²): 165.00 AR


Middle-Upper Pleistocene

LD ITGE (1993) in García-Mayordomo (2005)








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformed Middle-Upper Pleistocene alluvial fans ITGE (1993) in García-Mayordomo (2005)

Geological Set: Betic Range (Murcia-Albacete)


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 123

Página 182 de 632






16081 4480-115440 AR Considering the Maximum Earthquake Model (Wesnousky, 1986). According to relative age of the deformed deposits IR should be >>10 ka (García-Mayordomo, 2005). The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown











References

Variability





ES607

Yecla 1931 MSK: VI; M:4 IGN Catalogue

Spatial correlation (weak)

García-Mayordomo, J. (2005)627

Página 183 de 632



ID: ES608 Fault Name: Jumilla (Sector Valencia) (2/2)

Segment Name: Xátiva - Tavernes

Location X: -0.561

Location Y: 38.942






Dip (º): 90 LD García-Mayordomo (2005) To apply right hand rule criteria dip is considered towards S



Length (km): 34.8 5-10 to 30 LD 30 km is the total length of the segment. Note that 5-10 km is the length of single faults included in the shear zone of the segment. García-Mayordomo (2005) Table 3.12. Fault may extend offshore (Díaz del Río et al., 1986).



Width (km): 15.0 AR

Area (km²): 521.25 AR


Middle-Upper Pleistocene

LD Goy et al. (1987) in García-Mayordomo (2005)








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformed Middle-Upper Pleistocene alluvial fans Goy et al. (1987) in García-Mayordomo (2005)

Geological Set: Betic Range (Valencia)


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 125

Página 184 de 632








1748 AD LD This fault could have caused the historical Estubeny 1748 AD of IX (ESI-07 scale) intensity (Giner-Robles et al., 2014). This event could be its last maximum earthquake.


Díaz del Río, V., Rey, J. y Vegas, R. (1986). The Gulf of Valencia continental shelf. Marine Geology, 73, 169-179.


Giner-Robles, J.L., Silva, P.G., Rodríguez-Pascua, M.A., Pérez-López, R., Alberola Romá, A. (2014). Efectos geológicos y arqueológicos producidos por el terremoto de Estubeny de 1748 AD (SE de España). Resúmenes de la 2ª Reunión Ibérica sobre Falals Activas y Paleosismología, Lorca, España, 155-158.

Goy, J.L., Rey, J., Díaz del Río, V. y Zazo, C. (1987). Relación entre las unidades morfológicas cuaternarias del litoral y de la Plataforma intermedia-media de Valencia (España): implicaciones paleogeográficas. En: 3ª Reunión de Geología Ambiental y Ordenación del Territorio, Valencia, febrero de 1987, Universitat de Valencia, t.2, pp. 1351-1369.

Herraiz, M., De Vicente, G., Lindo-Ñaupari, R., Giner, J., Simón, J.L., González-Casado, J.M., Vadil lo, O., Rodríguez-Pascua, M.A., Cicuéndez, J.I., Casas, A., Cabañas, L., Rincón, P., Cortés, A.L., Ramírez, M. y Lucini, M. (2000). The recent (upper Miocene to Quaternary) and present tectonic stress distributions in the Iberian Peninsula. Tectonics, 19(4), 762-786.

Rodríguez-Estrella, T. (1977). Síntesis geológica del Prebético de la provincia de Alicante. II) Tectónica. Boletín geológico y Minero, LXXXVIII-IV, 273-299.





References

Variability





ES608

Xátiva 1519 Io(MSK) = VIII IGN catalogue

Spatial nearness García-Mayordomo (2005) Fig.3.19676

ES608

Tavernes 1396 Io(MSK) = IX IGN catalogue

Spatial neareness García-Mayordomo (2005) Fig.3.19677

ES608

Estubeny 1748 AD 23th March 1748

Io (MSK) = I X; IX (ESI-07

scale)

IGN, Giner-Robles et al. (2014)

Spatial nearness, aftershocks distribution

Giner-Robles et al. (2014). Also called Enguera 1748 earthquake (García-Mayordomo, 2005: Fig.3.19)

726

Página 185 de 632





Página 186 de 632



ID: ES609 Fault Name: Palomares (1/2)

Segment Name: Carboneras - Sierra de Almenara

Location X: -1.855

Location Y: 37.04





Average Strike(º): 014 + 3 / - 2 LD From García-Mayordomo (2005). To apply right hand rule criteria dip is considered towards E.

Dip (º): 90 LD García-Mayordomo (2005), table 4.21.

Rake (º): -75 EJ

Sense of Movement: N N to NS LD Bousquet, 1979; Ott d’Estevou et al., 1990; Aellen de La Chapelle, 1990; Huibregtse et al., 1998; Jonk y Biermann, 2002.

Length (km): 45.0 10 to 45-60 LD 45 km (onshore) to 60 km (onshore and offshore) is the total length of the segment. Note that 10 km is the max length of single faults included in the shear zone of the segment (10-15 width). García-Mayordomo (2005), p.185 and Table 3.12.

Min Depth (km): 0 LD Outcrops at the surface. García-Mayordomo (2005)

Max Depth (km): 8.0 LD Given value is the depth of the fragile crust. The fault depth is mantelic. García-Mayordomo (2005), table 4.21.

Width (km): 8.0 AR

Area (km²): 360.00 AR


100 ka Upper Pleistocene

LD T-III (100 ka) Thyrrenian marine terraces (Goy and Zazo, 1986) in García-Mayordomo (2005)


0.040 0.01-0.08 LD See discussion in García-Mayordomo (2005), p.182-184.


0.011 0.003-0.021 AR From NSR and -75º rake


0.041 0.010-0.083 AR From VSR, Dip and -75º rake


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformation in continental and marine deposits (see references in comments, and García-Mayordomo (2005), p. 182 for a summary)

Goy and Zazo (1986); Silva et al. (1997); Wenzens and Wenzens (1997); Stokes and Mather (2000); Booth-Rea et al. (2003); García-Mayordomo (2005)

Geological Set: Betic Range (Almería)


Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 190

Página 187 de 632




Unknown


6.40 ± 0.37 ER Mw from maximum single fault length (10 km) using Stirling et al. (2002) equation from the instrumental dataset. Mw is 6.34 (5.24-6.44) according to García Mayordomo (2005) based on: SRL(10 km) vs Mw from Wells and Coppersmith (1994) and sample "All".


10088 148449-1388 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d), for a maximum single fault length of 10 km. García-Mayordomo (2005) estimated 20,000 yrs.The occurrence of smaller, damaging earthquakes may be much shorter.


1518 AD EJ This fault could have caused the IX (MSK) intensity historical Vera earthquake.


Aellen de la Chapelle, M. (1990). Le couloir de Pulpi. En: Montenat, C. (ed.), Les Bassins néogènes du domaine Bétique oriental (Espagne), Documents et Travaux de l’Institut Geologique Albert de Lapparent, 12-13, 195-196.

Booth-Rea, G., Azañón, J.M., García-Dueñas, V. y Augier, R. (2003). Uppermost Tortonian to Quaternary depocentre migration related with segmentation of the strike-slip Palomares Fault Zone. C. R. Geoscience, 335, 751-761.

Bousquet, J.C. (1979). Quaternary strike-slip faults in southeastern Spain. Tectonophysics, 52, 277-286.


Goy, J.L. y Zazo, C. (1986). Síntesis of the Quaternary in the Almeria litoral neotectonic activity and its morphological features, Western Betics, Spain. Tectonophysics, 130, 259-270.

Huibregtse, P., van Alebeek, H., Zaal, M. y Biermann, C. (1998). Paleostress analysis of the northern Nijar and southern Vera basins: constraints for the Neogene displacement history of major strike-slip faults in the Betic Cordilleras, SE Spain. Tectonophysics, 300, 79-101.

I.G.M.E. (1982a). Mapa geológico de la plataforma continental española y zonas adyacentes. Escala 1/200.000. Hoja nº 84-85 Almería-Garrucha; Chella-Los Genoveses.

I.T.G.E. (1990). Mapa Geológico de la Plataforma Continental Española y Zonas Adyacentes a escala 1:200.000. Hoja nº 79-79E, Murcia.Jonk, R. y Biermann, C. (2002). Deformation in Neogene sediments of the Sorbas and Vera Basins (SE Spain): constraints on simple shear deformation and rigid body rotation along major strike-slip faults. Journal of Structural Geology, 24, 963-977.

Ott d’Estevou, Ph. Y Montenat, C. (1990). Le bassin de Sorbas-Tabernas. En: Montenat, C. (ed.), Les Bassins néogènes du domaine Bétique oriental (Espagne), Documents et Travaux de l’Institut Geologique Albert de Lapparent, 12-13, 287-301.

Silva, P.G. (1994). Evolución geodinámica de la Depresión del Guadalentín desde el Mioceno Superior hasta la actualidad: Neotectónica y Geomorfología. Tesis Doctoral, Universidad Complutense de Madrid, 642 pp.

Silva, P.G., Goy, J.L., Zazo, C., Lario, J. y Bardají, T. (1997). Paleoseismic indications along ‘aseismic’ fault segments in the Guadalentín Depression (SE Spain). Journal of Geodynamics, 24, 1-4, 105-115.

Slemmons, D.B. (1982). Determination of design earthquake magnitudes for microzonation. En: Proceedings of the 3rd International Earthquake Microzonation Conference, Seatle, Washington, v.1, 119-130.




References

Variability





ES609

Vera (Almeria) 1518 MSK: IX IGN Spatial correlation (weak)

Additionaly, earthquakes hypocenters at dephts corresponding to the lower crust (h>13 km) in the area could be related to the Palomares Fault Zone, as this is a deep tectonic structure. García-Mayordomo, J. (2005), fig. 4.23, p.294 and 297.

629

Página 188 de 632




Stokes, M. y Mather, A.E. (2003). Tectonic origin and evolution of a transverse drainage: the Río Almanzora, Betic Cordillera, Southeast Spain. Geomorphology, 50, 59-81.

Villamor, P. y Berryman, K. (1999). La tasa de deslizamiento de una falla como aproximación de primer orden en las estimaciones de peligrosidad sísmica. 1er Congreso Nacional de Ingeniería Sísmica, Murcia, I, 153-163.


Wenzens, E. y Wenzens, G. (1997). The influence of tectonics, sea-level fluctuations and river capture on the Quaternary morphogenesis of the semi-arid Pulpi Basin (southeast Spain). Catena, 30, 283-293.


Página 189 de 632



ID: ES610 Fault Name: Palomares (2/2)

Segment Name: Sierra de Almenara - Sierra de Hinojar

Location X: -1.73936299

Location Y: 37.44305338

Name of Compiler(s): García-Mayordomo, J., Martín-Banda, R.




Average Strike(º): 037 + 15 / - 10 LD Northern termination of Palomares Fault Zone, strike varies from N-S to NE-SW and ENE-WSW. García-Mayordomo (2005), p. 169. Cartographic trace of the fault has been revised in 10/2013 (Martín-Banda, Pers. Com.).

Dip (º): 90 LD García-Mayordomo (2005) table 4.21. To apply right hand rule dip is considered towards E and S.

Rake (º): -75 EJ

Sense of Movement: N N to NS EJ García-Mayordomo (2005).

Length (km): 25.0 ± 1 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a) after reviewing the cartographic trace in 10/2013 (Martín-Banda, Pers. Com.).

Min Depth (km): 0 LD Outcrops at the surface (García-Mayordomo, 2005).


Width (km): 8.0 AR

Area (km²): 240.00 AR


Lower-Middle Pleistocene

LD Silva (1994) in García-Mayordomo (2005) p. 169.


0.040 <0.05 m/ka LD By comparison to other active faults in the area (Tables 3.12 and 3.13 and Fig. 3.29 in García-Mayordomo, 2005)


0.011 0.003-0.021 AR From NSR and -75º rake


0.041 0.010-0.083 AR From VSR, dip and -75º rake


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformation in Lower-Middle Pleistocene alluvial fans (Silva, 1994).

Silva (1994) in García-Mayordomo (2005) p. 169.



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 191

Página 190 de 632




Unknown






Unknown










References

Variability



Página 191 de 632



ID: ES614 Fault Name: Carrascoy (2/2)

Segment Name: Northeast (El Palmar-Los Ramos)

Location X: -1.131

Location Y: 37.931

Name of Compiler(s): García-Mayordomo, J., Martín-Banda, R., Insua-Arévalo, J.M.




Average Strike(º): 050 ±5 LD Silva (1994), Silva et al. (2003), Martín-Banda et al (2014a,b)

Dip (º): 85 85-90 LD Subvertical. Silva (1994), Silva et al. (2003), Martín-Banda et al (2014a,b)

Rake (º): 20 LD García-Mayordomo (2005) estimation, p. 168, based on Silva (1994), Silva et al. (2003), Sanz de Galdeano et al (1998).

Sense of Movement: SR S to SR LD Silva (1994), Martín-Banda et al (2014a,b)

Length (km): 13.0 ±2 LD Martín-Banda et al (2014a,b)

Min Depth (km): 0 LD Outcrops at the surface. Silva (1994), Silva et al. (2003), Martín-Banda et al (2014a,b)

Max Depth (km): 12.0 LD Given value is the depth of the fragile crust. The fault depth reaches de lower crust. García-Mayordomo (2005), table 4.21.

Width (km): 12.0 AR

Area (km²): 156.60 AR


Upper Pleistocene

Holocene LD Very likely Holocene, to be confirmed by absolute dating methods. Martín-Banda et al (2014b)


0.200 LD García-Mayordomo (2005), p.168, estimation based on Silva (1994), Silva et al. (2003), Sanz de Galdeano et al (1998).






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Fault scarp affecting Upper Pleistocene alluvial fans, very likely Holocene.

Baena et al. (1993), Silva (1994), Silva et al. (2003), Martín-Banda et al (2014b)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 132

Página 192 de 632




6.51 ± 0.37 LD Magnitude from length using Stirling et al (2002) equation derived from the instrumental dataset.




Unknown (On going work, contact the compilers for more information)


Baena et al. (1993) in: ITGE (1993a): Mapa Neotectónico, Sismotectónico y de Actividad de Fallas de la Región de Murcia (Escalas 1:200.000 y 1:100.000) and ITGE (1993b): Fichero de Fallas del Mapa Neotectónico, Sismotectónico y de Actividad de Fallas de la Región de Murcia (Escalas 1:200.000 y 1:100.000).


Martín-Banda, R., J. García-Mayordomo, J.M. Insua-Arévalo, A.E. Salazar-Rincón, E. Rodríguez-Escudero, J.A. Álvarez-Gómez, J.J. Martínez-Díaz, A. Medialdea, M.J. Herrero (2014a) Potencial sismogénico del segmento SO de la Falla de Carrascoy, Cordillera Bética (SE de España). Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España (2014a), 31-34 pp.

Martín-Banda, J.M. Insua-Arévalo, J. García-Mayordomo, A.E. Salazar-Rincón, E. Rodríguez-Escudero, J.A. Álvarez-Gómez, J.J. Martínez-Díaz (2014b) Evidencias de deformación sinestral inversa en el segmento NE de la Falla de Carrascoy (Murcia, España). Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España (2014b), 27-30 pp.

Martín-Banda, R., J. García-Mayordomo, J.M. Insua-Arévalo, A.E. Salazar-Rincón, E. Rodríguez-Escudero, J.A. Álvarez-Gómez, A. Medialdea, M.J. Herrero (2015). Quaternary activity and seismogenic potential of the SW segment of the Carrascoy Fault Zone: new insights on the Eastern Betic Shear Zone (SE Spain). Tectonics (submitted).

Sanz de Galdeano, C., López-Garrido, A.C. y García-Tortosa, F.J. (1998). Nuevos datos para la estimación de los valores de levantamiento desde el Tortoniense Superior a la actualidad en la parte centro-occidental de la Sierra de Carrascoy (provincia de Murcia). Geogaceta, 23, 139- 142.








References

Variability



Página 193 de 632



ID: ES615 Fault Name: Carrascoy (1/2)

Segment Name: Southwest (Algezares-Casas Nuevas fault)

Location X: -1.322

Location Y: 37.877





Average Strike(º): 065 ±5 LD Martín-Banda et al (2014a,b)

Dip (º): 30 ±10 LD Measured in outcrop. Martín-Banda et al (2014a,b)

Rake (º): 90 90-80 LD Measured in outcrop. Martín-Banda et al (2014a,b)

Sense of Movement: R R to RS LD Since Middle Pleistocene (c. 209 ka) the activity progressively migrates northwards from the Nor-Carrascoy fault to the Algezares-Casas Nuevas fault, that shows an almost pure reverse kinematics. Martín-Banda et al (2014a,b).

Length (km): 23.0 LD Martín-Banda et al (2014a,b).

Min Depth (km): 0 LD Fault trace is mostly blind along strike, but it has been observed at road cuts as well as in trenches dug for paleoseismological investigation. Martín-Banda et al (2014a,b).

Max Depth (km): 12.0 LD Given value is the depth of the fragile crust. The fault depth reaches de lower crust. García-Mayordomo (2005), table 4.21.

Width (km): 24.0 AR

Area (km²): 552.00 AR


Holocene LD Radiocarbon and OSL dating at paleoseismic trenches (Martín-Banda et al, 2014a,b).


0.185 0.145-0.225 AR From NSR obtained in Martín-Banda et al (2014a,b). García-Mayordomo (2005), p.168, based on Silva (1994), Silva et al. (2003) and Sanz de Galdeano et al (1998) estimated previously 0.2 m/ky.


0 AR Pure reverse kinematics. García-Mayordomo (2005), p.168, based on Silva (1994), Silva et al. (2003) and Sanz de Galdeano et al (1998) estimated previously 0.5 m/ky.


0.37 ±0.08 LD From direct measurements at trenches and absolute dating of deposits (Martín-Banda et al, 2014a,b). García-Mayordomo (2005), p.168, based on Silva (1994), Silva et al. (2003) and Sanz de Galdeano et al (1998) estimated previously 0.54 m/ky.


1.19 ±0.14 LD On going work (Martín-Banda et al, 2015)


2 in 6.9±1.8 ky

2-1 LD On going work (Martín-Banda et al, 2015).

Identification


Quaternary Activity

Variability Source

Comment

Fault scarp in Upper Pleistocene and Holocene alluvial fans. The Nor-Carrascoy fault also shows Quaternary activity, but since 209 ka progressively migrates to the Algezares-Casas Nuevas fault.

Baena et al. (1993); Silva (1994); Silva et al. (2003); Martín-Banda et al (2014a,b).


Identification Method: Geological/Geomorphological field mapping and paleoseismic work.

Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 131

Página 194 de 632




EJ


6.74 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw from rupture area or seismic moment results 6.7±0.1 (On going work in Martín-Banda et al., 2015).


2389 10940-547 AR Considering MEM (Wesnousky,1986):RI = Mo f(Mw±d)/Mo f(SR±d). On going work in M-Banda et al. (2015) estimates 2.3-4.6 ky with a mean 3.3±0.7 ky. Previous estimate was 6 ky (G-M, 2005). The occurrence of smaller, damaging earthquakes may be much shorter.


c. 2730 BP 4.8-2.7 ka LD On going work in Martin-Banda et al. (2015)




Martín-Banda, R., J. García-Mayordomo, J.M. Insua-Arévalo, A.E. Salazar-Rincón, E. Rodríguez-Escudero, J.A. Álvarez-Gómez, J.J. Martínez-Díaz, A. Medialdea, M.J. Herrero (2014a) Potencial sismogénico del segmento SO de la Falla de Carrascoy, Cordillera Bética (SE de España). Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España (2014a), 31-34 pp.

Martín-Banda, J.M. Insua-Arévalo, J. García-Mayordomo, A.E. Salazar-Rincón, E. Rodríguez-Escudero, J.A. Álvarez-Gómez, J.J. Martínez-Díaz (2014b) Evidencias de deformación sinestral inversa en el segmento NE de la Falla de Carrascoy (Murcia, España). Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España (2014b), 27-30 pp.

Martín-Banda, R., J. García-Mayordomo, J.M. Insua-Arévalo, A.E. Salazar-Rincón, E. Rodríguez-Escudero, J.A. Álvarez-Gómez, A. Medialdea, M.J. Herrero (2015). Quaternary activity and seismogenic potential of the SW segment of the Carrascoy Fault Zone: new insights on the Eastern Betic Shear Zone (SE Spain). Tectonics (submitted).

Sanz de Galdeano, C., López-Garrido, A.C. y García-Tortosa, F.J. (1998). Nuevos datos para la estimación de los valores de levantamiento desde el Tortoniense Superior a la actualidad en la parte centro-occidental de la Sierra de Carrascoy (provincia de Murcia). Geogaceta, 23, 139- 142.








References

Variability





ES615

Sangonera 1946 MSK: VI; M: 4.2 IGN Catalogue

Spatial correlation (very likely)

García-Mayordomo, J. (2005) p.174 and fig. 3.21.

632

Página 195 de 632



ID: ES616 Fault Name: Torrevieja

Segment Name:

Location X: -0.75265354

Location Y: 38.07742277

Name of Compiler(s): García-Mayordomo, J., Perea, H., Alfaro, P., Martín-Banda, R.

Filiation: IGME, ICM-CSIC, UA, IGME



Average Strike(º): 116 LD The strike of the fault changes from 130º (onshore) to 090º (offshore)

Dip (º): 80 80-90 LD Based on sparker profiles in Perea et al. (2012). Dip is to the west (onshore) and to the south (offshore)

Rake (º): 135 EJ

Sense of Movement: RD LD Alfaro et al., 2012; Perea et al., 2012. Previous work interpreted the fault as dextral until Quaternary (Montenat et al., 1990) and normal from Middle Pleistocene (García-Mayordomo, 2005: p.166). The fault zone also shows Quaternary active folding.

Length (km): 22.0 LD The onshore length of the fault is 13 km and its offshore extension is 9 km. Folds are associated to the main fault onshore and offshore.

Min Depth (km): 0 LD Outcrops at surface. Offsets sea floor (Perea et al., 2012)

Max Depth (km): 12.0 8-12 LD Given value is seismogenic depth estimated for the fault itself (see table 4.21 in García-Mayordomo (2005). Seismogenic depth of the Cartagena crustal block is 8 km (see table 4.19 and figs. 4.25-4.27 in

Width (km): 12.2 AR

Area (km²): 268.07 AR


<20 ka 20 ka -Present LD Perea et al., 2012.


0.075 <0.075 LD From differences in elevation of the Pliocene between La Mata anticline and Cabo Cervera syncline. García-Mayordomo (2005) based on Taboada et al. (1993). Given value is an overestimation.


0.076 AR Assuming 135º Rake (reverse-dextral).


0.11 >0.075 AR Assuming 135º Rake (reverse-dextral). Net slip rate has to be larger than VSR (0.075)


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformation on Thyrrenian marine terraces and marine Quaternary sediments reaching to the sea floor as seen in sparker marine profiles.

Somoza, 1989; Perea et al., 2012.

Geological Set: Betic Range (Internal Zones), Alicante (onshore and off

Identification Method: Geological/Geomorphological field mapping and marine geophysical research

Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 133

Página 196 de 632




Unknown


6.73 ± 0.37 ER Mw from total length using Stirling et al. (2002) equation derived from the instrumental dataset.


15531 81756-4327 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). García-Mayordomo (2005) estimated 10,000-30,000 yrs. The occurrence of smaller, damaging earthquakes may be much shorter.


1829 AD LD The Torrevieja 1829 AD event is chiefly related to the Bajo Segura Fault, but it could be also related to Torrevieja, San Miguel de Salinas faults or ruptures of coupled segments of Bajo Segura Fault (García-Mayordomo y Martínez-Díaz, 2006).


Alfaro, P., Delgado, J., Estévez, A. y López-Casado, C. (2001). Paleoliquefaction in the Bajo Segura basin (eastern Betic Cordillera). Acta Geologica Hispanica, 36(3-4), 233-244.

Alfaro, P., Delgado, J., A. Estévez, Soria, J.M. y Yébenes, A. (2002a). Onshore and offshorecompressional tectonics in the eastern Betic Cordillera (SE Spain). Marine Geology, 186, 337-349.

Alfaro, P., Andreu, J.M., J. Delgado, Estévez, A., Soria, J.M. y Teixido, T. (2002b). Quaternary deformation of the Bajo Segura blind fault (eastern Betic Cordillera, Spain) revealed by high resolution reflection profiling. Geological Magazine, 139(3), 331-341.

Alfaro, A., Bartolomé, R., Borque, M.J., Estévez, A., García-Mayordomo, J., García-Tortosa, F.J., Gil, A., Gràcia, E., Lo Iacono, C., Perea, H. (2012): The Bajo Segura Fault Zone: Active blind thrusting in the Eastern Betic Cordillera (SE Spain). Journal of Iberian

Geology, 38(1): 271-284.


García-Mayordomo, J. y Martínez-Díaz, J.J. (2006) Caracterización sísmica del Anticlinorio del Bajo Segura (Alicante): Fallas del Bajo Segura, Torrevieja y San Miguel de Salinas. Geogaceta, 40, 19-22.




References

Variability





ES616

Agrupación del Bajo Segura-

Torrevieja

1000-2010 11 events of I=VII since year

1000

IGN Spatial correlation (strong)

García-Mayordomo (2005), p. 173628

ES616

Orihuela 1960 MSK: VI; M: 4.4 IGN Catalogue


ES616

Torrevieja 1829 21/03/1829 -0,6833; 38,0833

I(MSK)=X; Mw=6,8

Spatial correlation The Torrevieja event is chiefly related to the Bajo Segura Fault, but it could be also related to Torrevieja, San Miguel de Salinas faults or ruptures of coupled segments of Bajo Segura Fault (García-Mayordomo y Martínez-Díaz, 2006; Perea et al., 2012).

662

Página 197 de 632



Perea, H., Gràcia, E., Alfaro, P., Bartolomé, R., Lo Iacono, C., Moreno, X., Masana, E., and EVENT-SHELF Team: Quaternary active tectonic structures in the offshore Bajo Segura basin (SE Iberian Peninsula – Mediterranean Sea), Natural Hazards and Earth System Science, 12: 3151-3168, doi:10.5194/nhess-12-3151-2012, 2012.


Somoza, L. (1989). El Cuaternario litoral entre Cabo de Palos y Guardamar del Segura (Murcia-Alicante). Evolución geodinámica en relación con las variaciones del nivel del mar. Tesis Doctoral, Universidad Complutense de Madrid, 352 pp.


Taboada, A., Bousquet, J.C. y Philip, H. (1993). Coseismic elastic models of folds above blindthrusts in the Betic Cordilleras (spain) and evaluation of seismic hazard. Tectonophysics, 220,223-241.




Página 198 de 632



ID: ES617 Fault Name: San Miguel de Salinas

Segment Name:

Location X: -0.85842997

Location Y: 38.05589966

Name of Compiler(s): García-Mayordomo, J., Perea, H., Alfaro, P., Martín-Banda, R.

Filiation: IGME, ICM-CSIC, UA, IGME



Average Strike(º): 125 LD The strike of the fault changes from 130º (onshore) to 118º (offshore)

Dip (º): 80 80-90 EJ Assumed similar to Torrevieja Fault. Dip is to the southwest (onshore and offshore).

Rake (º): 135 EJ

Sense of Movement: RD LD Alfaro et al., 2012; Perea et al., 2012. Previous work interpreted the fault as dextral until Quaternary (Montenat et al., 1990) and normal from Middle Pleistocene (García-Mayordomo, 2005: p.166). The fault zone also shows Quaternary active folding.

Length (km): 30.5 LD The onshore length of the fault is 18.7 km and its offshore extension is 11.8 km. Folds are associated to the main fault onshore and offshore.

Min Depth (km): 0 EJ Outcrops at surface


Width (km): 12.2 AR

Area (km²): 371.65 AR


<135 ka <20 ka LD Fault offsets horizon H2 dated 135 ka (relative) and likely H1 horizon dated as 20 ka (last glacial maximum). See Perea et al. (2012)


0.300 0.50-0.10 LD From differences in elevation of the Pliocene between Torremendo y Cueva Blanca anticlines and Torrevieja syncline. García-Mayordomo (2005) based on Taboada et al. (1993). Given value may be an overestimation.


0.31 0.508-0.102 AR Assuming 135º Rake (dextral-reverse)


0.43 >0.3 AR Assuming 135º Rake (reverse-dextral). Net slip rate has to be larger than VSR (0.3)


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformation on Thyrrenian marine terraces (80-100 ka), and offsetting of horizons H2 and probably H1 dated in 135 and 20 ka, respectively, as shown in marine geophysical profiles.

Somoza, 1989; Perea et al., 2012

Geological Set: Betic Range (Internal Zones), Alicante (onshore and off

Identification Method: Geological/Geomorphological field mapping and marine geophysical research

Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 134

Página 199 de 632




Unknown


6.86 ± 0.37 ER Mw from total length using Stirling et al. (2002) equation derived from the instrumental dataset.


4565 23483-1272 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). García-Mayordomo (2005) estimated 8,000-10,000 yrs. The occurrence of smaller, damaging earthquakes may be much shorter.








Geology, 38(1): 271-284.





Somoza, L. (1989). El Cuaternario litoral entre Cabo de Palos y Guardamar del Segura (Murcia-Alicante). Evolución geodinámica en




References

Variability





ES617


Torrevieja


1000



ES617

Torrevieja 1829 21/03/1829 -0,6833; 38,0833

I(MSK)=X; Mw=6,8

Spatial correlation The Torrevieja event is chiefly related to the Bajo Segura Fault, but it could be also related to Torrevieja, San Miguel de Salinas faults or ruptures of coupled segments of Bajo Segura Fault (García-Mayordomo y Martínez-Díaz, 2006; Perea et al., 2012).

663

Página 200 de 632



relación con las variaciones del nivel del mar. Tesis Doctoral, Universidad Complutense de Madrid, 352 pp.






Página 201 de 632



ID: ES618 Fault Name: Bajo Segura (1/3)

Segment Name: Hurchillo (West Bajo Segura)



Name of Compiler(s): García-Mayordomo, J., Martín-Banda, R., Alfaro, P.

Filiation: IGME, UCM, UA



Average Strike(º): 083 + 10 / - 7 LD Alfaro et al. (2012)

Dip (º): 60 60-30 EJ See Alfaro et al. (2012). Dip is crucial for the estimation of the seismogenic potential of this fault.


Sense of Movement: R R-ANT LD Blind fault. See Taboada et al. (1993) and Alfaro et al. (2002) for different models of the subsurface structure of the fault.

Length (km): 10.0 LD Alfaro et al. (2012)

Min Depth (km): 1 0.5-1 LD Blind fault (Alfaro et al. 2002, 2012)

Max Depth (km): 12.0 LD Given value is seismogenic depth. Fault depth reaches upper crust. Table 4.21 in García-Mayordomo (2005).

Width (km): 12.7 AR

Area (km²): 127.02 127-220 AR 220 km^2 results from considering 30º dip (Alfaro et al. 2012)


Upper Pleistocene-Holocene


LD Alfaro et al. (2002, 2012)


0.300 0.3-0.2 LD Considering 606 m of accumulated uplift since 2000 or 3000 ka (base of the Rojales Formation) (see Alfaro et al., 2012)


0 EJ Pure reverse slip is assumed


0.4 ± 0.11 LD Best estimation is an average between values resulting from 60-30º dip and 2000-3000 ka age of the marker. Variation showed is for the average value. Possible NSR values range 0.23 to 0.61 m/ky (see Alfaro et al., 2012, 2014).


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformation in Upper Pleistocene to Holocene sediments inferred from seismic reflection lines.

Inferred from seismic reflection lines and field observations (Alfaro et al., 2002, 2012)


Identification Method: Geological/Geomorphological field mapping and geophysics (seismic reflection lines).

Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 135

Página 202 de 632




6.40 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. Alfaro et al. (2012) obtain a Mw 6.7 (6.6-6.8) using Stirling et al (2002) equation Mw f (Area) for the Censored Instrumental Dataset.


2931 14508-640 AR Considering the Maximum Earthquake Model and dip 60. Alfaro et al. (2012) preferred estimation is 6600 after considering dip 30 to 60. García Mayordomo (2005) estimated 1700-6000 yrs.The occurrence of smaller, damaging earthquakes may be much shorter.







Alfaro, P.; Bartolomé, R.; Borque, M.J.; Estévez, A.; García-Mayordomo, J.; García-Tortosa, F.J.; Gil, A.; Gràcia, E.; Lo Iacono, C.; Perea H. (2012). The Bajo Segura Fault Zone: Active blind thrusting in the Eastern Betic Cordillera (SE Spain). Journal of Iberian Geology,

38(1): 271-284.



Sánchez-Alzola, A.,Borque, M.J., Martín-Rojas, I., García- Tortosa, F.J., Alfaro, P., Estévez, A., Molina, S., Rodríguez-Caderot, G., de Lacy, C., García-Armenteros, J.A., Avilés, M., Herrera-Olmo, A., Rosa, S. & Gil, A.J. (2014). Tasas de deformación GPS en la cuenca




References

Variability





ES618

Orihuela 1960 MSK: VI; M: 4.4 IGN Catalogue


ES618


Torrevieja


1000



ES618

Torrevieja 1829 21/03/1829 -0,6833; 38,0833

I(MSK)=X; Mw=6,8

Spatial correlation The Torrevieja event is chiefly related to the Bajo Segura Fault, but it could be also related to Torrevieja, San Miguel de Salinas faults or ruptures of coupled segments of Bajo Segura Fault (García-Mayordomo y Martínez-Díaz, 2006).

664

Página 203 de 632



del Bajo Segura (Cordillera Bética oriental). Geogaceta, 54, 3-6.






Página 204 de 632




Segment Name: Benejúzar (Central Bajo Segura)














Width (km): 12.7 AR







0.225 0.14-0.31 LD Considering 406 m of accumulated uplift since 2000 or 3000 ka (base of the Rojales Formation), the VSR value varies between 0.2 and 0.14 (see Alfaro et al., 2012). Estimations from geodetics (Sánchez-Alzola et al., 2014) for this segment draw 0.31 mm/yr.




0.385 0.16-0.61 LD Alfaro et al. (2014) estimates 0.61 mm/yr for this segment based on shortening from geodetics (Sánchez-Alzola et al., 2014) assuming dip 30º and pure reverse. Preferred estimation here is the average from the range VSR 0.14-0.31 and dip 30-60.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 136

Página 205 de 632






2769 10934-487 AR Considering the Maximum Earthquake Model and dip 60. Alfaro et al. (2012) preferred estimation is 9600 after considering dip 30 to 60. García Mayordomo (2005) estimated 2000-9000 yrs.The occurrence of smaller, damaging earthquakes may be much shorter.








38(1): 271-284.









References

Variability





ES619

Orihuela 1960 MSK: VII; M: 4.4 IGN Catalogue


ES619

Torrevieja 1829 21/03/1829 -0,6833; 38,0833

I(MSK)=X; Mw=6,8


665

Página 206 de 632







Página 207 de 632




Segment Name: Guardamar (East Bajo Segura onshore)














Width (km): 12.7 AR







0.125 0.10-0.15 LD Considering 306 m of accumulated uplift since 2000 or 3000 ka (base of the Rojales Formation), the VSR value varies between 0.15 and 0.10 (see Alfaro et al., 2012). Estimations from geodetics (Sánchez-Alzola et al., 2014) draw 0.14 mm/yr.


0 EJ Pure reverse slip is assumed.


0.21 0.12-0.30 LD Alfaro et al. (2014) estimates 0.28 mm/yr based on shortening from geodetics (Sánchez-Añzola et al., 2014) assuming dip 30º and pure reverse. Preferred estimation here is the average from the range VSR 0.10-0.15 and dip 30-60.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 137

Página 208 de 632






5337 33525-1041 AR Considering the Maximum Earthquake Model and dip 60. Alfaro et al. (2012) preferred estimation is 12,900 after considering dip 30 to 60. García Mayordomo (2005) estimated 3000-10,000 yrs.The occurrence of smaller, damaging earthquakes may be much shorter.








38(1): 271-284.












References

Variability





ES620

Torrevieja 1829 21/03/1829 -0,6833; 38,0833

I(MSK)=X; Mw=6,8


666

Página 209 de 632




Página 210 de 632



ID: ES621 Fault Name: Bajo Segura (complete onshore)

Segment Name: Complete fault length onshore












Min Depth (km): 1 0.5-1 LD Blind fault (Alfaro et al. 2002)


Width (km): 12.7 AR





LD Alfaro et al. (2002, 2012).


0.220 0.1-0.30 m/ka LD Maximum uplift rates for Hurchillo, Benejuzar and Guardamar anticlines (García-Mayordomo (2005) based on Taboada et al. (1993).




0.33 ± 0.08 LD Average value from Hurchillo, Benejuzar and Guardamar segments. Alfaro et al. (2012) estimated 0.20 to 0.40 m/ka García-Mayordomo (2005) estimated 0.35 to 0.12 m/ka.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment



Geological Set: Betic Range (Alicante and offshore)


Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 138

Página 211 de 632






15713 74444-3524 AR Considering the Maximum Earthquake Model and dip 60. Alfaro et al. (2012) preferred estimation is 10,000 after considering dip 30 to 60. García Mayordomo (2005) estimated 6000-10,000 yrs.The occurrence of smaller, damaging earthquakes may be much shorter.








38(1): 271-284.












References

Variability





ES621

Torrevieja 1829 21/03/1829 -0,6833; 38,0833

I(MSK)=X; Mw=6,8


667

Página 212 de 632



Página 213 de 632



ID: ES622 Fault Name: Muro de Alcoy (o de Mariola)

Segment Name: Muro de Alcoy

Location X: -0.44513963

Location Y: 38.74554248





Average Strike(º): 335 308º to 15º LD Fault trace is curved, basically three trends: NW-SE, NNW-SSE and NE-SW. Average trend is N25W (335º) García-Mayordomo (1998). Cartography also in Pierson d’Autrey (1987) and Goy et al. (1989).

Dip (º): 60 ± 10 LD García-Mayordomo (1998)

Rake (º): -90 LD See next comment.

Sense of Movement: N N to ND LD At the central part (N-S trend) is pure normal and at the southern part (NW-SE trend) is normal-dextral. Striae are very clear on the fault-plane in both cases. At the northern part is difficult to observe either the fault scarp and striae.

Length (km): 6.0 >6 km LD 6 km is a minimum estimation García-Mayordomo (1998). Cartography also in Pierson d’Autrey (1987) and Goy et al. (1989).

Min Depth (km): 0 0 LD Fault plane developed on Cretaceous and Jurassic limestone rock outcrops along Sierra Mariola eastern mountain front.

Max Depth (km): 15.0 - 11 / - 4 LD Max depth matches with 90%percentile of seismicity distribution and with the bottom of the upper crust. Other possibilities for max depth are: a)Fragile-ductile transition at 11 km, b) bottom of Mesozoic cover

Width (km): 17.3 AR Calculated automatically.

Area (km²): 103.92 AR Calculated automatically from minimum length, dip, and max depth.


Quaternary Pliocene to Upper Pleistocene

LD García-Mayordomo (1998) from MAGNA maps. No absolute dates available


0.200 0.1-0.2 EJ Considering 800 m and 5 ma (Pliocene).




0.231 0.115-0.231 AR From VSR, dip and rake


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Fault controls a sharp and very straight mountain front, > 800 m offset, travertine terrace tilted towards fault plane, anomalous jumps on longitudinal profiles of streams running perpendicular to fault trace (continues in brief comment)

(continues) Plio-Quaternary adn Quaternary alluvial fans show anomalous steep slopes and some a deformed shape (García-Mayordomo, 1998).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 143

Página 214 de 632




Unknown


Unknown


6.19 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. This is a minimum Mw. Fault trace on surface could be longer than 6 km (10 to 15 km). Mw is 6 (6-6.4) using W&C (1994) Mw on Lenght and Rupture area for "All".


2995 21595-835 AR Considering the ME Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Previous estimates by Garcia-Mayordomo: 1000-17,000 yrs.The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown


García-Mayordomo, J. (1998). Riesgo Sísmico en la Cuenca de Alcoy (Alicante). Aproximación a una zonificación sísmica. Tesis del Máster de Ingeniería Geológica, Universidad Complutense de Madrid, 98 pp.

García-Mayordomo, J. (2005). Caracterización y análisis de la peligrosidad sísmica en el sureste de España. Tesis Doctoral, Universidad Complutense de Madrid, España, 379 pp.

Goy, J.L., Zazo, C., Silva, P. y Bardají, T. (1989b). Actividad neotectónica cuaternaria en la cuenca neógena de Alcoy (España). Aplicación de criterios geomorfológicos. En: El cuaternario de España y Portugal: actas de la 2ª Reunión del Cuaternario Ibérico, Madrid,25-29 de septiembre de 1989, I.T.G.E., Madrid, 1993, pp. 691-696.

Martínez-Solares JM, Mezcua J (2002) Catálogo Sísmico de la Península Ibérica (800 a.c.–1900). Instituto GeográficoNacional, monografía no. 18.

Pierson d’Autrey, L. (1987). Sedimentation et structuration synsedimentaire dans le basin Neogene d’Alcoy (Cordillères Bétiques Externes Orientales-Spagne). Tesis de la Universidad de París XI-Orsay, 314 pp.





References

Variability





ES622

Cocentaina (Alicante)

29/08/1547 -0.4333, 38.75

VII-VIII EMS IGN after Martínez Solares

and Mezcua (2002)

Possible spatial correlation, weak.

Cocentaina town is at the southern end of the fault. The earthquake could be also related to the Alcoy-Cocentaina fault, or to any other blind fault in the area.

634

ES622


09/05/1955 -0.45, 38.75 3.1 mbLg, MSK: III

IGN after Martínez Solares

and Mezcua (2002)

Possible spatial correlation

Epicenter is on fault trace, however, location error can be large (old instrumental period),

635

Página 215 de 632



ID: ES623 Fault Name: Alcoy-Cocentaina

Segment Name: Alcoy-Cocentaina


Location Y: 38.70626017





Average Strike(º): 050 ± 10 LD García-Mayordomo (1998) and Goy et al. (1989)

Dip (º): 75 ± 10 OD Field measurements unpublished.

Rake (º): 45 ± 20 OD Field measurements unpublished.

Sense of Movement: SR 0 LD Clearly Transpressive-sinistral. Development of positive flowers.

Length (km): 6.0 >6 km LD 6 km is a minimum estimation García-Mayordomo (1998). Cartography also in Pierson d’Autrey (1987) and Goy et al. (1989).

Min Depth (km): 0 0 LD Fault plane developed on Middle-Lower Pleistocene alluvial fan deposits.



Area (km²): 93.17 AR Calculated automatically from minimum length, dip, and max depth.



high LD The activity of the fault very likely reaches Upper Pleistocene due to the modifications on the drainage pattern. No absolute dating available. Goy et al. (1989) describe sinistral faulting on Lower-Middle Pleistocene alluvial fans at W Loma Redonda.


Unknown


Unknown. Horizontal slip rate would be larger than vertical.



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

The fault offsets sinistrally streams draining from Sierra Mariola, strong incision and sharp bends, abandoned canals.

Goy et al. (1989), García-Mayordomo (1998) and unpublished field measurements.



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 144

Página 216 de 632




6.19 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. This is a minimum Mw. Fault trace on surface could be longer than 6 km (10 to 15 km). Mw is 6 (6-6.4) using W&C (1994) Mw on Lenght and Rupture area for "All".




Unknown




Goy, J.L., Zazo, C., Silva, P. y Bardají, T. (1989b). Actividad neotectónica cuaternaria en la cuenca neógena de Alcoy (España). Aplicación de criterios geomorfológicos. En: El cuaternario de España y Portugal: actas de la 2ª Reunión del Cuaternario Ibérico, Madrid,25-29 de septiembre de 1989, I.T.G.E., Madrid, 1993, pp. 691-696.

Martínez-Solares JM, Mezcua J (2002) Catálogo Sísmico de la Península Ibérica (800 a.c.–1900). Instituto GeográficoNacional, monografía no. 18.






References

Variability





ES623

Alcoy (Alicante) 02/12/1620 -0.4667, 38.7

EMS: VII-VIII IGN after Martínez Solares

and Mezcua (2002)

Possible spatial correlation

636

ES623


29/08/1547 -0.4333, 38.75

VII-VIII EMS IGN after Martínez Solares

and Mezcua (2002)


Muro de Alcoy Fault is also a possible source

637

ES623

Alcoy (Alicante) 28/07/1941 -0.4667, 38.7167

MSK: III IGN after Martínez Solares

and Mezcua (2002)


Epicenter is on fault trace, however, location error can be big (old instrumental period),

638

Página 217 de 632



ID: ES624 Fault Name: Benasau

Segment Name: Benasau

Location X: -0.31998486

Location Y: 38.69076761





Average Strike(º): 300 ± 15 LD Pierson D'Autrey (1987), García-Mayordomo (1998), García-Mayordomo et al. (2002).

Dip (º): 60 LD Field observations in García-Mayordomo et al. (2002).

Rake (º): -90 ± 15 LD Commonly is 90º, could vary to 75º. Field observations in García-Mayordomo et al. (2002).

Sense of Movement: N N to DN LD Field observations in García-Mayordomo et al. (2002).

Length (km): 5.0 > 5 km (15 to 2 LD 5 km is a minimum estimation. Fault is very likely much longer (15-20 km).

Min Depth (km): 0 0 LD Fault plane is developed on Mesozoic limestones.García-Mayordomo et al. (2002).



Area (km²): 86.60 ER Calculated automatically from minimum length, dip, and max depth.


Quaternary Pleistocene to Holocene

LD Recent colluvial and paleosoil deposits. No absolute dates available. See García-Mayordomo et al. (2002).


0.200 0.10- 0.40 EJ García-Mayordomo et al. (2002) assumes 0.1 to 0.20 for similarity to other faults in the area. Other estimation is 700 m in 1.6 ma (Quaternary).


EJ Unknown. Very likely is very low.




6.4 6.4 to 5.1 LD Geometrically interpolated from outcrop to fault plane. They are very likely overestimated. García-Mayordomo et al. (2002).


>3 in Quaternary

3 to 4-5 events LD García-Mayordomo et al. (2002).

Identification


Quaternary Activity

Variability Source

Comment

Fault controls a sharp and very straight mountain front, > 700 m offset. Colluvial deposits (gravels) with intercalated organic paleosoils appear tilted towards the fault plane.

See figure 2 in García-Mayordomo et al. (2002).



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 145

Página 218 de 632




Unknown


6.69 ± 0.37 ER Mw from maximum length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw is 7 (6.6-7.4) using Wells and Coppersmith (1994) magnitude on maximum displacement relationship.




Unknown




García-Mayordomo, J., Martínez-Díaz, J.J., Arcos, A. y Blázquez, R. (2002). Estudio Preliminar de la Paleosismicidad de la Falla de Benasau (Cuenca de Alcoy, Alicante). 3ª Asamblea de Geodesia y Geofísica, Valencia 4-8 de Febrero de 2002. Memorias, Tomo I, 412-415.






References

Variability





ES624

Confrides (Alicante) 09/02/1949 -0.3, 38.7 m=3.8, I (MSK)= V

IGN Weak spatial correlationLocated 2 km east of the fault. Location error can be large (old instrumental period),

639

Página 219 de 632



ID: ES626 Fault Name: Alhama de Murcia (1/4)

Segment Name: Goñar - Lorca

Location X: -1.69655139

Location Y: 37.67875673

Name of Compiler(s): Martínez-Díaz, J.J., Ortuño Candela, M., Masana, E., García-Mayordomo, J.

Filiation: UCM, IGME, UNAM, UB



Average Strike(º): 215 ± 2 LD Martínez-Díaz et al. (2010) To apply the right hand rule dipping is considered towards the N.

Dip (º): 70 ± 10 LD Martínez-Díaz (1998), Masana et al. (2005). Dips to the North.

Rake (º): 20 ± 20 LD Inferred from striations on fault planes. Martínez-Díaz (1998) and coherent with vertical/horizontal slip rates reported for the fault. García-Mayordomo (2005) p. 123.

Sense of Movement: SR LD Oliveros, 1987; Martinez-Díaz, 1998; García-Mayordomo, 2005. p. 122

Length (km): 30.0 ± 3 LD Segment length coincides with fault trace length. García-Mayordomo (2005) Table 3.13. Martínez Díaz et al. (2010).


Max Depth (km): 12.0 LD Given value is max depth of fragile rupture (seismogenic) which for this fault is deeper that the fragile-ductile transition in the area. García-Mayordomo (2005). table 4.21. See discussion on p. 306

Width (km): 12.8 AR

Area (km²): 383.10 AR


3.25 ky Holocene LD Ortuño et al. (2012), Martínez-Díaz et al. (2012). Coherent with Silva (1994)


0.200 0.07-0.29 LD Obtained from two parallel fault branches (Ortuno et al.in prep.). Uplift rate of 0.08-0.12 m/ka since Pliocene (Silva, 1994); Mountain front classification: 0.08-0.15 m/ka in Silva et al., 2003. Discussion in García-Mayordomo (2005) p. 123


0.5 0.5-1.0 LD Ortuño et al. (2012). Martínez-Díaz et al. (2012). Echeverria et al. (2013) estimates from GPS data an upper bound horizontal slip rate of 1.5 ± 0.3 mm/yr.


0.5 0.5-1.0 LD Best estimation based on VSR=0.05 and HSR=0.07 m/ky (from Middle-Late Pleistocene markers) and dip=70. A larger NSR can be obtained considering SR from a different marker whose age is uncertain (VSR=0.29 and HSR=1 m/ka).


0.81 0.81-1.06 LD Observed at Gabarrones trench (Ortuño et al., 2012; Martínez-Díaz et al., 2012).)


at least 4 since 125

>4 LD As observed in the trenches (Ortuño et al., 2012; Martínez-Díaz et al., 2012).

Identification


Quaternary Activity

Variability Source

Comment

Geomorphic indexes, controls on alluvial fan evolution, deformation of alluvial fans, offset channels,... (Silva, 1994; Martínez-Díaz, 1998)

Silva (1994); Martínez-Díaz (1998); Martínez-Díaz et al. (2012)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 146

Página 220 de 632




Unknown


6.85 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw can varies 6.4-7 (Ortuño et al., 2012; Martínez-Díaz et al., 2012). Range of variation depends on rupture length considering 1-2 segments (Ortuño et al., 2012).


15000 15000-29000 LD Ortuño et al (2012) based on a minimum of six events in the last 174–274 ky, with a maximum recurrence interval between 15 and 29 ky for the last 59–116 ky. García-M. (2005) estimated previously 7000 yrs. Considering MEM results 3720 yrs, range:13350-518.


3250 3250-3890 LD Based on paleoseismic data from Ortuño et al. (2012)


Echeverria, A., Khazaradze, G., Asensio, E., Gárate, J., Martín Dávila, J. and Suriñach, E. (2013). Crustal deformation in eastern Betics from CuaTeNeo GPS network, Tectonophysics, 608: 600–612.



Martínez-Díaz, J.J. (1998). Neotectónica y Tectónica Activa del sector centroccidental de Murcia y Sur de Almería, Cordillera Bética (España). Tesis Doctoral, Universidad Complutense de Madrid, 466 pp.

Martínez-Díaz, J.J. (2000b). Indicios geomorfológicos indicativos de tectónica activa en el sector Lorca-Totana de la Falla de Alhama de Murcia. Boletín Geológico y Minero, 111(1), 67-76.

Martínez-Díaz, J.J. y Hernández-Enrile, J.L. (2001). Using travertine deformations to characterize paleoseismic activity along an active oblique-slip fault: the Alhama de Murcia fault (Betic Cordillera, Spain). Acta Geologica Hispanica, 36, 3-4, 297-313.

Martínez-Díaz, J.J. y Hernández-Enrile,J.L. (1999). Segmentación tectónica de la Falla de Alhama de Murcia y actividad paleosísmica




References

Variability





ES626

Lorca 1977 1977 MSK: VI; M: 4.2 IGN Catalogue

Spatial correlation See discussion and references in García-Mayordomo (2005), p. 130

646

ES626

SW Lorca Seismic Series 2000

23 to 24 August,

2000

M(mbLg)=3.4; I(MSK)=IV


Discussion in García-Mayordomo (2005), p. 130.

647

ES626

Deep events along fault trace

depth of seismicity vs. tectonic structure

Events well located at depths of ductile crust have to be related to the current activity of the fault in depht. Discussion in García-Mayordomo (2005), p. 298. Fig.4.27

648

Página 221 de 632



asociada. Contribución a la determinación de la peligrosidad sísmica en la región de Murcia. I Congreso Nacional de Ingeniería Sísmica, Murcia. Memorias Ia, 75-87.

Martínez-Díaz, J.J., Masana, E., Ortuño, M, (2010). Implications of the structure of the Alhama de Murcia Fault on its paleoseismological analysis. En: Contribución de la Geología al Análisis de la Peligrosidad Sísmica (J.M. Insua y F. Martín‐González, eds.), pp. 2‐5. Sigüenza (Guadalajara, España).

Martínez-Díaz, J.J., Masana, E. and Ortuño, M. (2012). Active tectonics of the Alhama de Murcia fault, Betic Cordillera, Spain. Journal of Iberian Geology 38(1): 253-270.

Oliveros, M.A. (1987). Estudio tectónico-cinemático de la fracturación reciente en el borde oriental y suroriental de la Sierra de Las Estancias (Murcia y Almería).Tesis de Licenciatura. Universidad Complutense de Madrid.

Ortuño, M., Masana, E., Martínez-Díaz, J, García-Meléndez, E. (2010). Limitations of the palaeo-earthquake chronology as a tool to identify simultaneous ruptures of active faults at slow deforming areas: an example from the eastern betics .In: Contribución de la Geología al Análisis de la Peligrosidad Sísmica (J.M. Insua y F. Martín‐González, eds.), pp.109‐112. Sigüenza (Guadalajara, Spain).

Ortuño, M C, Masana, E, Buylaert, J P., Canora, C., Cunha, P., García-Meléndez, E., Martínez-Díaz, J., Murrey, A., Sohbati, R. And Štěpančíková, P. (2009), Paleoseismic activity at the southern termination of Alhama de Murcia fault (Southeastern Betics, Spain): geomorphic and trenching evidence along a slow moving fault. Eos Trans. AGU, 90(52), Fall Meeting. Suppl., Abstract T21D-1851.

Ortuño, M., Masana, E., García-Meléndez, E., Martínez-Díaz, J.J., Štěpančíková,P., Cunha, P., Sohbati, R., Canora, C., Buylaert, J.P., Murray, A-S. (2012): An exceptionally long paleoseismic record of a slow-moving fault: the Alhama de Murcia fault (Eastern Betic Shear Zone, Spain). Geological Society of America Bulletin, 124(9/10): 1474–1494.

Silva, P.G., Goy, J.L., Somoza, L., Zazo, C. y Bardají, T. (1993). Landscape response to strike slip faulting linked to collisional settings: Quaternary tectonics and basin formation in the Eastern Betics, southeastern Spain. Tectonophysics, 224, 289-303









Página 222 de 632




Segment Name: Lorca - Totana

Location X: -1.50455085

Location Y: 37.77281561

Name of Compiler(s): Martínez-Díaz, J.J., García-Mayordomo, J. and Jiménez-Díaz, A.

Filiation: UCM and IGME



Average Strike(º): 238 + 5 / - 4 LD Martínez-Díaz et al. (2012)

Dip (º): 70 LD Martínez-Díaz et al. (2012). Dip is to the North

Rake (º): 18 18-75 LD Martínez-Díaz et al., 2012.

Sense of Movement: SR R to RS-SR LD Martínez-Díaz (1998) in García-Mayordomo (2005), p.123-124. Falla Norte de Lorca is mainly reverse. Falla Sur de Lorca is sinistral-reverse. See also Martínez-Díaz et al. (2012).

Length (km): 20.0 LD Martínez-Díaz et al. (2012).

Min Depth (km): 0 LD Martínez-Díaz et al. (2012).


Width (km): 12.8 AR

Area (km²): 255.40 AR


Holocene Middle Pleistocene-Holocene

LD Falla Norte de Lorca: Middle Pleistocene. Falla Sur de Lorca: Holocene,<10 ka. Martínez-Díaz y Hernández-Enrile, 1999 y 2001; Hernández-Enrile et al., 2000; Martínez-Díaz et al., 2001; Masana et al., 2004.


0.160 0.12-0.16 LD Martínez-Díaz et al. (2012). García-Mayordomo (2005) based on Masana et al. (2004) and Martínez-Díaz et al. (2003) using data from the last 30 ka.


0.21 LD Martínez-Díaz et al. (2012). García-Mayordomo (2005) based on offset channels (26.7 m in last 125 ka - Upper Pleistocene s.l.) from Martínez-Díaz et al., 2003. Echeverria et al. (2013) estimates from GPS data an upper bound of 1.5 ± 0.3 mm/yr.


0.3 0.14-0.30 EJ Martínez-Díaz et al. (2012). Based on Masana et al. (2004) and Martínez-Díaz et al. (2003), see discussion in García-Mayordomo, 2005, p.124-125.


0.45 0.43-0.45 LD From Rambla del Buitre outcrop (Martínez-Díaz and Hernández-Enrile, 1999), and considering vertical dip and 75º striae (García-Mayordomo, 2005, p.124).


5 to 8 in 26.9 ka

>=5 and <= 8 LD Based on Masana et al. (2004) paleoseismic results in García Mayordomo (2005),p. 125-126.

Identification


Quaternary Activity

Variability Source

Comment

In this segment fault trace splits in two: Falla Norte de Lorca: Changes in Guadalentin River dynamic, changes in drainage pattern, folding in Middle Pleistocene alluvial fans. Falla Sur: deformation in Upper Pleistocene alluvial fans, offset channels.

ITGE (1993), Silva (1994), Martínez-Díaz (1998), Martínez-Díaz y Hernández-Enrile (1999, 2001), Masana et al. (2004), Martínez-Díaz et al. (2003) in García-Mayordomo (2005), p.123-126; Martínez-Díaz et al. (2012).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 147

Página 223 de 632




Unknown


6.69 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw can varies 6.4-7 (Ortuño et al., 2012; Martínez-Díaz et al., 2012). Range of variation depends on rupture length considering 1-2 segments (Ortuño et al., 2012).


3500 3500 - <14000 LD Based on paleoseismic results, see Martínez-Diaz et al. (2012). García Mayordomo (2005) estimated previously 2000 yrs. Considering the MEM (Wesnousky, 1986) results 5217 yrs, range: 40126-1454 yrs.


1650 d.C. shortly before 1650

LD Based on Masana et al. (2004) paleoseismic results in García Mayordomo (2005),p. 125.





References

Variability





ES627

Lorca 1579 MSK: VIII Spatial correlation (weak)


ES627

Lorca 1674 MSK: VIII Spatial correlation (weak)


ES627

Totana 1907 1907 MSK: VII IGN Catalogue



ES627

Deep events along fault trace

IGN depth of seismicity vs. tectonic structure

Events well located at depths of ductile crust have to be related to the current activity of the fault in depht. Discussion in García-Mayordomo (2005), p. 298. Fig.4.27

652

ES627

Lorca 11 May 2011 11/05/2011 Máx Mw=5.2, Máx I

(EMS)=VII at Lorca

IGN Spatial, focal mechanism, directivity

effect

See Física de la Tierra (vol.24, 2012), Boletín Geológico y Minero (vol.123/4, 2012) and Bulletin of Earthquake Engineering (in press, 2013) special issues on the earthquake. There are also a number of special reports from IGME, IGN, IAG, IGC,

681

Página 224 de 632



Armijo, R. (1977). La zone des failles Lorca-Totana (Cordillères Béticas, Espagne). Étude tectonique et neotectonique. Thèse 3ème cycle, Paris VII, 229 pp.







Martínez-Díaz, J.J. y Hernández-Enrile,J.L. (1999). Segmentación tectónica de la Falla de Alhama de Murcia y actividad paleosísmica asociada. Contribución a la determinación de la peligrosidad sísmica en la región de Murcia. I Congreso Nacional de Ingeniería Sísmica, Murcia. Memorias Ia, 75-87.


Masana, E., Martínez-Díaz, J.J., Hernández-Enrile, J.L. y Santanach, P. (2004). Constrainingseismotectonics in a diffuse collisional plate boundary by paleoseismologic results. Apreliminary approach along the Alhama de Murcia Fault (Betic Cordillera, Ibero-Maghrebian region). Journal of Geophysical Research, 109(1).

Ortuño, M., Masana, E., García-Meléndez, E., Martínez-Díaz, J.J., Štěpančíková,P., Cunha, P., Sohbati, R., Canora, C., Buylaert, J.P., Murray, A-S. (2012): An exceptionally long paleoseismic record of a slow-moving fault: the Alhama de Murcia fault (Eastern Betic Shear Zone, Spain). Geological Society of America Bulletin, 124(9/10): 1474–1494.

Silva, P.G., Goy, J.L., Somoza, L., Zazo, C. y Bardají, T. (1993). Landscape response to strike slip faulting linked to collisional settings: Quaternary tectonics and basin formation in the Eastern Betics, southeastern Spain. Tectonophysics, 224, 289-303









Página 225 de 632




Segment Name: Totana - Alhama

Location X: -1.42364596

Location Y: 37.85213568






Dip (º): 70 LD Martínez-Díaz et al. (2012)

Rake (º): 50 75-15 EJ Assumed.

Sense of Movement: RS RS to SR LD Martinez-Díaz et al. (2010, 2012).

Length (km): 12.0 5 to 12 LD Martínez-Díaz et al. (2012). According to García-Mayordomo, J. (2005) Table 3.12., 5 km is the length of single faults in the fault zone.

Min Depth (km): 0 LD Outcrops at the surface. Martínez-Díaz et al. (2012)


Width (km): 12.8 AR

Area (km²): 153.24 AR


Middle Pleistocene

Lower to Middle Pleistocene

LD I.T.G.E., 1993; Martínez-Díaz et al. (2012)


0.050 0.03-0.07 EJ Values assumed to be the same order as in the Alhama-Alcantarilla segment.


0.045 0.045-0.063 AR From NSR (assuming rake=50 and assuming VSR are correct).


0.069 0.042-0.097 AR From assumed rake (50), dip and assumed VSR.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Very low geomorphic expression compare to Puerto Lumbreras-Lorca and Lorca-Totana segments but larger if compared to Alhama-Alcantarilla segment (Silva, 1994; Martínez-Díaz, 1998).

Silva (1994) and Martínez-Díaz (1998) in García-Mayordomo (2005), p. 126; Martínez-Díaz et al. (2012)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 148

Página 226 de 632




6.48 ± 0.37 ER Mw from maximum fault length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw is 5.89 (5.61-6.17) García Mayordomo (2005) based on: SRL (5km) vs Mw from Wells and Coppersmith (1994) and sample "All".




Unknown






Martínez-Díaz, J.J. y Hernández-Enrile, J.L. (1999). Segmentación tectónica de la Falla de Alhama de Murcia y actividad paleosísmica asociada. Contribución a la determinación de la peligrosidad sísmica en la región de Murcia. I Congreso Nacional de Ingeniería Sísmica, Murcia. Memorias Ia, 75-87.






References

Variability





ES628

Agrupación de Totana

1985-2002 IGN Catalogue

Spatial correlation (very weak)

García-Mayordomo (2005), p. 131, fig. 3.15. Additionally, few realtively deep earthquakes located along the trace may be evidence of current activity (fig. 4.27)

653

ES628

Totana 1907 MSK: VII IGN Catalogue

Spatial correlation García-Mayordomo (2005), p. 131, fig. 3.15.

654

ES628

Lorca 11 May 2011 11/05/2011 Máx Mw=5.2, Máx I

(EMS)=VII at Lorca

IGN Spatial, focal mechanism, directivity

effect

See Física de la Tierra (vol.24, 2012), Boletín Geológico y Minero (vol.123/4, 2012) and Bulletin of Earthquake Engineering (in press, 2013) special issues on the earthquake. There are also a number of special reports from IGME, IGN, IAG, IGC,

680

Página 227 de 632









Página 228 de 632




Segment Name: Alhama - Alcantarilla

Location X: -1.23109073

Location Y: 38.00316872






Dip (º): 70 LD Martínez-Díaz et al. (2012). Dips to the North.

Rake (º): 50 75-15 EJ Assumed.

Sense of Movement: RS RS to SR LD Martínez-Díaz et al. (2012)

Length (km): 25.0 17 to 25 LD Martínez-Díaz et al. (2012). According to García-Mayordomo (2005) Table 3.12, 17 km is the length of single faults in the fault zone.

Min Depth (km): 0 LD Outcrops at the surface. Martínez-Díaz et al. (2012)


Width (km): 12.8 AR

Area (km²): 319.25 AR


Middle Pleistocene

Lower to Middle Pleistocene

LD I.T.G.E. (1993); Martínez-Díaz et al. (2012)


0.050 0.03-0.07 LD Average valued from Silva et al. (2003) classification of mountain fronts in García-Mayordomo (2005), p.126. Martínez-Díaz et al. (2012) states 0.07 m/ky.


0.045 0.045-0.063 AR From NSR (assuming rake=50).


0.069 0.042-0.097 AR From assumed rake (50), dip and VSR


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Low geomorphic expression compared to Puerto Lumbreras-Lorca, Lorca-Totana and Totana-Alhama segments (Silva, 1994; Martínez-Díaz, 1998).

Silva (1994) and Martínez-Díaz (1998) in García-Mayordomo (2005), p. 126. Martinez-Díaz et al. (2010); Martínez-Díaz et al. (2012)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 149

Página 229 de 632




6.78 ± 0.37 ER Mw from maximum fault length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw is 6.51 (6.23-6.79) García Mayordomo (2005) based on: SRL (17km) vs Mw from Wells and Coppersmith (1994) and sample "All".


24944 147083-4944 AR Considering the MEM (Wesnousky, 1986): slip rate represents the rate at which maximum earthquakes are released by the fault. RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter. Previous estimation was 24000.


Unknown


García-Mayordomo, J. (2005). Caracterización y Análisis de la Peligrosidad Sísmica en el Sureste de España. Tesis Doctoral, Universidad Complutense de Madrid, 373 pp.




Martínez-Díaz, J.J. y Hernández-Enrile, J.L. (1999). Segmentación tectónica de la Falla de Alhama de Murcia y actividad paleosísmica asociada. Contribución a la determinación de la peligrosidad sísmica en la región de Murcia. I Congreso Nacional de Ingeniería Sísmica, Murcia. Memorias Ia, 75-87.






References

Variability





ES629

Agrupación de Alhama

1996 MSK: III; M: 3.5 IGN Catalogue


García-Mayordomo (2005). Additionally, few realtively deep earthquakes located along the trace may be evidence of current activity (fig. 4.27)

655

ES629

Alhama 1864 MSK: VI IGN Catalogue



ES629

Sangonera 1946 MSK: VI; M: 4.2 IGN Catalogue

Spatial correlation (very likely)

García-Mayordomo, J. (2005) p.174 and fig. 3.21.

657

Página 230 de 632












Página 231 de 632



ID: ES630 Fault Name: Carboneras (1/2)

Segment Name: Northern

Location X: -2.76389467

Location Y: 36.42757359

Name of Compiler(s): Moreno, X., Masana, E. and Gràcia, E.

Filiation: RISKNAT-UB and UTM-CSIC



Average Strike(º): 048 + 9 / - 5 LD Measured on multibeam bathymetric data (Moreno, 2010)

Dip (º): 90 ± 10 LD Calculated from seismic profiles (Moreno, 2010)

Rake (º): 10 LD Calculated from offsets of a calcrete crust dated between 130-71 ka. Dip-slip is a maximum value and with a larger uncertainty than strike-slip component (Moreno, 2010).

Sense of Movement: SR LD A predominant left-lateral strike-slip deformation with some vertical slip component was observed by P-C microstructures in trenches at La Serrata and by displacement of linear features such as gullies (Moreno, 2010; Moreno et al., 2008, 2010).

Length (km): 110.5 ± 1 EJ In our opinion, this segment most probably gathers two or more segments, but we have no conclusive evidence to place a segment limit along it. As Expert Judgement, a segment limit may occur along La Serrata, but more evidence are needed.

Min Depth (km): 0 LD Outcrops at surface (Moreno, 2010).

Max Depth (km): 11.0 LD Lower depth of the instrumental seismicity according to IGN online seismic data base (Moreno, 2010).

Width (km): 11.0 AR

Area (km²): 1215.50 AR


1190 yr BP ± 25 yr LD Calculated from a faulted and buried paleochannel observed in trenches at El Hacho site (southern part of La Serrata range) (Moreno et al., 2008, 2010). Holocene reflections are also apparently faulted in TOPAS profiles along the offshore portion.


0.040 LD Minimum long-term value obtained from multichannel seismic profiles We can't distinguish at this scale what is dip slip offset from what is lateral movement of terrains having different elevations It has much larger strike slip component than dip slip one


1.1 LD Calculated from onshore (along La Serrata range) and offset gullies offshore (Moreno, 2010; Moreno et al., 2010). Minimum value. GPS is suggesting also a 1 mm/yr order of magnitude of strike-slip rate.


1.101 LD Moreno, 2010.


1.5 0-3 LD Maximum offset estimated from buried paleochannel observed in trenches at El Hacho site (southern part of La Serrata range) (Moreno, 2010; Moreno et al., 2008).

Identification


Quaternary Activity

Variability Source

Comment

Rectilinear mountain front, offset gullies, beheaded alluvial fans, alluvial fans without drainage area, faulted and folded quaternary deposits

Moreno, 2010.



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 192

Página 232 de 632




6 LD A minimum of 6 events since the Mid Pleistocene are observed in trenches along La Serrata. However, we are most probably missing events due to the intermittent deposit aggradation and erosion of the region (Moreno, 2010; Moreno et al., 2008).


Unknown


7.39 ± 0.37 ER Mw from length using Stirling et al. (2002) equation derived from the instrumental dataset. Mw is 7.4 (± 0.3) according to W&C'94 empirical relationship between Mw and max. SRL for strike-slip faults. If considering smaller segments, Mw decreases.


1150 <13500 LD Considering a long term slip-rate of 1.3 mm/yr and a slip per event of 1.5 m (estimated in 3D trenches at El Hacho). A much longer recurrence is obtained if considering 3 events in the last 40 ka (Moreno, 2010). Considering MEM (W'86) results 3413 yrs.


<1178 BP younger than 1178 BP

OD Younger than the age of the youngest deposit affected by the fault: the buried paleochannel observed at El Hacho site (southern part of La Serrata range).


Gràcia, E., Pallas, R., Soto, J. I., Comas, M., Moreno, X., Masana, E., Santanach, P., Diez, S., García, M., and Dañobeitia, J. (2006). Active faulting offshore SE Spain (Alboran Sea): Implications for earthquake hazard assessment in the Southern Iberian Margin. Earth and Planetary Science Letters 241, 734-749.


Moreno, X., Masana, E., Gràcia, E., Bartolomé, R., and Piqué-Serra, O. (2008). Estudio paleosismológico de la Falla de Carboneras: Evidencias tierra-mar de actividad tectónica reciente. GeoTemas 10, 1035-1038.

Moreno, X. (2010). Neotectonic and Paleoseismic Onshore-Offshore integrated study of the Carboneras Fault (Eastern Betics, SE Iberia). Doctoral Thesis, Barcelona University.

Masana, E., Gràcia, E., Martínez Díaz, J.J., Moreno, X., Ortuño, M., Perea, H., Khazaradze, G., Pallàs, R., Rodés, A., Queralt, P., Coll, M, Bartolomé, R., García-Meléndez, E., Ruano, P., Stepancikova, P., Dañobeitia, J.J., Santanach, P. (2010). Characterizing the seismic potential of the Eastern Betics Shear Zone (EBSZ), a major source of earthquakes in Southeastern Iberia. En: Contribución de la Geología al Análisis de la Peligrosidad Sísmica (J.M. Insúa y F.Martín-González, eds.), pp. 101-104. IBERFAULT, Sigüenza (Guadalajara), 27-29 Octubre 2010.

Moreno, X., Masana, E., Gràcia, E., Bartolomé, R., Rodés, A., and Pallàs, R. (2010). Onshore-Offshore active tectonics along the Carboneras Fault Zone (Eastern Betic Cordilleras). In "Contribución de la Geología al Análisis de la Peligrosidad Sísmica." (J. M. Insua-Arévalo, and F. Martín-González, Eds.), pp. 105-107, Sigüenza (Guadalajara, Spain).

Reicherter, K. and Hübscher,C. (2007) Evidence for a seafloor rupture of the Carboneras Fault Zone (southern Spain): Relation to the 1522 Almería earthquake? Journal of Seismology, 11:15-16.





References

Variability





ES630

Almeria 1522 earthquake

22/09/1522 -2.40,36.58 EMS=IX; M>6.5 IGN and Reicherter

and Hübscher

(2007)

Reicherter and Hübscher (2007)

Reicherter and Hübscher (2007)727

Página 233 de 632




Página 234 de 632



ID: ES631 Fault Name: Amarguillo

Segment Name: Amarguillo

Location X: -1.51032411

Location Y: 37.77421717

Name of Compiler(s): Martinez-Diaz, J.J.

Filiation: UCM



Average Strike(º): 020 ± 4 LD Martinez -Díaz et al. (2010); IGME (1993).

Dip (º): 90 ± 5 OD Observation in the field

Rake (º): 90 60-90 EJ

Sense of Movement: R N to ND LD Martinez -Díaz et al. (2010); IGME (1993).

Length (km): 12.0 - 0.5 / + 2 EJ Based on data from Martinez -Díaz et al. (2010); IGME (1993).

Min Depth (km): 0

Max Depth (km): 8.0 EJ Inferred from data included in Martinez -Díaz et al. (2010); IGME (1993) to maintain a realistic shape factor.

Width (km): 8.0 AR



Upper Pleistocene

LD Martinez-Díaz et al. (2010); IGME (1993).


0.100 +0.1/-0.05 EJ From cartographic data of Martínez-Díaz et al. (2010) and IGME (1993).


0 EJ Pure reverse


0.1 +0.1/-0.05 EJ From cartographic data of Martínez-Díaz et al. (2010) and IGME (1993).


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Very clear surface expression, deforms alluvial fans and produce blocking and deflections in fluvial network

Martinez-Díaz et al. (2010); IGME (1993).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 150

Página 235 de 632




6.48 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 5.70 (5.5-5.8) from maximum rupture area projected on empirical relation od W&C.




Unknown



IGME (1993). Mapa Geologico de España. Hoja 954.



Source Comment



References

Variability



Página 236 de 632



ID: ES632 Fault Name: Las Viñas

Segment Name: Las Viñas

Location X: -1.70770893

Location Y: 37.68206054

Name of Compiler(s): Martínez-Díaz, J. J.

Filiation: UCM



Average Strike(º): 285 ± 3 LD Geometrical data from Martinez-Díaz, J.J. (1998; 2000)

Dip (º): 80 ± 5 LD Geometrical data from Martinez-Díaz, J.J. (1998; 2000)

Rake (º): 70 + 10 / - 20 OD

Sense of Movement: ND N to ND-DN LD From Martinez-Díaz, J.J. (1998; 2000)

Length (km): 3.5 to 5.5 LD From Martinez-Díaz, J.J. (2000)

Min Depth (km): 0 LD From Martinez-Díaz, J.J. (2000)

Max Depth (km): 5.0 EJ This is a coherent value to maintain a realistic shape factor considering that this fault do not affect the entire brittle crust.

Width (km): 5.1 AR



Upper Pleistocene

Holocene-Upper Pleistocene

LD Martinez-Díaz, J.J. (1998; 2000); IGME, 1993.


0.400 +0.1/-0.1 LD From Martinez-Díaz, J.J. (1998). Geological slip rate from Pliocene time.


0.137 0.171-0.034 AR From NSR and rake


0.4 +0.1/-0.3 EJ From data and paleoseismic descriptions in Martinez-Díaz, J.J. (1998).


0.5 +0.2/-0.1 EJ From data and paleoseismic descriptions in Martinez-Díaz, J.J. (1998).


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

The fault produce tilting on fluvial terraces and alluvial fans and the migration to the south of the Guadalentín river

Martinez-Díaz, J.J. (1998; 2000)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 151

Página 237 de 632




5.97 ± 0.37 ER To 6.15 if considering maximum length (5.5 km) and using Stirling et al (2002) equation derived from the instrumental dataset. Mw 5.50 (5.30-5.6) from Martinez-Díaz, J.J. (1998; 2000)




Unknown



Martínez-Díaz, J.J. (2000). Neotectonica Y Tectonica Activa De La Falla De Las Viñas: Influencia De Las Perturbaciones Del Campo De Esfuerzos Regional Generadas Por La Falla De Alhama De Murcia. Boletín Geológico y Minero, 111-1: 33-52.



Source Comment



References

Variability



Página 238 de 632



ID: ES633 Fault Name: Torremendo

Segment Name:



Name of Compiler(s): Alfaro, P.

Filiation: Universidad de Alicante



Average Strike(º): 079 LD Alfaro et al., 2002

Dip (º): 30 LD Alfaro et al., 2002

Rake (º):

Sense of Movement: R LD Alfaro et al., 2002

Length (km): 11.8 LD Alfaro et al., 2002

Min Depth (km): 1 LD Alfaro et al., 2002

Max Depth (km): 12.0 LD Alfaro et al., 2002

Width (km): 22.0 AR

Area (km²): 259.60 AR




LD Alfaro et al., 2002


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Deformation in Upper Pleistocene to Holocene sediments inferred from seismic reflection lines (Alfaro et al., 2002).

Inferred from seismic reflection lines (Alfaro et al., 2002); García-Mayordomo (2005), p.167.


Identification Method: Geological/Geomorphological field mapping and geophysical methods (seismic reflection lines).

Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 142

Página 239 de 632




6.47 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset.




Unknown


Alfaro, P., Andreu, J.M., J. Delgado, Estévez, A., Soria, J.M. y Teixido, T. (2002). Quaternary deformation of the Bajo Segura blind fault (eastern Betic Cordillera, Spain) revealed by high resolution reflection profiling. Geological Magazine, 139(3), 331-341.


Source Comment



References

Variability



Página 240 de 632



ID: ES635 Fault Name: Polopos fault zone (1/2)

Segment Name: North Alhamilla reverse fault


Location Y: 37.03004153

Name of Compiler(s): Giaconia, F., Booth-Rea, G., Martínez-Martínez, J.M., Azañón, J.M. and Pérez-Peña,V.

Filiation: Dpto. Geodinámica, IACT (CSIC-UGR)



Average Strike(º): 080 LD Giaconia et al. (2013)

Dip (º): 40 30-50 LD Giaconia et al. (2013)

Rake (º): 80 LD Giaconia et al. (2013)

Sense of Movement: R LD Giaconia et al. (2013)

Length (km): 17.0 LD Giaconia et al. (2013)

Min Depth (km): 0 LD Giaconia et al. (2013)


Width (km): 15.6 AR

Area (km²): 264.47 AR


Upper Pleistocene

LD This fault cut through Early Tortonian turbidites and Quaternary alluvial fans associated to the north Alhamilla mountain front (see Giaconia et al., 2012, 2013)


0.100 0.05-0.50 LD Giaconia et al. (2012 and 2013)


0.03 EJ


0.25 0.19-0.31 LD Net displacements range between 80 and 125 m in the last 400 ky (see Giaconia et al., 2013)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Scarps, deformed alluvial fans, offset channel, drainage pattern, topographic lineament, geomorphic indices.

Azañón et al. (2012); Giaconia et al. (2012); Giaconia et al. (2013);



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 194

Página 241 de 632








Unknown


Azañón, J.M., Pérez-Peña, J.V., Giaconia, F., Booth-Rea, G., Martínez-Martínez, M., Rodríguez-Peces, M.J. (2012) Active tectonics in the central and eastern Betic Cordillera through morphotectonic analysis: the case of Sierra Nevada and Sierra Alhamilla.Journal of Iberian Geology, 38(1):225-238.

Giaconia, F., Booth-Rea, G., Martínez-Martínez, J.M., Azañón, J.M., Pérez-Peña, J.V., Pérez-Romero, J., Villegas, I., 2012. Geomorphic evidence of active tectonics in the Sierra Alhamilla (eastern Betics, SE Spain). Geomorphology, 145-146:90-106. http://dx.doi.org/10.1016/j.geomorph.2011.12.043.

Giaconia, F., Booth-Rea, G., Martínez-Martínez, J.M., Azañón, J.M., Pérez-Romero, J. and Villegas, I. (2013) Mountain front migration and drainage captures related to fault segment linkage and growth: The Polopos transpressive fault zone (southeastern Betics, SE Spain). Journal of Structural Geology, 46:76-91.



Source Comment



References

Variability





ES635

Serie Sísmica de Sierra Alhamilla

1984 MSK: V; M:5.0 IGN Catalogue


Rueda et al. (1992); García-Mayordomo, J. (2005)

630

Página 242 de 632



ID: ES636 Fault Name: Polopos fault zone (2/2)

Segment Name: South Gafarillos fault

Location X: -2.15634852

Location Y: 37.03281211

Name of Compiler(s): Booth-Rea, G., Giaconia, F., Martínez-Martínez, J.M., Azañón, J.M. and Villegas, I.

Filiation: Dpto. Geodinámica, IACT (CSIC-UGR)



Average Strike(º): 095 90-120 LD Giaconia et al. (2013)

Dip (º): 80 LD Giaconia et al. (2013)

Rake (º): 135 LD Giaconia et al. (2013)

Sense of Movement: RD DR-DN LD Giaconia et al. (2013)

Length (km): 13.0 LD Giaconia et al. (2013)

Min Depth (km): 0 LD Giaconia et al. (2013)


Width (km): 10.2 AR

Area (km²): 132.01 AR


Upper Pleistocene

LD This fault cut through Early Tortonian turbidites and Quaternary alluvial fans associated to the north Alhamilla mountain front (see Giaconia et al., 2012, 2013)


0.100 LD 320 m in the last 3.2 ma (see Giaconia et al., 2013)


0.15 EJ


0.24 0.04-0.44 LD Net displacements range between 30-100 m and 144-176 m in the last 400 ky (see Giaconia et al., 2013).


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Deformed alluvial fans, channel offset, drainage pattern, topographic lineament, geomorphologic indices.

Azañón et al. (2012); Giaconia et al. (2012); Giaconia et al. (2013);



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 195

Página 243 de 632








Unknown


Azañón, J.M., Pérez-Peña, J.V., Giaconia, F., Booth-Rea, G., Martínez-Martínez, M., Rodríguez-Peces, M.J. (2012) Active tectonics in the central and eastern Betic Cordillera through morphotectonic analysis: the case of Sierra Nevada and Sierra Alhamilla.Journal of Iberian Geology, 38(1):225-238.

Giaconia, F., Booth-Rea, G., Martínez-Martínez, J.M., Azañón, J.M., Pérez-Peña, J.V., Pérez-Romero, J., Villegas, I., 2012. Geomorphic evidence of active tectonics in the Sierra Alhamilla (eastern Betics, SE Spain). Geomorphology, 145-146:90-106. http://dx.doi.org/10.1016/j.geomorph.2011.12.043.

Giaconia, F., Booth-Rea, G., Martínez-Martínez, J.M., Azañón, J.M., Pérez-Romero, J. and Villegas, I. (2013) Mountain front migration and drainage captures related to fault segment linkage and growth: The Polopos transpressive fault zone (southeastern Betics, SE Spain). Journal of Structural Geology, 46:76-91.



Source Comment



References

Variability



Página 244 de 632



ID: ES638 Fault Name: Norte de Cubillas

Segment Name:

Location X: -3.74838114


Name of Compiler(s): Sanz de Galdeano, C. and Peláez, J.A.

Filiation: I.A.C.T. and Universidad de Jaén

Email: [email protected]; japelaez@uj


Average Strike(º): 072 LD Calculated from its tips (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Dip (º): 50 ± 10 LD Rodríguez-Fernández and Sanz de Galdeano (2006), Sanz de Galdeano et al. (2012).

Rake (º): -90 LD Rodríguez-Fernández and Sanz de Galdeano (2006), Sanz de Galdeano et al. (2012).

Sense of Movement: N LD Rodríguez-Fernández and Sanz de Galdeano (2006), Sanz de Galdeano et al. (2012).

Length (km): 8.6 OD Lenght of the fault trace as observed in the field (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Min Depth (km): 0 OD

Max Depth (km): 5.0 >5 OD Estimated depth is deeper than 5 km based on seismic exploration (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Width (km): 6.5 AR



Pliocene-Quaternary

LD Rodríguez-Fernández and Sanz de Galdeano (2006), Sanz de Galdeano et al. (2012).


0.060 LD From the displacement observed in the last 5 Ma (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).




0.078 AR From VSR, dip and rake of the fault


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It has scarce geomorphic evidence This fault is mainly known from seismic profiles (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Geological Set: Betic Range (Granada)

Identification Method: Geological/Geomorphological field mapping and geophysical methods

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 215

Página 245 de 632




Unknown


6.34 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.10 (± 0.6) from the equation Mw=Mw(l) of Wells and Coppersmith (1994) for normal faults.




Unknown


Rodríguez-Fernández, J.C., Sanz de Galdeano, C. (2006): Late orogenic intramontane basin development: the Granada basin, Betics (southern Spain). Basin Research 18, 85-102. doi: 10.1111/j.1365-2117.2006.00284.x

Peláez, J.A., Sanz de Galdeano, C. y López Casado, C. (2001). Potencialidad sísmica de las fallas de la Cuenca de Granada en La Cuenca de Granada. Estructura, tectónica activa, sismicidad, geomorfología y dataciones existentes (Sanz de Galdeano, C., Peláez, J.A. y López, A.C., eds.), 158-174 (ISBN: 84-699-5561-6)

Peláez J.A., Sanz de Galdeano, C. y López Casado, C. (2001). Base de datos de fallas de la Cuenca de Granada y evaluación de su potencialidad sísmica. II Congreso Iberoamericano de Ingeniería Sísmica. 16-19 Octubre, Madrid, 2001. 22-30

Peláez, J.A., Sanz de Galdeano, C. and López Casado, C. (2003). Use of active fault data versus seismicity data in the evaluation of seismic hazard in the Granada basin (Southern Spain). Bulletin of the Seismological Society of America 93, 1670-1678

Sanz de Galdeano, C., Peláez, J.A. and López Casado, C. (2003). Seismic potential of the main active faults in the Granada Basin (southern Spain). Pure and Applied Geophysics 160, 1537-1556.

Sanz de Galdeano, C., Peláez, J.A., López Casado, C., Alfaro, P., García Tortosa, F.J., Galindo Zaldívar, J., y López Garrido, A.C. (2010). Estudios de tectónica activa en las Cuencas de Granada y Guadix-Baza (Cordillera Bética, Sur de España). En: Contribución de la Geología al Análisis de la Peligrosidad Sísmica (Insua, J.M., y Martín González, F., eds.), pp. 141-144. Sigüenza (Guadalajara, España).

Sanz de Galdeano, C., García Tortosa, F.J., Peláez, J.A., Alfaro, P., Azañón, J.M., Galindo Zaldívar, J., López Casado, C., López Garrido, A.C., Rodríguez-Fernández, J. y Ruano, P. (2012). Main active faults in the Granada and Guadix-Baza Basins (Betic Cordillera). Journal of Iberian Geology 38 (1) 2012: 209-223





References

Variability



Página 246 de 632



ID: ES639 Fault Name: E de Cubillas

Segment Name:

Location X: -3.66928311

Location Y: 37.32259647






Dip (º): 50 - 10 / + 20 LD Listric geometry (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Length (km): 5.1 LD Lenght of the fault trace as observed in the field (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).


Max Depth (km): 3.0 >3 LD Estimated depth is deeper than 3 km based on seismic exploration (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Width (km): 3.9 AR



Pliocene-Pleistocene



0.080 OD From the displacement observed in the last 5 Ma (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).






Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It has scarce geomorphic evidence Known from seismic profiles (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 216

Página 247 de 632




Unknown






Unknown







Sanz de Galdeano, C., García Tortosa, F.J., Peláez, J.A., Alfaro, P., Azañón, J.M., Galindo Zaldívar, J., López Casado, C., López Garrido, A.C., Rodríguez-Fernández, J. y Ruano, P. (2012). Main active faults in the Granada and Guadix-Baza Basins (Betic Cordillera). Journal of Iberian Geology 38 (1) 2012: 209-223Sanz de Galdeano, C., Peláez, J.A. and López Casado, C. (2003). Seismic potential of the main active faults in the Granada Basin (southern Spain). Pure and Applied Geophysics 160, 1537-1556





References

Variability



Página 248 de 632



ID: ES640 Fault Name: Oeste de Cubillas

Segment Name:

Location X: -3.69338255

Location Y: 37.25849645











Max Depth (km): 4.0 >4 LD Estimated depth is deeper than 4 km based on seismic exploration (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Width (km): 4.6 AR






0.150 OD From the displacement observed in the last 5 Ma (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).




0.173 AR From dip and rake of the fault


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It has scarce geomorphic evidence Known from seismic profiles (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 217

Página 249 de 632




Unknown






Unknown






Sanz de Galdeano, C., Peláez, J.A. and López Casado, C. (2003). Seismic potential of the main active faults in the Granada Basin (southern Spain). Pure and Applied Geophysics 160, 1537-1556







References

Variability



Página 250 de 632



ID: ES641 Fault Name: Obéilar - Pinos Puente

Segment Name:

Location X: -3.84467874

Location Y: 37.25479653






Dip (º): 75 ± 15 LD Generally the fault deeps 60-70 to the south (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Rake (º):

Sense of Movement: ND LD Normal component is predominant although there is a certain dextral strike slip component of unknown magnitude (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Max Depth (km): 10.0 > 10 LD Estimated depth is deeper than 10 km based on seismic exploration and geologic features (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Width (km): 10.4 AR








0.299 AR From NSR and -120º rake


0.598 AR From VSR, dip and -120º rake


Unknown

Identification


Quaternary Activity

Variability Source

Comment

A general and linear change of relief. This fault is also known from seismic profiles (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 218

Página 251 de 632




Unknown


Unknown


6.30 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.0 (± 0.6) from the equation Mw=Mw(l) of Wells and Coppersmith (1994) for normal faults. As a strike slip fault maximum magnitude would be 6.2 (0.2 sigma).




Unknown













References

Variability



Página 252 de 632



ID: ES643 Fault Name: Tocón-Obéilar

Segment Name:

Location X: -3.96257578

Location Y: 37.24789658





Average Strike(º): 079 LD Calculated from its tips (Rodríguez-Fernández and Sanz de Galdeano, 2006).

Dip (º): 45 + 20 LD Rodríguez-Fernández and Sanz de Galdeano (2006).

Rake (º): -90 LD Rodríguez-Fernández and Sanz de Galdeano (2006).

Sense of Movement: N LD Rodríguez-Fernández and Sanz de Galdeano (2006).

Length (km): 8.8 LD Lenght of the fault trace as observed in the field (Rodríguez-Fernández and Sanz de Galdeano, 2006).


Max Depth (km): 3.0 > 3 LD Estimated depth is deeper than 3 km based on seismic exploration (Rodríguez-Fernández and Sanz de Galdeano, 2006).

Width (km): 4.2 AR




LD Rodríguez-Fernández and Sanz de Galdeano (2006)


0.100 LD From the displacement observed in the last 5 Ma (Rodríguez-Fernández and Sanz de Galdeano, 2006).






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It has scarce geomorphic evidence This fault is mainly known from seismic profiles (Rodríguez-Fernández and Sanz de Galdeano, 2006).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 219

Página 253 de 632








Unknown












References

Variability



Página 254 de 632



ID: ES644 Fault Name: Alitaje

Segment Name:

Location X: -3.77408052

Location Y: 37.26309649







Rake (º): -90 LD (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Sense of Movement: N LD (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Max Depth (km): 5.0 > 5 LD Estimated depth is deeper than 5 km based on seismic exploration (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Width (km): 6.5 AR




LD (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).








Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It has scarce geomorphic evidence This fault is known by seismic profiles (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 220

Página 255 de 632




Unknown






Unknown













References

Variability



Página 256 de 632



ID: ES646 Fault Name: Pinos Puente

Segment Name:

Location X: -3.75728094

Location Y: 37.26329648






Dip (º): 60 ± 20 LD Listric geometry (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).


Sense of Movement: N N to ND LD (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Max Depth (km): 10.0 > 10 LD Estimated depth is deeper than 10 km based on seismicity possibly associated to the fault (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Width (km): 11.5 AR

Area (km²): 108.54 AR


Recent Quaternary

LD (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).


0.400 LD From the displacement observed in the last 5 Ma. (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).




0.462 ± 0.1 AR From dip and rake of the fault


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Spectacular scarp and many other geomorphic features. On the scarp can be seen striations with normal and normal-dextral movements. The fault has associated seismicity. It is also known by seismic profiles (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 221

Página 257 de 632




Unknown






Unknown














References

Variability



Página 258 de 632



ID: ES648 Fault Name: Pedro Ruiz

Segment Name:

Location X: -3.78348028









Sense of Movement: N LD (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Length (km): 5.9 LD (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012)


Max Depth (km): 5.0 > 5 LD Estimated depth is deeper than 5 km based on seismic exploration (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).

Width (km): 6.5 AR



Pliocene-Quaternary

OD


0.100 LD From the displacement observed in the last 5 Ma (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012)..






Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It has scarce geomorphic evidence This fault is known from seismic profiles (Rodríguez-Fernández and Sanz de Galdeano, 2006; Sanz de Galdeano et al., 2012).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 222

Página 259 de 632




Unknown






Unknown








Sanz de Galdeano, C., García Tortosa, F.J., Peláez, J.A., Alfaro, P., Azañón, J.M., Galindo Zaldívar, J., López Casado, C., López Garrido, A.C., Rodríguez-Fernández, J. y Ruano, P. (2012). Main active faults in the Granada and Guadix-Baza Basins (Betic Cordillera). Journal of Iberian Geology 38 (1) 2012: 209-223.





References

Variability



Página 260 de 632



ID: ES651 Fault Name: Atarfe

Segment Name:

Location X: -3.74358129

Location Y: 37.25549648





Average Strike(º): 134 LD Calculated from its tips (Sanz de Galdeano et al., 2012).

Dip (º): 60 ± 15 LD Listric geometry (Sanz de Galdeano et al., 2012).

Rake (º): -90 LD (Sanz de Galdeano et al., 2012).

Sense of Movement: N LD (Sanz de Galdeano et al., 2012).

Length (km): 10.3 LD Lenght of the fault trace as observed in the field (Sanz de Galdeano et al., 2012).


Max Depth (km): 10.0 > 10 LD Estimated depth is deeper than 10 km based on seismicity possibly associated to the fault and geologic features (Sanz de Galdeano et al., 2012).

Width (km): 11.5 AR

Area (km²): 118.93 AR


Recent Quaternary

LD (Sanz de Galdeano et al., 2012)


0.150 LD From the displacement observed in the last 5 Ma (Sanz de Galdeano et al., 2012).


0 LD Some striae indicate a dextral horizontal strike but it is not possible to know it importance. In any case the throw is the principal feature (Sanz de Galdeano et al., 2012).


0.173 ± 0.01 AR From dip and rake of the fault.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Well expressed scarp and minor structures related This fault has associated abundant seismicity, particularly low magnitude earthquakes. The scarp is well conserved (Sanz de Galdeano et al., 2012).



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 223

Página 261 de 632








Unknown













References

Variability



Página 262 de 632



ID: ES653 Fault Name: El Fargue-Jun

Segment Name:

Location X: -3.63190819

Location Y: 37.25026761





Average Strike(º): 138 LD Calculated from its tips (Sanz de Galdeano et al., 2012).

Dip (º): 60 ± 10 LD Listric geometry (Sanz de Galdeano et al., 2012).





Max Depth (km): 10.0 > 10 LD Estimated depth is deeper than 10 km based on seismicity possibly associated to the fault (Sanz de Galdeano et al., 2012).

Width (km): 11.5 AR

Area (km²): 135.10 AR


Pliocene-Quaternary

LD (Sanz de Galdeano et al., 2012).


0.350 LD From the displacement observed in the last 0.8 Ma. (Sanz de Galdeano et al., 2012).




0.404 AR From dip and rake of the fault.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

The scarp and the line of the fault. The scarp formed in soft Pliocene-Pleistocene sediments was conserved till its destruction to build new houses. The fault is also known from seismic profiles (Sanz de Galdeano et al., 2012).



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 224

Página 263 de 632








Unknown









Source Comment



References

Variability





ES653

Serie sísmica del 04/06/1998

04/06/1998 -3.6062, 37.1551

3.0 mbLg Geographic proximity Possible seismic series associated616

Página 264 de 632



ID: ES655 Fault Name: Escóznar

Segment Name:

Location X: -3.78828022

Location Y: 37.16469647





Average Strike(º): 330 LD Calculated from its tips (Sanz de Galdeano et al., 2010)

Dip (º): 60 LD Listric geometry based on seismic sections (Sanz de Galdeano et al., 2010)

Rake (º): -90 LD (Sanz de Galdeano et al., 2010)

Sense of Movement: N LD (Sanz de Galdeano et al., 2010)

Length (km): 9.7 LD Lenght of the fault trace as observed in the field (Sanz de Galdeano et al., 2010)


Max Depth (km): 3.0 >3 LD Estimated depth is deeper than 3 km based on geologic features (Sanz de Galdeano et al., 2010)

Width (km): 3.5 AR






0.100 LD From the displacement observed in the last 5 Ma (Sanz de Galdeano et al., 2010)






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Linear change of relief separating different types of sediments It is also known from seismic profiles (Sanz de Galdeano et al., 2010)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 225

Página 265 de 632








Unknown











References

Variability



Página 266 de 632



ID: ES656 Fault Name: Santa Fe

Segment Name:


Location Y: 37.10469639












Width (km): 11.5 AR

Area (km²): 150.11 AR











Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

A linear change of relief It is also known from seismic profiles (Sanz de Galdeano et al., 2010)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 226

Página 267 de 632








Unknown












References

Variability



Página 268 de 632



ID: ES658 Fault Name: Granada

Segment Name:


Location Y: 37.21374668





Average Strike(º): 150 LD Calculated from its tips. (Sanz de Galdeano et al., 2003, 2010, 2012)

Dip (º): 60 ± 15 LD Listric geometry based on seismic sections (Sanz de Galdeano et al., 2003, 2010, 2012)Calculated from its tips. (Sanz de Galdeano et al., 2003, 2010).

Rake (º): -90 LD

Sense of Movement: N LD (Sanz de Galdeano et al., 2003, 2010, 2012).

Length (km): 16.8 LD Lenght of the fault trace as observed in the field (Sanz de Galdeano et al., 2003, 2010, 2012).

Min Depth (km): 0 LD Sanz de Galdeano et al., 2003, 2010, 2012.

Max Depth (km): 10.0 > 10 EJ Estimated depth is deeper than 10 km based on seismicity possibly associated to the fault.

Width (km): 11.5 AR

Area (km²): 193.99 AR



>150 ka LD From TL-dating estimates >150 ka (Azañón et al., 2009 and 2013).


0.120 0.38-0.12 LD 0.38 m/ky results from 300 m displacement observed in the last 0.8 ma (Sanz de Galdeano et al., 2003). From the last 2.5 ma Sanz de Galdeano et al., 2012 estimates 0.12 m/ky. Azañón et al. (2013) estimate 0.003 m/ky.






0.056 0.48-0.07 LD Azañón et al., 2009 and 2013


8 in the last 150 ky

8-9 LD Azañón et al., 2009 and 2013


Unknown

Identification


Quaternary Activity

Variability Source

Comment

The scarp, only well conserved in some points. This fault cross the town of Granada and the scarp has been generally destroyed. To the South is better conserved. In some new constructions have been possible to see some parts of the scarp (see Azañón et al., 2009 and 2013).



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 227

Página 269 de 632








Unknown


Azañón. J.M., García-Mayordomo, J., Insua-Arévalo, J.M. and Rodríguez-Peces, M.J. (2009) Palaeosismological features of the Granada Fault. En: Pérez-López, R., Grützner, C., Lario, J., Reicherter, K. and Silva, P.G. (eds.), Archaeoseismology and Palaeosismology in the Alpine-Himalayan Collisional Zone: 5-7 p, Baelo Claudia (Cádiz, España), 7-13 de Septiembre de 2009.

Azañón. J.M., García-Mayordomo, J., Insua-Arévalo, J.M. and Rodríguez-Peces, M.J. (2013) Seismiic hazard of the Granada fault. Cuaternario y Geomorfología, 27(3-4):5-32.

Peláez J.A., Sanz de Galdeano, C. y López Casado, C. (2001). Base de datos de fallas de la Cuenca de Granada y evaluación de su potencialidad sísmica. II Congreso Iberoamericano de Ingeniería Sísmica. 16-19 Octubre, Madrid, 2001. 22-30.


Peláez, J.A., Sanz de Galdeano, C. and López Casado, C. (2003). Use of active fault data versus seismicity data in the evaluation of seismic hazard in the Granada basin (Southern Spain). Bulletin of the Seismological Society of America 93, 1670-1678.








References

Variability



Página 270 de 632



ID: ES660 Fault Name: Belicena-Alhendín

Segment Name:

Location X: -3.63828403

Location Y: 37.10839639











Max Depth (km): 5.0 >5 LD Estimated depth is deeper than 5 km based on geologic features (Sanz de Galdeano et al., 2010).

Width (km): 5.8 AR












Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

General change of relief separating Upper Miocene sediments to Pliocene-Pleistocene deposits

(Sanz de Galdeano et al., 2010)



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 232

Página 271 de 632








Unknown












References

Variability



Página 272 de 632



ID: ES662 Fault Name: Huenes

Segment Name:


Location Y: 37.14144993






Dip (º): 65 ± 10 LD (Sanz de Galdeano et al., 2010)


Sense of Movement: SN LD Sinistral strike slip is predominant (depending on the site), although its magnitude is unknown (Sanz de Galdeano et al., 2010)

Length (km): 8.0 to 7.5 EJ Compiler's measurement, based on Sanz de Galdeano et al. (2012).



Width (km): 11.0 AR



Quaternary LD (Sanz de Galdeano et al., 2010)


0.250 LD From the displacement observed in the last 0.4 Ma (Sanz de Galdeano et al., 2010)


0.394 AR From NSR and rake of the fault.


0.481 ± 0.1 AR From VSR, dip and rake of the fault.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

The scarp with many indicators of sense of displacement Some of the scarps have the appearance of very recent formation (Sanz de Galdeano et al., 2010)



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 233

Página 273 de 632








Unknown







Sanz de Galdeano, C., F.J. García-Tortosa, J.A. Peláez, P. Alfaro, J.M. Azañón, J. Galindo-Zaldívar, C. López Casado, A.C. López Garrido, J. Rodríguez-Fernández, P. Ruano (2012): Main active faults in the Granada and Guadix-Baza Basins (Betic Cordillera). Journal of Iberian Geology, 38, 209-223.



Source Comment



References

Variability



Página 274 de 632



ID: ES664 Fault Name: Dílar

Segment Name:

Location X: -3.59523383

Location Y: 37.10494186





Average Strike(º): 140 LD Calculated from its tips. (Sanz de Galdeano et al., 2012).

Dip (º): 60 ± 10 LD (Sanz de Galdeano et al., 2012).






Width (km): 11.5 AR



Holocene probably

LD In some places the triangular facets are very well conserved and they seem very recent. (Sanz de Galdeano et al., 2012).


0.330 LD From the displacement observed in the last 1 Ma. If the displacement of the last 5 Ma is considered, vertical slip rate is of the order of 0.16 m/ka. (Sanz de Galdeano et al., 2012).




0.381 ± 0.1 AR From VSR, dip and rake of the fault.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Splendid scarp and other associated features In some places the triangular facets are very well conserved and they seem very recent. Locally the Pliocene-Pleistocene sediments are vertical for the effect of the drag of the fault (Sanz de Galdeano et al., 2012).



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 234

Página 275 de 632








Unknown







Sanz de Galdeano, C., F.J. García-Tortosa, J.A. Peláez, P. Alfaro, J.M. Azañón, J. Galindo-Zaldívar, C. López Casado, A.C. López Garrido, J. Rodríguez-Fernández, P. Ruano (2012): Main active faults in the Granada and Guadix-Baza Basins (Betic Cordillera). Journal of Iberian Geology, 38, 209-223.



Source Comment



References

Variability



Página 276 de 632



ID: ES666 Fault Name: Padul-Nigüelas

Segment Name:

Location X: -3638

Location Y: 37049

Name of Compiler(s): Sanz de Galdeano, C., Peláez, J.A., García-Mayordomo, J., Martín-Banda, R.

Filiation: I.A.C.T., Universidad de Jaén, IGME, UCM



Average Strike(º): 130 LD Sanz de Galdeano et al. (2012)

Dip (º): 50 + 20 / - 10 LD Sanz de Galdeano et al. (2012)

Rake (º): -90 LD Sanz de Galdeano et al. (2012)

Sense of Movement: N LD Sanz de Galdeano et al. (2012)

Length (km): 13.0 OD At surface comprises two paralel faults (Padul and Padul-Durcal). Length is from Padul-Durcal fault. Sanz de Galdeano et al. (2012)

Min Depth (km): 0 LD Sanz de Galdeano et al. (2012)

Max Depth (km): 5.0 > 5 EJ Estimated depth is deeper than 5 km based on geologic features. It is assumed that Padul and Padul-Durcal faults converge in depth.

Width (km): 6.5 AR



Upper Pleistocene

Upper Pleistocene to Holocene

LD Sanz de Galdeano et al. (2012)


0.350 0.16-0.35 LD From the displacement observed in the last 1 Ma. If the displacement of the last 5 Ma is considered, vertical slip rate is of the order of 0.16 m/ka.


0 EJ Fault seems pure normal




Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Very well-expressed triangular facets, fault scarps, and recent peat layers tilted towards the fault. Alluvial fans are cut by the fault.The mountain front sinuosity points to medium-high to high activity.

Fault scarp is spectacular. Sanz de Galdeano et al. (2012); Hürtgen et al. (2013)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 235

Página 277 de 632




6.51 ± 0.37 ER Using length and Stirling et al (2002) for the instrumental dataset.




Unknown


Hürtgen, J., Rudersdorf, A., Grützner, c. and Reicherter, K. (2013). Morphotectonics of the Padul-Nigüelas Fault Zone, southern Spain. Annals of Geophysics,56:6, S0679; doi:10.4401/ag-6208.











References

Variability



Página 278 de 632



ID: ES672 Fault Name: Noroeste de Játar

Segment Name:

Location X: -3.894

Location Y: 36.912





Average Strike(º): 314 OD Calculated from its tips.

Dip (º): 60 OD

Rake (º): -90 OD


Length (km): 5.2 LD Compiler's measurement, based on Elorza et al. (1979)


Max Depth (km): 5.0 >5 OD Estimated depth is deeper than 5 km based on geologic features.

Width (km): 5.8 AR



Plio-Quaternary

LD Elorza et al. (1979)


0.080 OD From the displacement observed in the last 10 Ma.




0.092 AR From VSR, dip and rake.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

The general scarp The scarp separates metamorphic and sedimentary rocks



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 236

Página 279 de 632








Unknown


Elorza, J.J., García-Dueñas, V., Matas, J., Martín, L., González-donoso, J.M., Gómez-Prieto, J. (1979). Hoja de Zafarraya (1040) del Mapa Geológico de España a escala 1: 50.000. Madrid, España.








Source Comment



References

Variability



Página 280 de 632



ID: ES673 Fault Name: Ventas de Zafarraya - Norte de Sierra Tejeda

Segment Name: Norte de Sierra Tejeda

Location X: -3.95936829






Average Strike(º): 282 LD Calculated from its tips (Sanz de Galdeano et al., 2003, 2012)

Dip (º): 75 60-90 LD Sanz de Galdeano et al., 2012

Rake (º): -90 EJ

Sense of Movement: N ND-N LD At Present the normal component is predominant versus dextral strike slip. The magnitude of the latter is unknown (Sanz de Galdeano et al., 2012).

Length (km): 12.0 LD Lenght of the fault trace as observed in the field along the north front of Sierra Tejeda (Sanz de Galdeano et al., 2003, 2012).

Min Depth (km): 0 LD Sanz de Galdeano et al., 2012.

Max Depth (km): 10.0 >10 EJ Estimated depth is deeper than 10 km based on geologic features.

Width (km): 10.4 AR

Area (km²): 124.23 AR


Holocene LD Sanz de Galdeano et al. (2012)


0.125 LD From the displacement observed in the last 10 Ma. The throw was formed especially from the late Miocene (Sanz de Galdeano et al., 2012).


0 LD The main dextral displacement occurred during the early and middle Miocene Sanz de Galdeano et al. (2012).


0.129 LD From dip, rake and VSR.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

The general scarp. In some places it is well conserved and has striae and other features associated

Sanz de Galdeano et al. (2012)

Geological Set: Betic Range (Granada-Málaga)


Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 237

Página 281 de 632




6.48 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset and from the equation of W&C'94 for strike slip faults. As a normal fault Mw would be 6.6 (0.7 sigma). This fault also has a different interpretation (see ES681).




Unknown



Sanz de Galdeano, C.,García-Tortosa, F.J., Peláez, J.A., Alfaro, P., Azañón, J.M.,Galindo-Zaldívar, J., López Casado, S., López Garrido, A.C., Rodríguez-Fernández, J. and Ruano, P. (2012)Main active faults in the Granada and Guadix-Baza Basins (Betic Cordillera), Journal of Iberian Geology 38 (1) 2012: 209-223.











References

Variability





ES673

Terremoto de Arenas del Rey de

1884

25/12/1884 -3.983, 37.000

IX-X Geographic proximity617

Página 282 de 632



ID: ES675 Fault Name: Albuñuelas

Segment Name:

Location X: -3.5976

Location Y: 36.9137






Dip (º): 50 ± 10 LD Sanz de Galdeano et al. (2012)






Width (km): 6.5 AR



Pleistocene LD Sanz de Galdeano et al. (2012)


0.140 LD From the displacement observed in the last 5 Ma. Sanz de Galdeano et al. (2012)




0.183 AR From VSR, dip and rake of the fault.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

The line of the fault and at some point the surface of the scarp The general scarp is superior to 200m. Locally some small alluvial fans are cut (Sanz de Galdeano et al., 2012).



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 239

Página 283 de 632




6.22 ± 0.37 ER Magnitude from length using Stirling et al (2002) equation derived from the instrumental dataset.




Unknown









Source Comment



References

Variability



Página 284 de 632



ID: ES681 Fault Name: Ventas de Zafarraya - Norte de Sierra Tejeda

Segment Name: Ventas de Zafarraya

Location X: -4.08196679

Location Y: 36.95090904

Name of Compiler(s): Rodríguez Peces, M.J., García-Mayordomo, J. and Martín-Banda, R.





Dip (º): 60 60-90 LD Reicherter et al., 2003; Sanz de Galdeano et al. (2012)

Rake (º): -102 -102 to -117 LD Reicherter et al., 2003; Sanz de Galdeano et al. (2012)

Sense of Movement: N N to ND LD Reicherter et al., 2003; Sanz de Galdeano et al. (2012)

Length (km): 8.0 to 7.5 OD

Min Depth (km): 0 LD Outcrops at surface. Reicherter et al., 2003; Sanz de Galdeano et al. (2012)

Max Depth (km): 10.0 >10 EJ Estimated depth is deeper than 10 km based on geologic features ( Sanz de Galdeano et al., 2003 and 2012)

Width (km): 11.5 AR



Holocene (Present Day)

LD The fault ruptured at surface in the 1884 event (Reicherter et al., 2003; Grützner et al., 2013).


0.350 0.3 to 0.45 LD Preferred value is for Holocene (2.96m/8.8ka) (Grützner et al., 2013). Considering a total slip since post-Tortonian results 0.17+/-0.03 m/ka (Reicherter et al, 2003).






1.5 1.0-1.5 LD Reicherter et al, 2003


3 since 8800 BP

± 130 LD From trenches and radiocarbon dating (Reicherter et al., 2003; Grützner, et al 2013)


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Quaternary sediments offset, fault scarp, Geomorphic anomalies Reicherter et al. (2003) and Grützner et al. (2013)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 238

Página 285 de 632




6.31 ± 0.37 ER Magnitude from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.5 (to 7.0) according to Reicherter et al. (2003) and Grützner et al. (2013).


2000 2000-3000 LD From paleoseismological work of Reicherter et al. (2003) and Grützner et al. (2013). Considering the Maximum Earthquake Model (Wesnousky, 1986) and SR=0.413 m/ky and M=6.31, results 2840 yrs.


1884 LD Reicherter et al. (2003) and Grützner et al. (2013).


Grützner, C., Ruano,P., Jabaloy, A., Galindo-Zaldívar, J.Becker-Heidmann, P.,Sanz de Galdeano, C., Rudersdorf, A., Reicherter, K.(2013) Late Holocene rupture history of the Ventas de Zafarraya Fault (Southern Spain), Cuaternario y Geomorfología, 27 (3-4):5-32.

Mezcua, J., Rueda, J. and García Blanco, R.M. (2004). Reevaluation of Historic Earthquakes in Spain. Seismological Research Letters, 75 (1): 75-81.

Reicherter, K.R.; Jabaloy, A.; Galindo-Zaldívar, J.; Ruano, P.; Becker-Heidmann, P.; Morales, J.; Reiss, S. and González-Lodeiro, F. (2003). Repeated palaeoseismic activity of the Ventas de Zafarraya fault (S Spain) and its relation with the 1884 Andalusian earthquake. International Journal of Earth Sciences (Geologische Rundschau), 92: 912-922.

Sanz de Galdeano, C.; Peláez Montilla, J.A. and López Casado, C. (2003). Seismic Potential of the Main Active Faults in the Granada Basin (Southern Spain). Pure and Applied Geophysics, 160: 1537-1556.






References

Variability





ES681

Terremoto de Arenas del Rey

(Granada)

25/12/1884 -3.98, 36.95 X (EMS) IGN, IAG Paleoseismological study (Reicherter et al,

2003)

Estimated Mw=6.5 (+0.3, -0.3) (Reicherter et al, 2003; Mezcua et al, 2004)

618

Página 286 de 632



ID: ES682 Fault Name: Galera

Segment Name:

Location X: -2.487

Location Y: 37.798

Name of Compiler(s): García Tortosa, F.J., Peláez, J.A., Alfaro, P., Sanz de Galdeano, C. and Galindo, J.

Filiation: Universidades de Jaén, Alicante, Granada e IACT.



Average Strike(º): 228 LD Calculated from the tips of an intermediate trace inside the fault zone (Sanz de Galdeano et al., 2012)

Dip (º): 50 10 LD Average dip as observed at surface (Sanz de Galdeano et al., 2012)

Rake (º): 40 LD Sanz de Galdeano et al. (2012)

Sense of Movement: SR LD Sanz de Galdeano et al. (2012)

Length (km): 25.0 2 LD Lenght of the fault trace as observed in the field (Sanz de Galdeano et al., 2012)


Max Depth (km): 5.0 LD Estimated depth is deeper than 5 km based on gravimetric study and associated seismicity (Sanz de Galdeano et al., 2012)

Width (km): 6.5 AR

Area (km²): 163.18 AR


205 ka 205-600 LD Age of glacis dated by a calcrete (Sanz de Galdeano et al., 2012). Pérez-Peña et al. (2009) estimates a much younger age, 45 ka.


0.160 0.08-0.24 LD Average value from the deformation of Quaternary markers, mainly from Middle Pleistocene (Sanz de Galdeano et al., 2012)






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It generates a small mountain front and affects a Quaternary glacis surface.




Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 201

Página 287 de 632




6.78 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.6 (± 0.7) from the equation Mw=Mw(l) of W&C'94 for normal faults. As a strike slip fault Mw would be 6.7 (0.2 sigma).




Unknown


Alfaro, P., Gibert, L., Moretti, M., García-Tortosa, F.J., Sanz de Galdeano, C., Galindo-Zaldívar, J. y López Garrido, A.C.( 2010). Giant seismites in the Plio-Pleistocene Baza paleolake (S Spain). Terra Nova 22, 172-179.

García Tortosa, F.J., Sanz de Galdeano, C., Alfaro, P. y Ureña, M. (2007). El glacis de la cuenca de Guadix-Baza. Una superficie de referencia para el análisis tectónico y la evolución geomorfológica de la cuenca, en La cuenca de Guadix-Baza. Estructura, tectónica activa, sismicidad, geomorfología y dataciones existentes (Sanz de Galdeano, C., y Peláez, J.A., eds.), Granada, 111-126

García Tortosa, F.J., Sanz de Galdeano, C., Alfaro, P., Galindo Zaldívar, J., y Peláez, J.A. (2007). La falla y los pliegues de Galera, en La cuenca de Guadix-Baza. Estructura, tectónica activa, sismicidad, geomorfología y dataciones existentes (Sanz de Galdeano, C., y Peláez, J.A., eds.), Granada, 141-153.

García-Tortosa, F.J., Sanz de Galdeano, C., Alfaro, P., Galindo-Zaldívar, J. (2008). Deformación reciente de la Cuenca de Guadix-Baza. GeoTemas 10, 1007-1010.

García-Tortosa, F.J., Sanz de Galdeano, C., Peláez, J.A., Alfaro, P., López-Casado, C., Galindo-Zaldívar, J. (2008). Actividad de la falla de Galera (cuenca de Guadix-Baza, Cordillera Bética central). VI Asamblea Hispano-Portuguesa de Geodesia y Geofísica, Tomar (Portugal). 363-364.

García-Tortosa, F.J., Alfaro, P., Sanz de Galdeano, C. y Galindo-Zaldívar, J. (2010). Glacis geometry as a geomorphic marker of recent tectonics: The Guadix-Baza Basin (South Spain). Geomorphology, doi.: 10.1016/j.geomorph.2010.10.021.

Peláez, J.A., Sanz de Galdeano, C., y López Casado, C. (2007). Determinación preliminar del potencial sísmico de la Cuenca de Guadix-Baza (Granada). 3er Congreso Nacional de Ingeniería Sísmica. Girona (España).

Peláez, J.A., Sanz de Galdeano, C., y López Casado, C. (2007). Peligrosidad sísmica en la Cuenca de Guadix-Baza a partir de datos de fallas activa, en La Cuenca de Guadix-Baza. Estructura, Tectónica activa, sismicidad, Geomorfología y dataciones existentes (C. Sanz de Galdeano & J.A. Peláez, eds.). Granada. 301-310.

Pérez-Peña, J.V., Azañón, J.M., Azor, A., Tuccimei, P., Della Seta, M., Soligo, M. (2009b). Quaternary landscape evolution and erosionrates for an intramontane Neogene basin (Guadix-Baza basin, SE Spain). Geomorphology 106, 206-218.

Sanz de Galdeano, C., Peláez, J.A., y López Casado, C. (2007). Fallas activas y potencial sísmico de la cuenca de Guadix-Baza, en La cuenca de Guadix-Baza. Estructura, tectónica activa, sismicidad, geomorfología y dataciones existentes (Sanz de Galdeano, C., y Peláez, J.A., eds.), Granada, 283-299.






References

Variability





ES682

Terremoto de SW de Galera de 1964

09/06/1964 -2.5667, 37.7367

4.8 mbLg, VIII I.G.N. Geographic proximity Possible associated seismicity619

Página 288 de 632




Página 289 de 632



ID: ES684 Fault Name: Botardo-Alfahuara

Segment Name:

Location X: -2.56112098

Location Y: 37.81215119





Average Strike(º): 112 OD Calculated from the tips (in the previous section the coordinate of the northern tip is given).

Dip (º): 85 LD Sanz de Galdeano et al. (2012)

Rake (º): 135 180-90 EJ Original record modified by García-Mayordomo (14/10/2013) in order to calculate NSR based on Sanz de Galdeano et al. (2012) description of the fault.

Sense of Movement: RD D to R LD Sanz de Galdeano et al. (2012)

Length (km): 25.0 ± 3 LD Trace of the structure observed in the field and estimation of its continuity towards NW due to seismicity possibly associated (Sanz Galdeano et al., 2012).

Min Depth (km): 0 0-0.5 LD This fault is associated with an anticline structure that produces a N120ºE elongated structural high of more than 20 km length (Sanz Galdeano et al., 2012). Part of the fault is blind.

Max Depth (km): 11.0 5-11 LD At least deeper than 5 km based on gravimetric study (Galdeano et al. (2007, 2012). Original record modified by García-Mayordomo (14/10/2013) to include the depth of the seismogenic crust in the

Width (km): 11.0 AR

Area (km²): 276.05 AR


Holocene Upper Pleistocene-Holocene

LD Fault associate to folding affecting upper Miocene to Pleistocene rocks. Several travertines and discontinuous small faults could be related to a blind fault.


0.030 LD From the displacement observed in the last 5 Ma. Galdeano et al. (2007, 2012).


0.03 AR Using VSR and -135º Rake


0.043 AR Using VSR and -135º Rake


Unknown

Identification


Quaternary Activity

Variability Source

Comment

This fault has been an active fault since the Lat Miocene but not always with a clearly visible fault plane at surface. This structure probably also displaces the glacis of the basin.

Considering its seemingly associated seismicity, it appears more active in its western section (Sanz de Galdeano et al., 2012).


Identification Method: Geological/Geomorphological field mapping and association to seismicity

Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 202

Página 290 de 632




Unknown


Unknown


6.78 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.6 (± 0.2) from the equation Mw=Mw(l) of W&C'94 for strike slip fault.




Unknown







Sanz de Galdeano, C., García Tortosa, F.J., Alfaro, P., López Garrido, A.C., Delgado, J., Gibert, L., y López Garrido, A.C. (2007). El anticlinal de Alfahuara-Botardo (sector de Orce-Huéscar, cuenca de Guadix-Baza, Cordillera Bética), en La cuenca de Guadix-Baza. Estructura, tectónica activa, sismicidad, geomorfología y dataciones existentes (Sanz de Galdeano, C., y Peláez, J.A., eds.), Granada, 127-139.


Sanz de Galdeano, C., J.A. Peláez, C. López Casado, P. Alfaro, F.J. García Tortosa, J. Galindo Zaldívar y A.C. López Garrido (2010). Tectónica activa en las cuencas de Granada y Guadix‐Baza (Cordillera Bética, sur de España). En: Contribución de la Geología al Análisis de la Peligrosidad Sísmica (J.M. Insua y F. Martín‐González, eds.), pp. 2‐5. Sigüenza (Guadalajara, España).

Sanz de Galdeano, C., F.J. García Tortosa, J.A. Peláez, P. Alfaro, Azañón, J.M., J. Galindo Zaldívar, C. López Casado, A.C. López Garrido, J. Rodríguez-Fernández y P. Ruano (2012). Main active faults in the Granada and Guadix-Baza basins (Betic Cordillera). Journal of Iberian Geology, 38(1):209-224.





References

Variability





ES684

Terremoto de NE de Orce de 1973

21/03/1973 -2.4583, 37.7850

4.0 mbLg I.G.N. Geographic proximity Possible associated seismicity620

Página 291 de 632





Página 292 de 632



ID: ES686 Fault Name: Baza

Segment Name:

Location X: -2.68327084

Location Y: 37.35163302





Average Strike(º): 341 LD Calculated from the tips of the main fault trace, which varies its orientation from the southern part to the northern part (see extended data). Some branches of the fault are very important as regards its dimensions. See Sanz de Galdeano et al. (2012).

Dip (º): 65 45-65 LD Average dip as observed at surface. Deep geometry is listric, as observed in seismic sections. Sanz de Galdeano et al. (2012)


Sense of Movement: N LD The striations visible on different surfaces indicate purely normal movements (Sanz de Galdeano et al., 2012).


Min Depth (km): 0 LD Outcrops at the surface (Sanz de Galdeano et al., 2012).

Max Depth (km): 11.0 LD The estimated depth from geologic features, gravimetric studies and seismic exploration is deeper than 5 km. Value is the depth of the seismogenic crust in the region: 11 km (García-Mayordomo, 2005).

Width (km): 12.1 AR

Area (km²): 450.29 AR




0.330 0.17-0.49 LD Preferred value is the mean considering geological and geomorphological markers (glacis surface) from the Middle Pleistocene. Variability considers the age of a calcrete dated 200 to 600 ka.






Unknown

Identification


Quaternary Activity

Variability Source

Comment

It generates an important mountain front of more than 25 km length, coinciding with the main fault branch. Secondary branches generate conspicuous topographic scarps, which can be continued laterally for several hundreds of meters and even

Considering its associated seismicity, the Baza Fault seems to be more active inits northern part (Sanz de Galdeano et al., 2012).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 203

Página 293 de 632




Unknown


Unknown






1531 AD LD The Baza 1531 AD event is very likely related to the Baza fault (Sanz de Galdeano et al., 2012).


Alfaro, P., Delgado, J., Sanz de Galdeano, C., Galindo Zaldívar, J., García Tortosa, F.J., López Garrido, A.C., López Casado, C., Marín, C., Gil, A., and Borque, M.J. (2008). The Baza Fault: a major active extensional fault in the Central Betic Cordillera (South Spain). Int. J. Earth Sci. 97, 1353-1365.

Alfaro, P., Gibert, L., Moretti, M., García-Tortosa, F.J., Sanz de Galdeano, C., Galindo-Zaldívar, J. y López Garrido, A.C.( 2010). Giant seismites in the Plio-Pleistocene Baza paleolake (S Spain). Terra Nova 22, 172-179.


García Tortosa, F.J., Sanz de Galdeano, C., Alfaro, P., Galindo Zaldívar, J., y Peláez, J.A. (2007). La falla y los pliegues de Galera, en La cuenca de Guadix-Baza. Estructura, tectónica activa, sismicidad, geomorfología y dataciones existentes (Sanz de Galdeano, C., y Peláez, J.A., eds.), Granada, 141-153.


García Tortosa, F.J., Alfaro, P., Galindo Zaldívar, J., Gibert, L., López Garrido, A.C., Sanz de Galdeano, C., and Ureña, M. (2008). Geomorphologic evidence of the active Baza Fault (Betic Cordillera, South Spain). Geomorphology 97, 374-391.





Sanz de Galdeano, C., Peláez, J.A., y López Casado, C. (2007). Fallas activas y potencial sísmico de la cuenca de Guadix-Baza, en La




References

Variability





ES686

Terremoto de Baza de 1531

30/09/1531 -2.5333, 37.5333

VIII-IX, 6.0+-0.6 macroseismic

I.G.N. Geographic proximity Possible associated seismicity621

Página 294 de 632



cuenca de Guadix-Baza. Estructura, tectónica activa, sismicidad, geomorfología y dataciones existentes (Sanz de Galdeano, C., y Peláez, J.A., eds.), Granada, 283-299.




Página 295 de 632



ID: ES695 Fault Name: Solana de Zamborino Fault Zone

Segment Name:


Location Y: 37.46991846





Average Strike(º): 148 -10 LD Calculated from the tips of a trace located in between the different ramifications in which the fault branches in its northern half (see extended). It might extend towards the south as there is seismicity aligned with the same orientation.

Dip (º): 65 LD Average dip as observed at surface (Sanz de Galdeano et al., 2012).



Length (km): 27.0 0.5 LD It has a wide fault zone, similar to the Baza Fault, with several splays that produce small topographic escarpments that in several sectors have been eroded (Sanz de Galdeano et al., 2012).


Max Depth (km): 11.0 LD The estimated depth from geologic features, gravimetric studies and seismic exploration is deeper than 5 km. Value is the depth of the seismogenic crust in the region: 11 km (García-Mayordomo, 2005).

Width (km): 12.1 AR

Area (km²): 327.70 AR




0.160 0.08-0.24 LD Considering geological and geomorphological markers from Middle Pleistocene (Sanz de Galdeano et al., 2012).




0.177 0.088-0.265 AR From dip and rake of the fault.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Several scarps in a Quaternary glacis surface, which coincide with different branches of the fault. Fault zone cuts Pliocene and Quaternary sediments, displacing the glacis about 50 m.

(Sanz de Galdeano et al., 2012).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 204

Página 296 de 632




Unknown






Unknown















References

Variability



Página 297 de 632



ID: ES699 Fault Name: Graena-Lugros Fault Zone

Segment Name:

Location X: -3.16821649

Location Y: 37.20952436





Average Strike(º): 326 LD Calculated from the tips (Sanz de Galdeano et al., 2012).

Dip (º): 70 LD Average dip as observed at surface (Sanz de Galdeano et al., 2012).



Length (km): 11.0 LD Maximum length of single fault traces (Sanz de Galdeano et al., 2012).

Min Depth (km): 0 LD Outcrops at the surface (Sanz de Galdeano et al., 2012).

Max Depth (km): 11.0 LD The estimated depth from geologic features is of the order of 5 km (Sanz de Galdeano et al., 2012).Value is the depth of the seismogenic crust in the region: 11 km (García-Mayordomo, 2005).

Width (km): 11.7 AR

Area (km²): 128.77 AR




0.130 0.07-0.19 LD Average value considering geological and geomorphological markers from the Middle Pleistocene (glacis) (Sanz de Galdeano et al., 2012).




0.138 0.074-0.202 AR From dip and rake of the fault.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

The faults produce metric to decametric vertical displacements in Pleistocene fluvial rocks and an accumulated displacement of around 40 m across the glacis. Scarps in a Quaternary glacis surface.

(Sanz de Galdeano et al., 2012).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 205

Página 298 de 632








Unknown




García-Tortosa, F.J., Alfaro, P., Sanz de Galdeano, C. y Galindo-Zaldívar, J. (2010). Glacis geometry as a geomorphic marker of recent tectonics: The Guadix-Baza Basin (South Spain). Geomorphology, doi.: 10.1016/j.geomorph.2010.10.021











References

Variability





ES699

Terremoto de Guadix de 1946

09/06/1946 -3.1833, 37.3000

3.9 mbLg, V I.G.N. Geographic proximity Possible associated seismicity622

Página 299 de 632



ID: ES705 Fault Name: Laujar

Segment Name:

Location X: -2.94141763

Location Y: 37.00410339

Name of Compiler(s): García Tortosa, F.J., Peláez, J.A. and Sanz de Galdeano, C.

Filiation: Universidad de Jaén, IACT



Average Strike(º): 095 5 LD Calculated from the tips of the main fault trace. There is a number of vertical fault planes parallel or subparallel, with their corresponding scarps very well preserved (García Tortosa and Sanz de Galdeano, 2007).

Dip (º): 60 10 LD Average dip as observed at surface (García Tortosa and Sanz de Galdeano, 2007).

Rake (º): -90 LD García Tortosa and Sanz de Galdeano (2007)

Sense of Movement: N LD García Tortosa and Sanz de Galdeano (2007)

Length (km): 10.0 10 to 20 LD Lenght of the fault trace as observed in the field is 5 km, although its geomorphologic expression can be extended for more than 10 km to the west and few km to the east (García Tortosa and Sanz de Galdeano, 2007).

Min Depth (km): 0 LD Outcrops at the surface (García Tortosa and Sanz de Galdeano, 2007).

Max Depth (km): 8.0 LD Max depth is bottom fragile crust in this area (García-Mayordomo, 2005, table 4.12 and 4.20, fig, 4.21).

Width (km): 9.2 Unknown

Area (km²): 92.38 Unknown


Upper Pleistocene

LD No absolute dates available yet. It is assumed ca 140ka for cemented colluvial deposits and ca 20 ky for the ones not cemented (García-Tortosa and Sanz de Galdeano, 2007).


0.430 0.43-0.75 LD SR estimations are maximum values representative of the uplift associated to the south border of Sierra Nevada Range. Variability indicates estimations from 60m/140ka and 15m/20 ka, respectively (García-Tortosa and Sanz de Galdeano, 2007).




0.497 0.497-0.866 AR From VSR, dip and rake. Very likely an overestimation.


Unknown

Identification


Quaternary Activity

Variability Source

Comment

The fault produces a sharp mountain front and small topographic scarps that can be continued for hundreds of meters.

García Tortosa and Sanz de Galdeano (2007)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 213

Página 300 de 632




Unknown


Unknown






Unknown


García Tortosa F.J. y Sanz de Galdeano C. (2007). Evidencias geomorfológicas de actividad tectónica cuaternaria en el frente montañoso del borde sur de Sierra Nevada: la falla normal de Laujar de Andarax. Cuaternario y Geomorfología 21 (3-4), 101-112.





References

Variability



Página 301 de 632



ID: ES706 Fault Name: Alfacar

Segment Name:

Location X: -3.56755443

Location Y: 37.25631689

Name of Compiler(s): Azañón, J.M., Rodríguez Peces, M.J. and Pérez Peña, J.V.

Filiation: IACT and Universidad Complutense de Madrid

Email: [email protected]; martinjr@g


Average Strike(º): 129 128-150 LD Compiler's measurement, based on the Sheet number 1009 (Granada) from the Geologic Map of Spain, scale 1:50000 (Lupiani and Soria, 1988) and Pérez-Peña et al (2009), following the right-hand rule.

Dip (º): 50 ± 10 EJ

Rake (º): -80 EJ

Sense of Movement: ND EJ

Length (km): 5.3 LD Compiler's measurement, based on the Sheet number 1009 (Granada) from the Geologic Map of Spain, scale 1:50000 (Lupiani and Soria, 1988) and Pérez-Peña et al (2009), following the right-hand rule.

Min Depth (km): 0 LD Lupiani and Soria (1988)

Max Depth (km): 11.0 EJ Depth of the fragile crust based on similarities in crustal thickness and heat flux to the Central Betic Crustal Block (cf. García-Mayordomo, 2005)

Width (km): 14.4 AR



Quaternary EJ Late Pleistocene-Holocene, age of the slope and travertine deposits (Lupiani and Soria, 1988)


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Well defined mountain front in its NW termination. Fault scarp is traceable in several points. It produces anomalies in drainage network courses. It controls travertine deposits in this mountain front and affects slope deposits.

Lupiani and Soria (1988) and Pérez-Peña et al (2009).



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 228

Página 302 de 632




Unknown






Unknown


Azañón JM, Azor A, Booth-Rea G, Torcal F. (2004): Small-scale faulting, topographic steps and seismic ruptures in the Alhambra (Granada, southeast Spain). Journal of Quaternary Science 19: 219-227. DOI: 10.1002/jqs.838

Lupiani, E. and Soria, J. (1988). Mapa geológico de España a escala 1:50.000. Hoja número 1009 (Granada). Madrid, España.

Pérez-Peña JV, Azañón JM, Azor a, Delgado J, González-Lodeiro F. (2009): Spatial analysis of stream power using GIS: SLk anomaly maps. Earth Surface Processes and Landforms 34: 16-25. DOI: 10.1002/esp





References

Variability



Página 303 de 632



ID: ES707 Fault Name: Cogollos

Segment Name:

Location X: -3.57137173

Location Y: 37.31302214

Name of Compiler(s): Azañón, J.M.; Rodríguez Peces, M.J. and Pérez Peña, J. V.




Average Strike(º): 177 145-195 LD Compiler's measurement, based on the Sheet number 1009 (Granada) from the Geologic Map of Spain, scale 1:50.000 (Lupiani and Soria, 1988) and Pérez-Peña et al. (2009), following the right-hand rule.

Dip (º): 70 ± 10 EJ

Rake (º): -90 EJ

Sense of Movement: N EJ

Length (km): 5.5 LD Compiler's measurement, based on the Sheet number 1009 (Granada) from the Geologic Map of Spain, scale 1:50.000 (Lupiani and Soria, 1988)

Min Depth (km): 0 LD Lupiani and Soria (1988)


Width (km): 11.7 AR



Quaternary EJ It controls travertine deposits of age Late Pleistocene- Holocene


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

The fault system forms a well defined mountain front that separates sediments of Granada basin (Plio-Pleistocene) from its basement. Fault scarps are traceable in several points. It produces anomalies in the drainage network

Pérez-Peña et al. (2009).



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 229

Página 304 de 632




Unknown






Unknown


Azañón JM, Azor A, Booth-Rea G, Torcal F. (2004): Small-scale faulting, topographic steps and seismic ruptures in the Alhambra (Granada, southeast Spain). Journal of Quaternary Science 19: 219-227. DOI: 10.1002/jqs.838

Lupiani, E. and Soria, J. (1988). Mapa geológico de España a escala 1:50.000. Hoja número 1009 (Granada). Madrid, España.

Pérez-Peña JV, Azañón JM, Azor a, Delgado J, González-Lodeiro F. (2009): Spatial analysis of stream power using GIS: SLk anomaly maps. Earth Surface Processes and Landforms 34: 16-25. DOI: 10.1002/esp





References

Variability



Página 305 de 632



ID: ES712 Fault Name: Malahá

Segment Name:

Location X: -3.77570794

Location Y: 37.12389315

Name of Compiler(s): Azañón, J.M.; Rodríguez Peces, M.J.; Pérez-Peña, J.V.




Average Strike(º): 112 LD Azañón et al. (2007)

Dip (º): 60 ± 10 EJ

Rake (º): -70 EJ

Sense of Movement: ND LD Azañón et al. (2007)

Length (km): 11.2 LD Compiler's measurement, based on Azañón et al. (2007)

Min Depth (km): 0 LD Azañón et al. (2007)


Width (km): 12.7 AR

Area (km²): 142.26 AR


<887 years BP ± 48 LD Radiocarbon dating (Azañón et al., 2007)


0.400 LD Actual VSR is unknown but geological evidences point to an activity comparable to the Granada fault. Sedimentary rates associated to the fault plane range from 0.4 to 1.7 mm/yr in the last 3ka (Azañón et al., 2007)


0.168 AR From NSR and rake


0.492 ± 0.1 AR From VSR, dip and rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Linear break in the landscape with associated mountain front. Traceable fault surface. Related archaeological evidences.

It generates a moderate mountain front within Granada basin sediments. The fault surface can be viewed in several locations along fault trace. It has associated archaeological evidences of recent deformation (dated by Radiocarbon).



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 230

Página 306 de 632








Unknown


Azañón, J.M., Booth-Rea, G., Martínez-Martínez, J.M. and Pérez-Peña, V. (2007) Actividad tectónica durante la época medieval y romana en la cuenca de Granada (La Falla de la Malahá). Resúmenes XII Reunión Nacional de Cuaternario, Ávila, p:131-132.



Source Comment



References

Variability



Página 307 de 632



ID: ES716 Fault Name: Albox

Segment Name: Alto del Ruchete - El Saltador

Location X: -1.95161584

Location Y: 37.42568713

Name of Compiler(s): García-Meléndez, E.

Filiation: Universidad de León



Average Strike(º): 255 LD García-Meléndez (2000), García-Meléndez et al. (2003)

Dip (º): 45 60-30 LD Value shown is the average from dips measured in creeks and in the trenches (Masana et al., 2005)

Rake (º): 90 90-110 LD The strike-slip component is negligible (Masana et al., 2005)

Sense of Movement: R LD Also observed by field and aerospace criteria (García-Meléndez, 2000; García-Meléndez et al., 2003)

Length (km): 10.0 LD Calculated by subtle slope changes through DEM in a GIS (García-Meléndez et al., 1996; García-Meléndez, 2000; García-Meléndez et al., 2002; García-Meléndez et al., 2003; García-Meléndez et al., 2004a y b)

Min Depth (km): 0 LD Outcrops at the surface (García-Meléndez, 2000; García-Meléndez et al., 2003; Masana et al., 2005)

Max Depth (km): 10.0 LD Depth of the fragile-ductile transition in the Central Betic Block (García-Mayordomo, 2005)

Width (km): 14.1 AR

Area (km²): 141.42 AR


around 660 AD

LD Masana et al. (2005)


0.025 0.01-0.04 LD Masana et al. (2005) at Ruchete (0.01-0.02 m/ka) and Úrcal (0.02-0.04 m/ka) sites. Value shown is the average.


0 LD The strike-slip component is negligible (Masana et al., 2005)




Unknown


2 minimum LD Masana et al. (2005)

Identification


Quaternary Activity

Variability Source

Comment

Deformation of three different Quaternary sedimentary phases. Right lateral displacement of elongated hill. Subtle slope change for at least 4 km The fault trace interaction with drainage controls areas of differential erosional and depositional patterns.

Masana et al. (2005)



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 231

Página 308 de 632




Unknown


6.40 ± 0.37 ER Magnitude from length using Stirling et al (2002) equation for the instrumental dataset. Masana et al. (2005) based on Mw f (AD) from Wells and Coppersmith (1994) estimated Mw 6.50 (± 0.1).




after 650AD LD Masana et al. (2005): "…may have occurred before the XVIII century, the date of the oldest records in the catalogue"


Briend, M. (1981): Evolution morpho-tectonique du basin neogene de Huércal-Overa (Cordilleres Bétiques orientales-Espagne). Documents et travaux, IGAL 4, 208 pp.

García-Meléndez, E. (2000): Geomorfología y Neotectónica del Cuaternario de la cuenca de Huércal-Overa y corredor del Almanzora. Análisis y Cartografía mediante Teledetección y SIG. Unpublished PhD Thesis. Universidad de Salamanca, 528 pp.

García-Meléndez, E.; Goy, J.L.; Zazo, C.; Ferrer-Julià, M. (1996): Neotectonic features detection with geomorphologic indicators using GIS analysis. Geographical Information, from Research to Application. (Eds. M. Rumor, R. McMillan & H.F.L. Ottens). IOS press, Amsterdam Vol.1:493-498.

Garcia Melendez, E.; Ferrer-Julià, M.; Goy, J.L.; Zazo, C. (2002). Reconstrucción morfoestructural mediante modelos de elevación digital en un SIG del fondo de la cuenca sedimentaria de la Cubeta del Saltador (Cordilleras Béticas Orientales). Geogaceta 32:2003-2006

García-Meléndez, E., Goy, J.L., Zazo, C. (2003). Neotectonics and Plio-Quaternary landscape development within the eastern Huércal-Overa Basin (Betic Cordilleras, southeastern Spain). Geomorphology 50, 111–133.

García-Meléndez, E., Goy, J.L., Zazo, C. (2004a): Actividad tectónica cuaternaria en la Cuenca de Huércal-Overa (Almería, Sureste de España): deformaciones asociadas a la falla de Albox. Geogaceta 36, 63–66.

García-Meléndez, E.; Goy, J.L.; Zazo, C. (2004b): Síntesis de la evolución geodinámica durante el Cuaternario de la Zona Oriental de la Cuenca de Huércal-Overa (Almería, Cordilleras Béticas Orientales). Geotemas 6(4), 227-230

Masana, E., Pallàs, R., Perea, H., Ortuño, M., Martínez-Díaz, J.J., García-Meléndez, E., Santanach, P. (2005). Large Holocene morphogenic earthquakes along the Albox fault, Betic Cordillera, Spain. J. Geodynamics 40, 119–133.


Wells, D. L. y K.J. Coppersmith (1994). New empirical relationships among magnitude, rupture length, rupture area, and surface displacement. Bulletin of the Seismological Society of America, 84(4): 974-1002.





References

Variability



Página 309 de 632



ID: ES717 Fault Name: El Acebuchal

Segment Name: El Acebuchal

Location X: -4.66207025


Name of Compiler(s): Insua-Arévalo, J.M.

Filiation: Universidad Complutense de Madrid



Average Strike(º): 037 +7 / -10 LD Fault trace gently curve (Insua Arévalo, 2008)

Dip (º): 90 -10 LD Subvertical. No fault plane outcropping (Insua Arévalo, 2008)

Rake (º): -90 LD (Insua Arévalo, 2008)

Sense of Movement: N LD Probably normal. No fault plane outcropping (Insua Arévalo, 2008)

Length (km): 11.0 9 to 12 LD (Insua Arévalo, 2008)

Min Depth (km): 0 LD (Insua Arévalo, 2008)

Max Depth (km): 8.0 +2 / -1 EJ Estimated in relation with the length

Width (km): 8.0 AR



780 ka +800/-600 LD Estimated as Lower-middle Pleistocene by the development of calcrete on the faulted alluvial fans (Insua Arévalo, 2008)


0.050 +0.1/-0.03 LD Considering since 780 ka (beginning of the Middle Pleistocene, Insua Arévalo, 2008)


0 LD No horizontal movement considered (Insua Arévalo, 2008)


0.05 0.15-0.02 AR From VSR, dip and rake (pure normal)


0.39 ER Wells & Coppersmith (1994). Following the empirical relationship between Surface Rupture Length (SRL) and Maximum Displacement (MD)


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Topographic lineament, and displacement of alluvial fans deposits

(Insua Arévalo, 2008)

Geological Set: Betic Range (Málaga)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 242

Página 310 de 632




6.44 ± 0.37 ER Magnitude from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.19 (± 0.28) using Wells & Coppersmith (1994), following the empirical relationship between Surface Rupture Length (SRL) and Maximum Magnitude.


38762 46376-26999 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Previous estimations using W&C'94 relationships led to 6500±1300 yrs.The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown


Insua, J.M. (2008) Neotectónica y Tectónica Activa de la Cuenca de Málaga (Cordillera Bética Occidental). Tesis Doctoral. Universidad Complutense de Madrid. 265 pp. http://www.ucm.es/info/tectact/DOCS/Tesis/Tesis%20Insua-Arevalo.pdf



Wesnousky, S.G. (1994). The Gutenberg-Richter or the characteristic earthquake model, which is it? Bulletin of the Seismological Society of America, 84: 1940-1959.

Source Comment



References

Variability



Página 311 de 632



ID: ES718 Fault Name: Los Alamillos

Segment Name: Los Alamillos

Location X: -4.64591311






Average Strike(º): 230 +5 / -10 LD Fault trace gently curve (Insua Arévalo, 2008)

Dip (º): 90 -10 LD Subvertical. No fault plane outcropping (Insua Arévalo, 2008)

Rake (º): -90 LD (Insua Arévalo, 2008)

Sense of Movement: N LD Probably normal. No fault plane outcropping (Insua Arévalo, 2008)

Length (km): 7.0 6 LD (Insua Arévalo, 2008)

Min Depth (km): 0 LD (Insua Arévalo, 2008)

Max Depth (km): 8.0 +2 / -1 EJ Estimated in relation with the length

Width (km): 8.0 AR



780 ka +800/-600 LD Estimated as Lower-middle Pleistocene by the development of calcrete on the faulted alluvial fans (Insua Arévalo, 2008)


0.050 +0.1/-0.03 LD Considering since 780 ka (beginning of the Middle Pleistocene, Insua Arévalo, 2008)


0 LD No horizontal movement considered (Insua Arévalo, 2008)


0.05 0.15-0.02 AR From VSR, dip and rake (pure normal)




Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

topographic lineament, and displacement of alluvial fans deposits (Insua Arévalo, 2008)



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 243

Página 312 de 632




6.25 ± 0.37 ER Magnitude from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.06 (± 0.28) using Wells & Coppersmith (1994), following the empirical relationship between Surface Rupture Length (SRL) and Maximum Magnitude.


31988 287029-2971 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Previous estimations using W&C'94 relationships led to 5100±900 yrs.The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown






Source Comment



References

Variability



Página 313 de 632



ID: ES723 Fault Name: Cartama

Segment Name: Cartama

Location X: -4.66107162

Location Y: 36.68918173





Average Strike(º): 070 LD (Insua Arévalo, 2008)

Dip (º): 10 +5 LD Blind thrust (Insua Arévalo, 2008)

Rake (º): 90 LD (Insua Arévalo, 2008)

Sense of Movement: R LD (Insua Arévalo, 2008)

Length (km): 6.0 LD (Insua Arévalo, 2008)

Min Depth (km): 0.5 LD (Insua Arévalo, 2008)

Max Depth (km): 2.5 +2 / -0.5 LD Insua Arévalo (2008)

Width (km): 11.5 AR



Quaternary s.l. EJ Pliocene (4700 ka) marine deposit folded up to 30º in the northern flank of the Sierra de Cartama (Insua Arévalo, 2008)


0.010 LD Minimum value considering the evolution of the geometry of the associated anticline of the Sierra de Cartama since 4700 ka (in Insua Arévalo, 2008)




0.06 AR Considering Dip, Rake and VSR.




Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Active anticline, drainage pattern affected (Insua Arévalo, 2008)



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 248

Página 314 de 632








Unknown






Source Comment



References

Variability



Página 315 de 632



ID: ES725 Fault Name: Villafranco de Guadalhorce

Segment Name: Villafranco de Guadalhorce

Location X: -4.74406845

Location Y: 36.68418126





Average Strike(º): 070 LD (Insua Arévalo, 2008)

Dip (º): 10 + 5 LD Blind thrust (Insua Arévalo, 2008)

Rake (º): 90 LD (Insua Arévalo, 2008)

Sense of Movement: R LD (Insua Arévalo, 2008)

Length (km): 7.0 LD (Insua Arévalo, 2008)

Min Depth (km): 0.5 LD (Insua Arévalo, 2008)

Max Depth (km): 2.5 + 2 / - 0.5 LD Insua Arévalo (2008)

Width (km): 11.5 AR



Quaternary s.l. EJ Pliocene (4700 ka) marine deposit folded up to 5º in the southern flank of the Villafranco de Guadalhorce hill (Insua Arévalo, 2008).




0.05 LD Probably similar to that from Cartama Fault (Upper Flat) (in Insua Arévalo, 2008). See referred record on this database.


0.06 AR Considering Dip, Rake and VSR.


0.77 EJ Probably similar to that from Cartama Fault (Upper Flat) (in Insua Arévalo, 2008). See referred record on this database.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Active anticline, drainage pattern affected (Insua Arévalo, 2008)



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 250

Página 316 de 632








Unknown






Source Comment



References

Variability



Página 317 de 632



ID: ES728 Fault Name: Socovos (1/2)

Segment Name: Socovos-Calasparra

Location X: -1.72680662

Location Y: 38.23370362

Name of Compiler(s): García-Mayordomo, J.

Filiation: IGME



Average Strike(º): 295 ± 5 LD Baena et al. (1993), Pérez-López et al. (2010), Sánchez-Gómez et al. (2010), Pérez-Valera et al. (2014)

Dip (º): 85 ± 5 EJ Subvertical. Based on Baena et al. (1993), Pérez-López et al. (2010), Sánchez-Gómez et al. (2010), Pérez-Valera et al. (2014).

Rake (º): 180 ± 10 LD Dextral since Tortonian ( Baena et al., 1993). Pérez-López et al. (2010), Sánchez-Gómez et al. (2010), Pérez-Valera et al. (2014).

Sense of Movement: D ± 10 LD Dextral since Tortonian (Baena et al., 1993). Pérez-López et al. (2010), Sánchez-Gómez et al. (2010), Pérez-Valera et al. (2014).

Length (km): 53.0 ± 2 EJ Based on Baena et al (1993), Pérez-López et al (2010) and Sánchez-Gómez et al. (2010). These last authors consider Socovos fault divided into three distinct sectors: Molinicos (15 km), Abejuela (36 km) and Calasparra (28 km)

Min Depth (km): 0 ± 5 LD Outcrops at the surface. Baena et al. (1993), Pérez-López et al. (2010), Sánchez-Gómez et al. (2010), Pérez-Valera et al. (2014)

Max Depth (km): 15.0 LD Given value is seismogenic depth. Fault depth reaches lower crust. Table 4.21 in García-Mayordomo (2005).

Width (km): 15.1 AR

Area (km²): 798.04 AR


Upper Pleistocene

Lower Pleistocene to Upper

LD Based on Baena et al. (1993) and Pérez-Varela et al. (2014). Radiometric dating is necessary.


0.000 EJ Pure dextral strike-slip assumed


0.1 0.04-0.15 EJ Based on Pérez-Valera et al. (2014) estimation at the Abejuela sector: 0.10-0.15 m/ka. Pérez et al. (2010) estimates 0.04 m/ka. Sánchez-Gómez et al. (2010) estimates 0.9-0.3 m/ka since Upper Miocene.


0.1 0.04-0.15 EJ Pure dextral strike-slip assumed


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Deformed Upper Pliocene and Lower Pleistocene? geomorphic levels (travertines and alluvial fans). Consistent surface expression. Likely association to seismicity.

Baena et al. (1993), Pérez-López et al. (2010), Sánchez-Gómez et al. (2010), Pérez-Varela et al. (2014).

Geological Set: Betic Range (Albacete-Murcia)


Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 126

Página 318 de 632




Unknown


7.09 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Pérez-López et al (2010) estimated Mw 6.80 from SRL (40 km) using Wells and Coppersmith (1994) for strike-slip faults.


20088 180255-3731 AR Considering the MEM (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter. Pérez et al. (2010) estimated 60000-30000 yrs based on Slemmons (1982).


Unknown



García-Mayordomo, J. (2005). Caracterización y análisis de la peligrosidad sísmica en el SE de España. Tesis Doctoral. UCM. Madrid. 379 pp.

Pérez-López, R., MA Rodríguez-Pascua, PG Silva, JL Giner-Robles and J García-Mayordomo. (2010). The Socovos Fault as seismic source for earthquake-size M>6-. Tectonic slip-rate from geomorphology and instrumental seismicity (SE Spain). In: Contribución de la Geología al análisis de la Peligrosidad Sísmica. Resúmenes de la 1ª Reunión Ibérica sobre Tectónica Activa y Paleosismología. Sigüenza. España, 27-29 de Octubre, pp 117-120.

Pérez-Varela, L.A., Sánchez-Gómez, M., Azor, A., and Pérez-Varela, F. (2014). Actividad Cuaternaria del sistema de estructuras asociado a la Falla de Socovos (Béticas Orientales). Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España, pp 35-38.

Sánchez-Gómez, M., L.A. Pérez-Valera, F. Pérez-Valera y A. Azor (2010) Segmentación de la falla de Socovos a partir de datos geológicos. Resúmenes de la 1ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Sigüenza, España, pp. 137-140.

Slemons, J. (1982). Determination of desing earthquake magnitudes for mnicrozonation. En: Proceedings of the 3rd International Earthquake Microzonation Conference. Seatle, Washington (USA), pp. 119-130.


Wells, DL and Coppersmith, KJ (1994). New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bull. Sesimol. Soc. Am., 974-1002.




References

Variability





ES728

Calasparra 1941 -1.7361; 38.2348

MSK: VI - Magnitude: 4.1

IGN Catalogue

Spatial correlation Additionally, close to the fault trace relatively deep earthquakes (h>25 km) well located show, which are very likely related to current activity of the fault as this is the deepest tectonic structure in the area (García-Mayordomo (2005) p.273).

659

Página 319 de 632



ID: ES729 Fault Name: Socovos (2/2)

Segment Name: Calasparra-Cieza

Location X: -1.4008

Location Y: 38.22509999


Filiation: IGME



Average Strike(º): 272 ± 5 LD Baena et al. (1993), Pérez-López et al. (2010), Sánchez-Gómez et al. (2010), Pérez-Valera et al. (2014)

Dip (º): 75 ± 10 EJ Based on Baena et al. (1993), Pérez-López et al. (2010), Sánchez-Gómez et al. (2010), Pérez-Valera et al. (2014).

Rake (º): 90 ± 10 EJ Assumed pure reverse. Sánchez-Gómez et al. (2010) interprets the fault zone as a positive flower structure.

Sense of Movement: R LD Baena et al. (1993), Sánchez-Gómez et al. (2010), Pérez-Valera et al. (2014)

Length (km): 36.0 ± 7 LD Pérez-Valera et al. (2014) indicates that the fault trace is offset by minor NE-SW system faults.

Min Depth (km): 0 ± 5 LD Outcrops at the surface. Baena et al. (1993), Pérez-López et al. (2010), Sánchez-Gómez et al. (2010), Pérez-Valera et al. (2014).

Max Depth (km): 15.0 LD Given value is seismogenic depth. Fault depth reaches lower crust. Table 4.21 in García-Mayordomo (2005).

Width (km): 15.5 AR

Area (km²): 559.05 AR


Middle Pleistocene

Lower Pleistocene to Holocene

LD Baena et al. (1993), Pérez-López et al. (2010). Pérez-Valera et al. (2014) indicates that parts of the fault trace are covered by undeformed Upper Pleistocene sediments.


0.097 0.077-0.116 AR From NSR, dip and rake.


0 EJ Pure reverse faulting is assumed.


0.1 0.08-0.12 EJ Based on Pérez et al. (2010), table 1, for reverse kinematics.


Unknown


1 in 5820-3710 yr BP

LD Sánchez-Gómez et al. (2011) interpret a roof-collapse in a archeological outcrop 1 km away from the fault trace as due to the occurrence of an earthquake, dated in between 5820-3710 yr BP, from which the most likely source would be the Socovos fault.

Identification


Quaternary Activity

Variability Source

Comment

Fresh and dramatic surface expression, deformed alluvial fans, possibly deformed colluvial deposits, possible river captures associated to tectonic uplift. Likely association to seismicity.

Baena et al. (1993), Pérez-López et al. (2010), Pérez-Valera et al. (2014)



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 127

Página 320 de 632




Unknown


6.93 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Pérez-López et al (2010) estimated Mw 6.70 from SRL (30 km) using Wells and Coppersmith (1994).


16526 74143-3837 AR Considering the MEM (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter. Pérez et al. (2010) estimated 5000-30000 yrs based on Slemmons (1982).


Unknown



García-Mayordomo, J. (2005). Caracterización y análisis de la peligrosidad sísmica en el SE de España. Tesis Doctoral. UCM. Madrid. 379 pp.

Pérez-López, R., MA Rodríguez-Pascua, PG Silva, JL Giner-Robles and J García-Mayordomo. (2010). The Socovos Fault as seismic source for earthquake-size M>6. Tectonic slip-rate from geomorphology and instrumental seismicity (SE Spain). En: Contribución de la Geología al análisis de la Peligrosidad Sísmica. Resúmenes de la 1ª Reunión Ibérica sobre Tectónica Activa y Paleosismología. Sigüenza. España, 27-29 de Octubre, pp 117-120.

Pérez-Varela, L.A., Sánchez-Gómez, M., Azor, A., and Pérez-Varela, F. (2014). Actividad Cuaternaria del sistema de estructuras asociado a la Falla de Socovos (Béticas Orientales). Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España, pp 35-38.

Sánchez-Gómez, M., L.A. Pérez-Valera, F. Pérez-Valera y A. Azor (2010) Segmentación de la falla de Socovos a partir de datos geológicos. Resúmenes de la 1ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Sigüenza, España, pp. 137-140.

Sánchez-Gómez, M., Martínez-Sánchez, C., García-García, F., Peláez, J.A., Pérez-Valera, F., Martínez-Andreu, M. & Pérez-Valera, L.A., (2011). Evidence for a 4700-2100 BC palaeoearthquake recorded in a fluvial-archaeological sequence of the Segura River, SE Spain. Quaternary International 242, 106–114.

Slemons, J. (1982). Determination of desing earthquake magnitudes for mnicrozonation. En: Proceedings of the 3rd International Earthquake Microzonation Conference. Seatle, Washington (USA), pp. 119-130.






References

Variability





ES729

Cieza 1936 4.5 IGN660

Página 321 de 632



ID: ES730 Fault Name: Pozohondo

Segment Name: Tobarra-Cordovilla

Location X: -1.75799561

Location Y: 38.60510254

Name of Compiler(s): Pérez-López, R., Rodríguez-Pascua, M.A., García-Mayordomo, J., Jiménez-Díaz, A.

Filiation: IGME - Instituto Geológico y Minero de España



Average Strike(º): 113 ± 10 LD Rodríguez-Pascua et al. (2010a)

Dip (º): 75 ± 5 LD Rodríguez-Pascua et al. (2010a)

Rake (º): -120 ± 10 LD Rodríguez-Pascua et al. (2010a)

Sense of Movement: ND ± 10 LD Rodríguez-Pascua et al. (2008, 2010a)

Length (km): 25.0 11-28 LD Lenght of the segment where best evidence of recent activity is found (Tobarra-Cordovilla).Cartographic length of complete fault is more than 75 km.

Min Depth (km): 0 0 LD Surface rupturing; Rodríguez-Pascua et al. (2008)

Max Depth (km): 11.0 ±2 LD From analysis of the rheology of the crust and seismicity depth distribution (García-Mayordomo, 2005).

Width (km): 11.4 AR

Area (km²): 284.70 AR


Holocene LD Rodríguez-Pascua et al. (2012)


0.050 ± 0.02 AR Estimated from net slip and rake, Rodríguez-Pascua et al. (2008, 2009, 2010a, 2012)


0.09 ± 0.02 AR Estimated from net slip and rake, Rodríguez-Pascua et al. (2008, 2009, 2010a, 2012)


0.1 ± 0.02 LD Obtained from palaeoseismic trenching analysis (Holocene); Rodríguez-Pascua et al. (2012). Slip rate for Late Miocene is 0.05 m/ky, and for Middle-Late Pleistocene is 0.06-0.09 m/ky


1.2 80-1.2 LD Max. Slip from last event recorded in trench. Fault scarp maximum height varies from 0.6-1.9 m Rodríguez-Pascua et al. (2008, 2009, 2010a, 2012)


2 in last 8 ka

2 to 3 LD There is also evidence for at least another event younger than 26 ka; Rodríguez-Pascua et al. (2012)


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Coseismic surface rupturing, dammed lakes (Alboraj), deformed fluvial network, topographic lineaments, soil cracks, overturned blocks, crossed alluvial fans, fault scarp.

Rodríguez-Pascua et al. (2008, 2009, 2010a, 2012)

Geological Set: Betic Range (Albacete-Murcia)


Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 128

Página 322 de 632




6.78 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.55 (6.3-6.8) from max. Displacement vs. Mw using Wells and Coppersmith (1994) for normal faults (Rodríguez-Pascua et al., 2012).


7600 6600 to 8600 yr LD Estimated from paleoseismic events; Rodríguez-Pascua et al. (2012). Considering the Maximum Earthquake Model (Wesnousky, 1986) with NSR 0.1 m/ky results 19,300 yrs.


1578 BP +/- 204 yrs LD Average radiocarbon age from 7 samples. Calendric age is between centuries I-VI AD, Rodríguez-Pascua et al. (2012)


Rodriguez-Pascua MA.(1999). Tesis Doctoral. Universidad Complutense de Madrid. 600 pp.

Rodríguez-Pascua MA. (2001). Paleosismicidad y sismotectónica de las cuencas lacustres neógenas del Prebético de Albacete. Instituto de Estudios Albacetenses, 123. Albacete, 285 pp.

Rodríguez-Pascua MA, De Vicente G, Calvo JP and Pérez-López, R.(2003) Similarities between recent seismic activity and paleoseismites during the Late Miocene in the external Betic Chain (Spain). Journal of Structural Geology 25(4): 749-753.

Rodríguez-Pascua MA, Pérez-López R, Calvo JP and del Cura MAG. (2008) Recent seismogenic fault activity in a Late-Quaternary closed-lake graben basin (Albacete, Spain). Geomorphology 102(1): 169-178.

Rodríguez-Pascua MA, Bischoff JL., Garduño-Monroy VH, Pérez-López, R., Ginber-Robles JL, Israde-Alcántara I, Calvo JP and Willians RW. (2009). Estimation of the tectonic slip-rate from Quaternary lacustrine facies within the intraplate Albacete province (SE of Spain). Sedimentary Geology 222(1-2): 89-97.

Rodríguez-Pascua MA, Pérez-López R., Garduño-Monroy VH, Giner-Robles JL and BischoffJL. (2010a). Estudio paleosismico de la falla de Pozohondo. Prebético externo (Albacete, SE de España). En: Contribución de la Geología al análisis de la Peligrosidad Sísmica. Resúmenes de la 1ª Reunión Ibérica sobre Tectónica Activa y Paleosismología. Sigüenza. España, 27-29 de Octubre, pp 117-120.

Rodríguez-Pascua MA, Silva PG, Garduño-Monroy VH, Pérez-López R., Israde-Alcántara I, Giner-Robles JL, Bischoff JL and Calvo JP. (2010b). Ancient earthquakes from archaeoseismic evidence during the Visigoth and Islamic periods in the archaeological site of "Tolmo de Minateda" (SE of Spain). Geological Society of America Special Paper, 471: 171-184.

Rodríguez-Pascua MA, Pérez-López R, Garduño-Monroy VH, Giner-Robles JL, Silva PG, Perucha-Atienza MA, Hernández-Madrigal VM and Bischoff JL. (2012). Paleosesimic and geomorphologic evidence of recent tectonic activity of the Pozohondo Fault (Betic Cordillera, SE Spain). Journal of Iberian Geology, 38(1): 239-251.






References

Variability



Página 323 de 632



ID: ES736 Fault Name: East of Guadix

Segment Name:

Location X: -3.15714548

Location Y: 37.36179807





Average Strike(º): 142 5 LD Calculated from the tips of the trace (Sanz de Galdeano et al.,2012)

Dip (º): 90 LD Average dip as observed at surface (Sanz de Galdeano et al.,2012)



Length (km): 10.8 LD Sanz de Galdeano et al. (2012)

Min Depth (km): 0 LD Sanz de Galdeano et al. (2012)

Max Depth (km): 10.0 ±2 LD Depth of the seismogenic crust in the area: 10 km (García-Mayordomo, 2005).

Width (km): 10.0 AR

Area (km²): 108.00 AR



LD Sanz de Galdeano et al. (2012)


0.020 LD Average value from deformed Quaternary markers (Sanz de Galdeano et al., 2012)




0.02 AR From VSR, dip and rake (pure normal)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

It appears as great vertical joints, partially eroded by the glacis of the Guadix-Baza Basin. Linked geological features are scarce. Seismicity seemingly related.




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 208

Página 324 de 632








Unknown




García-Tortosa, F.J., Alfaro, P., Sanz de Galdeano, C. y Galindo-Zaldívar, J. (2010). Glacis geometry as a geomorphic marker of recent tectonics: The Guadix-Baza Basin (South Spain). Geomorphology, doi.: 10.1016/j.geomorph.2010.10.021








Source Comment



References

Variability



Página 325 de 632



ID: ES737 Fault Name: Benamaurel

Segment Name:

Location X: -2.72914222

Location Y: 37.58480527






Dip (º): 60 LD Sanz de Galdeano et al. (2012)



Length (km): 18.7 LD Inferred from gravity surveying and seismicity data (Sanz de Galdeano et al., 2012)

Min Depth (km): 1 >0 LD Fault revealed from gravity survey (Sanz de Galdeano et al., 2007). The fault has no surface-deformation features associated with it.

Max Depth (km): 10.0 >10 LD Sanz de Galdeano et al. (2012)

Width (km): 10.4 AR

Area (km²): 194.34 AR


Unknown LD Fault deduced from seismicity and gravity surveying (Sanz de Galdeano et al., 2012). It is potentially responsible for the November 16, 2003 (mbLg=4.1, I=IV) SW Benamaurel earthquake.


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

There are no geomorphic evidence. The fault is deduced from seismicity and gravimetric data.

It is antithetic respect to the Baza Fault (Sanz de Galdeano et al., 2012)

Geological Set: Betic Range (Granada, Guadix Basin)

Identification Method: Geophysical methods and seismological techniques

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 209

Página 326 de 632








Unknown












References

Variability





ES737

Benamaurel 16/11/2003 4.1 mblg, IV Peláez et al, 2007661

Página 327 de 632



ID: ES739 Fault Name: Oeste del Negratín

Segment Name:

Location X: -3.00440465

Location Y: 37.59359178





Average Strike(º): 180 LD Calculated from the tips of the trace (Sanz de Galdeano and Peláez, 2007)

Dip (º): 70 LD Average dip as observed at surface (Sanz de Galdeano and Peláez, 2007)

Rake (º): -90 LD Sanz de Galdeano and Peláez (2007)

Sense of Movement: N LD Sanz de Galdeano and Peláez (2007)

Length (km): 7.8 LD Sanz de Galdeano and Peláez (2007)

Min Depth (km): 5 LD Sanz de Galdeano and Peláez (2007)

Max Depth (km): 10.0 > 5 LD Sanz de Galdeano and Peláez (2007)

Width (km): 5.3 AR



Pleistocene LD Sanz de Galdeano and Peláez (2007)


0.200 LD From Quaternary markers (Sanz de Galdeano and Peláez, 2007)






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It affects Pleistocene sediments Sanz de Galdeano and Peláez (2007)



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 211

Página 328 de 632








Unknown











References

Variability



Página 329 de 632



ID: ES741 Fault Name: Sencelles

Segment Name:

Location X: 2.804

Location Y: 39.601

Name of Compiler(s): García-Mayordomo, J., Martín-Banda, R.

Filiation: IGME, UCM



Average Strike(º): 050 45-60 LD Silva et al. (2001), Mas et al (2014)

Dip (º): 75 70-80 LD Silva et al. (2001)

Rake (º): 45 EJ Based on Mas et al (2014)

Sense of Movement: SR LD It is interpreted as a left-lateral strike-slip fault zone since Upper Miocene-Pliocene (Mas et al., 2014).

Length (km): 22.5 LD Silva et al. (2001)

Min Depth (km): 0 LD Outcrops at the surface. Silva et al. (2001), Mas et al (2014)

Max Depth (km): 10.0 LD Silva et al. (2001)

Width (km): 10.4 AR

Area (km²): 232.94 AR


<780 ka Holocene LD Silva et al. (2001) indicates deformation very likely reaches Holocene.


0.180 0.003-0.35 EJ Based on Silva et al. (2001) data on Portol doline (2.56 m / 780 ka) and Sta. Eugènia (3.5 m/ 10 ka) assuming thrown is given as vertical offsets. Preferred value is the average.






0.275 0.4-0.15 LD Silva et al. (2001). It is assumed that they are vertical displacements.


5 3-9 EJ Based on Silva et al. (2001) estimations of displacement/event.


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Surface expression, fresh morphology scarps, faulted Quaternary sediments, possible association to seismicity.

Silva et al. (2001), Giménez (2003), Mas et al. (2014)

Geological Set: Betic Cordillera (Mallorca)

Identification Method: Geological/geomorphological field mapping

Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 259

Página 330 de 632






6285 903-148889 AR Considering the MEM (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter. Silva et al. (2001) indicates 70-90 yrs based on historical seismicity.


1851 LD According to Silva et al. (2001). See also Giménez (2003).


Giménez, J. 2003. Nuevos datos sobre la actividad post-Neógena en la Isla de Mallorca. Geogaceta, 33, 79-82.

Giménez, J. & Gelabert, B. 2002. Análisis de la actividad tectónica reciente en la isla de Mallorca. In: III Asamblea Hispano-Portuguesa de Geodesia y Geofísica, Valencia, Vol 1, 390-394.

Mas, G., Gelabert, B., and Fornós, J.J. (2014). Evidencias de desplazamiento direccional de la fallaa de Sencelles (Mallorca, Isalas Baleares). Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España, 47-50.

Silva, P.G., González Hernández, F.M., Goy, J.L., Zazo, C. and Carrasco, P. (2001). Paleo and historical seismicity in Mallorca (Baleares, Spain): a preliminary approach. Acta Geológica Hispánica, 36 (3-4), 245-266.


Source Comment



References

Variability





ES741

Palma earthquake, 1851

15-05-1851 02,48,00E-39,36,00N

VIII MSK IGN and Galbis (1932)

Seismic sequence lasted for more than 6 months Silva et al. (2001).

668

ES741

Sencelles, 1764 26-05-1764 03,00,0E-39,36,0N

unknown IGN According to Silva et al. (2001), Table 1.

669

ES741

Sencelles, 1921 22-10-1921 02,54,00E; 39,39,00N

IV ING According to Silva et al. (2001), Table 1.

671

ES741

Sencelles, 1996 09-04-1996 02,55,6E; 39,38,8N

II-III IGN According to Silva et al. (2001), Table 1.

672

Página 331 de 632



ID: ES743 Fault Name: West Cabezo Gordo (Murcia - Mar Menor)

Segment Name:

Location X: -1.01373478

Location Y: 37.86994441


Filiation: IGME



Average Strike(º): 140 ± 10 LD Compiler's measurement, based on the Record number 111 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b), following the right-hand rule.

Dip (º): 60 EJ García-Mayordomo (2005).

Rake (º): -90 LD Record number 111 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Sense of Movement: N LD Record number 111 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Length (km): 30.9 ± 0.2 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).

Min Depth (km): 0.02 ± 0.005 EJ Based on the Plio-Quaternary Isopach Map of the Campo de Cartagena and Guadalentín Basins (ITGE, 1993a).

Max Depth (km): 8.0 LD 8 km is the depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005).

Width (km): 9.2 AR

Area (km²): 284.73 AR


Upper Pleistocene

LD Record number 111 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


0.075 LD Record number 111 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


0 EJ Assuming pure normal slip.


0.087 ± 0.01 AR Assuming pure normal slip and using VSR, Dip and Rake.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Topographic lineament 2) Threshold between San Pedro del Pinatar Basin and Torrepacheco Basin.

Record number 111 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


Identification Method: Geomorphological mapping and geophysics

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 152

Página 332 de 632




Unknown






Unknown



ITGE (1993a): Mapa Neotectónico, Sismotectónico y de Actividad de Fallas de la Región de Murcia (Escalas 1:200.000 y 1:100.000).

ITGE (1993b): Fichero de Fallas del Mapa Neotectónico, Sismotectónico y de Actividad de Fallas de la Región de Murcia (Escalas 1:200.000 y 1:100.000).






References

Variability



Página 333 de 632



ID: ES744 Fault Name: Cartagena-2

Segment Name:

Location X: -0.72498855

Location Y: 37.75026723


Filiation: IGME



Average Strike(º): 258 ± 5 EJ Compiler's measurement, based on the Record number 114 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b), following the right-hand rule.


Rake (º): 90 EJ García-Mayordomo (2005).

Sense of Movement: R EJ García-Mayordomo (2005).



Max Depth (km): 8.0 EJ Its maximum depth should be within the upper crust. 8 km is the depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005).

Width (km): 9.2 AR

Area (km²): 193.50 AR


Gelasian (Early Pleistocene)



Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Controls on early Pleistocene sedimentation 2) Tilting Record number 114 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Geological Set: Betics (Murcia)

Identification Method: Geological, geomorphological field mapping and geophysics

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 153

Página 334 de 632




Unknown






Unknown









References

Variability



Página 335 de 632



ID: ES745 Fault Name: El Cantal

Segment Name:

Location X: -1.60692076

Location Y: 37.45738574


Filiation: IGME




Dip (º): 80 90 to 60 EJ García-Mayordomo (2005).


Sense of Movement: NS LD Record number 119 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


Min Depth (km): 0 EJ It outcrops at the surface (ITGE, 1993a).

Max Depth (km): 8.0 EJ Its maximum depth should be within the upper crust. 8 km is the depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005).

Width (km): 8.1 AR



Holocene EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


0.050 0.05-0.09 LD The Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


0.051 0.051-0.091 AR Using NSR and Rake


0.072 0.072-0.129 AR Using VSR, Dip and Rake


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Deformed Quaternary alluvial fans 2) Scarp 3) Tilting 4) Overlaps 5) Abrupt changes in the profile of the hydrographic network 6) Triangular facets



Identification Method: Geological and geomorphological field mapping

Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 154

Página 336 de 632




Unknown






Unknown










References

Variability



Página 337 de 632



ID: ES746 Fault Name: Garrovilla

Segment Name:


Location Y: 37.45352314


Filiation: IGME









Max Depth (km): 5.0 5-8 EJ 8 km is the depth of the depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005). However, the short length of the fault suggests that is a secondary fault, not likely to

Width (km): 5.0 AR



Upper Pleistocene





0 0 EJ Assuming pure normal slip




Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Tilting 2) Topographic lineament 3) Controls on the Quaternary outcrops 4) Inflections of the river network




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 155

Página 338 de 632




Unknown






Unknown










References

Variability



Página 339 de 632



ID: ES747 Fault Name: Llano de las Cabras

Segment Name:

Location X: -1.77227249



Filiation: IGME




Dip (º): 45 ± 10 LD Record number 122 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).





Max Depth (km): 5.0 5-11 EJ Its maximum depth should be the main detachment level at the base of the sedimentary cover. 11 km is the fragile-ductile transition in the Central Betic Crustal Block (García-Mayordomo, 2005).

Width (km): 7.1 AR



Middle Pleistocene

EJ Deduced from the local geology.


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Faceted faces 2) Tilting 3) Inflections of the river network Record number 122 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


Identification Method: Geomorphological field mapping

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 156

Página 340 de 632




Unknown






Unknown









References

Variability



Página 341 de 632



ID: ES748 Fault Name: Mazarrón Norte

Segment Name:

Location X: -1.32954952

Location Y: 37.61920566


Filiation: IGME






Sense of Movement: NS LD Record number 123 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).



Max Depth (km): 8.0 EJ 8 km is the depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005).

Width (km): 8.0 AR

Area (km²): 128.49 AR


Upper Pleistocene



Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Tilting 2) Overlaps 3) Dissection of the slopes 4) Hanging valleys




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 157

Página 342 de 632








Unknown









References

Variability



Página 343 de 632



ID: ES749 Fault Name: Hinojar

Segment Name:

Location X: -1.44766216

Location Y: 37.69679325


Filiation: IGME





Rake (º): 45 EJ The Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).

Sense of Movement: SR EJ The Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).




Width (km): 11.3 AR



Early Pleistocene

EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Triangular facets 2) Tilting 3) Overlaps Record number 128 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 158

Página 344 de 632




Unknown






Unknown









References

Variability



Página 345 de 632



ID: ES750 Fault Name: La Puebla

Segment Name:

Location X: -0.72265022

Location Y: 37.71215697


Filiation: IGME








Min Depth (km): 0.02 ± 0.005 EJ Based on Plio-Quaternary Isopach Map of the Campo de Cartagena and Guadalentín Basins (ITGE, 1993a).


Width (km): 9.2 AR

Area (km²): 276.44 AR


Tyrrhenian Terrace III

80-10 ky EJ Record number 131 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).




0 EJ Assuming pure normal slip


0.081 ± 0.01 AR Using VSR, Dip and Rake.


Unknown


3 LD 3 instrumental seismic events with 4.2 Mw (Record number 131 from ITGE (1993b)).

Identification


Quaternary Activity

Variability Source

Comment

1) It marks the axis of maximum subsidence of the Mar Menor Basin during Quaternary 2) Drainage pattern 3) Offset channels 4) Fluvial captures




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 159

Página 346 de 632




Unknown






Unknown










References

Variability





ES750

Mar Menor West Event

Max Mag 4.2 IGN Spatial association ITGE (1993b) reports 3 instrumental events likely related to this fault (record number 131).

682

Página 347 de 632



ID: ES751 Fault Name: Falla del Chopillo

Segment Name:


Location Y: 38.25853737


Filiation: IGME




Dip (º): 40 + 10 LD Record number 133 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).





Max Depth (km): 11.0 11-5 EJ 11 km is the depth of the fragile-ductile transition in the Prebetic Crustal Block (García-Mayordomo, 2005). 5 km is the estimated maximum depth of the main detachment level or thickness of the

Width (km): 17.1 AR

Area (km²): 179.17 AR


Middle Pleistocene

EJ Inferred from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Tilting, dissection and overlapping of the early-middle Pleistocene alluvial fans




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 160

Página 348 de 632




Unknown






Unknown









References

Variability



Página 349 de 632



ID: ES752 Fault Name: Sucina - El Estacio

Segment Name:


Location Y: 37.89410996


Filiation: IGME




Dip (º): 85 ± 5 EJ García-Mayordomo (2005)


Sense of Movement: D EJ Record number 134 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).



Max Depth (km): 8.0 EJ 8 km is the depth of the fragile-ductile transition in the Cartagena Block (García-Mayordomo, 2005). According to geophysics the fault reaches the basement (Record number 134 from IGTE, 1993b).

Width (km): 8.0 AR

Area (km²): 199.46 AR


Tyrrhenian (Upper Pleistocene)



Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Hanging valleys 2) Inflections of the river network 3) It affects eolian Tyrrhenian deposits



Identification Method: Geological, geomorphological field mapping and geophysical methods

Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 161

Página 350 de 632




Unknown






Unknown









References

Variability



Página 351 de 632



ID: ES753 Fault Name: Cartagena-1 (Murta - Cartagena)

Segment Name:

Location X: -1.08736936

Location Y: 37.70371662


Filiation: IGME






Sense of Movement: DN LD Record number 135 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Length (km): 17.1 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).



Width (km): 9.2 AR

Area (km²): 157.20 AR


90 ky 80 to 105 ky EJ Tyrrhenian III. Record number 135 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).






0.098 ± 0.01 AR From VSR, dip and rake


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Deformed alluvial fans 2) Fluvial captures 3) Inflections of the river network (it displaces the E-W Rambla Fuente Álamo towards the South ) 4) Subsidence at its SE edge (responsible for creating the Almarjal lagoon complex).




Comment


B+*Strength Class:


Paleoearthquakes

Orden Visual: 162

Página 352 de 632




Unknown






Unknown










References

Variability





ES753

Campo de Cartagena NW

Cluster

1985-2002 mbLg=1.8-3.0 IGN catalogue from 1985

to 2002

Spatial association García-Mayordomo, 2005, p.172, fig.3.2.1 and ITGE, 1993a,b (record num. 135)

683

Página 353 de 632



ID: ES754 Fault Name: Corvera

Segment Name:

Location X: -1.13684482

Location Y: 37.84858317


Filiation: IGME





Rake (º): 90 LD Record number 137 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Sense of Movement: R LD Record number 137 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).




Width (km): 13.9 AR

Area (km²): 285.49 AR


Upper Pleistocene



Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Tilting 2) Superposition of different alluvial fan systems along the mountain front of the Villares Range




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 163

Página 354 de 632




Unknown






Unknown









References

Variability





ES754

1998 and 2002 seismic series SE

Murcia

27-28/10/1998

and 27-28/04/2002

mbLg max 3.0 IGN catalogue from 1985

to 2002

Spatial correlation - NW-SE alignment

García-Mayordomo, 2005, p.172, fig.3.2.1

684

Página 355 de 632



ID: ES755 Fault Name: Rebate

Segment Name:

Location X: -1.02134992

Location Y: 37.899


Filiation: IGME





Rake (º): -90 EJ Error in the original record number 138 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).





Width (km): 9.7 AR

Area (km²): 104.72 AR


Early Pleistocene



Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Tilting Record number 138 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 164

Página 356 de 632




Unknown






Unknown









References

Variability





ES755

1998 and 2002 seismic series SE

Murcia

27-28/10/1998

and 27-28/04/2002

mbLg max 3.0 IGN catalogue from 1985

to 2002

Spatial correlation - NW-SE alignment

García-Mayordomo, 2005, p.172, fig.3.2.1

685

Página 357 de 632



ID: ES756 Fault Name: La Galera

Segment Name:

Location X: -1.56633812

Location Y: 37.50371048


Filiation: IGME










Width (km): 8.1 AR



130 ky LD Record number 141 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).






0.072 0.072-0.129 AR Using VSR, Rake and Dip


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It controls the direction of the Quaternary delta fans 2) Topographic lineament 3) Tilting 4) Overlaps 5) Abrupt changes in the profile of the hydrographic network




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 165

Página 358 de 632




Unknown






Unknown










References

Variability



Página 359 de 632



ID: ES757 Fault Name: Lomas de Cliler - Avilés Sur

Segment Name:

Location X: -1.71030334

Location Y: 37.96405544


Filiation: IGME




Dip (º): 45 + 10 LD Record number 60 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).





Max Depth (km): 5.0 5-11 EJ 5 km is the estimated maximum depth of the main detachment level or thickness of the Mesozoic sedimentary cover. 11 km is the depth of the fragile-ductile transition in the Central Betic Crustal Block (García-

Width (km): 7.1 AR



Middle Pleistocene

EJ Observed on of the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It affects the formation of alluvial cones 2) Fault scarps 3) Faceted faces 4) Tilting 5) Overlapping slopes 6) Inflections of the river network




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 166

Página 360 de 632




Unknown






Unknown









References

Variability



Página 361 de 632



ID: ES758 Fault Name: West of Carche

Segment Name:


Location Y: 38.42376366


Filiation: IGME




Dip (º): 40 to 50 LD Record number 149 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).





Max Depth (km): 5.0 5-11 EJ Its maximum depth should be the main detachment level at the base of the sedimentary cover. 11 km is the fragile-ductile transition in the Prebetic Crustal Block (García-Mayordomo, 2005).

Width (km): 7.8 AR



Middle Pleistocene

EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Tilting and dissection of the Early-Middle Pleistocene alluvial fans 2) Clear topographic lineament in remote sensing imagery and DEMs




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 167

Página 362 de 632




Unknown






Unknown









References

Variability



Página 363 de 632



ID: ES759 Fault Name: Las Lomas System

Segment Name:

Location X: -1.37092159



Filiation: IGME



Average Strike(º): 150 ± 10 LD Compiler's measurement, based on the Geological Map of Spain Memory, Digital Edition, Sheet number 954 - Totana (Leyva et al., 2004), following the right-hand rule.


Rake (º): -45 (-045) to (-090) EJ Observed on the Geological Map of Spain, Digital Edition, Sheet number 954 - Totana (Leyva et al., 2004)

Sense of Movement: NS NS to N EJ Observed on the Geological Map of Spain, Digital Edition, Sheet number 954 - Totana (Leyva et al., 2004)

Length (km): 6.5 ± 0.5 EJ It is a small fault system with a width of 5.3 km and a maximum length of 6.5 km. Observed on the Geological Map of Spain, Digital Edition, Sheet number 954 - Totana (Leyva et al., 2004)


Max Depth (km): 5.0 5-8 EJ 8 km is the depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005). However, the short length of the fault suggests that is a secondary fault, not likely to reach the F-

Width (km): 5.1 AR



Early Pleistocene

LD Observed on the Geological Map of Spain, Digital Edition, Sheet number 954 - Totana (Leyva et al., 2004)


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It determines the morphology of Saladillo Scarp 2) Associated gravitational processes

Geological Map of Spain Memory, Digital Edition, Sheet number 954 - Totana (Leyva et al., 2004)



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 168

Página 364 de 632




Unknown






Unknown


Garcia-Mayordomo, J. (2005). Caracterización y Análisis de la Peligrosidad Sísmica en el Sureste de España. Tesis Doctoral, Universidad Compultense de Madrid, 373 pp.

Leyva, F., Silva, P.G., García-Tortosa, F.J., Roldán, F.J. and Nozal, F. (2004). Mapa Geológico de España,Edición Digital, Hoja núm.954 (Totana).





References

Variability



Página 365 de 632



ID: ES760 Fault Name: Los Tollos

Segment Name:

Location X: -1.44877532

Location Y: 37.72121719





Average Strike(º): 037 ± 5 LD Insua-Arévalo et al (submitted).

Dip (º): 85 80-90 LD Mapped previously as a normal fault dipping to the NW (Silva, 1994; Leyva Cabello et al., 2010), Insua-Arévalo et al (submitted) shows that it is a high angle (sub-vertical) southeast dipping fault.

Rake (º): 15 ± 5 LD As measured in trenches, Insua-Arévalo et al (submitted).

Sense of Movement: S LD Left-lateral strike slip fault with reverse component, as seen in trenches (Insua-Arévalo et al, submitted).

Length (km): 15.0 ± 2 LD Previously interpreted as the SW extension of the Carrascoy Fault (I.-Arévalo et al 2012). I.-Arévalo et al (subm.) interprets it as an independent fault extending SW under Gualentín Dep., as revealed in seismic profiles (Martínez del Olmo, 2006).

Min Depth (km): 0 0-0.01 LD Outcrops at the surface, though its extension to the SW may be covered partially by Guadalentin Depression Holocene filling (Insua-Arévalo et al, submitted).

Max Depth (km): 8.0 LD Depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005).

Width (km): 8.0 AR

Area (km²): 120.46 AR


Holocene LD Silva, 1994; Leyva Cabello et al., 2010; Insua-Arévalo et al (submitted) have dated sediments affected by the fault as recent as 2350 BP.


0.041 0.015-0.064 AR From NSR, dip and rake




0.16 0.06-0.25 LD Preferred value is the average from maximum and minimum NSR as shown in Insua-Arévalo et al (submitted).


0.46 0.386-0.541 LD Preferred value is the average from maximum and minimum, based on Insua-Arévalo et al (submitted).

Identification


Quaternary Activity

Variability Source

Comment

1) Fault scarp in Quaternary deposits, 2) Control on drainage network

Silva, 1994; Leyva Cabello et al., 2010; Insua-Arévalo et al (submitted). The evidence is mostly concentrated in the NE section of the fault.



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 169

Página 366 de 632




at least 2 in the last 9 ky

3 to 4 LD Insua-Arévalo et al (submitted).


EJ No evidence found.


6.57 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Considering Wells and Coppersmith (1994) results Mw 6.2-6.7 (Insua-Arévalo et al, subm.)


4530 6860-2200 LD Preferred value is the average from maximum and minimum RI from Insua-Arévalo et al, subm.) paleoseismological research. Considering the MEM (Wesnousky, 1986) results 13767 yrs (using 0.16 m/ky and Mw 6.57).


between 2740-2140 BP

LD Insua-Arévalo et al. (submitted).


García-Mayordomo, J. (2005). Caracterización y Análisis de la Peligrosidad Sísmica en el Sureste de España. Tesis Doctoral, Universidad Complutense de Madrid, 373 pp.

Insua-Arévalo, J.M., García-Mayordomo, J., Salazar, A., Rodríguez-Escudero, E., Martín-Banda, R., Álvarez-Gómez, J.A., Canora, C. and Martínez-Díaz, J.J. (submitted): Paleoseismological evidence of Holocene activity in Los Tollos Fault (Murcia, SE Spain): A new relevant feature of the Eastern Betic Shear Zone. Geomorphology.

Insua-Arévalo, J.M., García-Mayordomo, J., Salazar, A., Rodríguez-Escudero, E., Martínez-Díaz, J.J., Álvarez-Gómez, J.A., Canora, C., Martín-Banda, R., Pérez-López, R., Rodríguez-Pascua, M.A. (2012). Actividad holocena y pleistocena de la falla de Carrascoy, Murcia. Resultados preliminares de un análisis paleosísmico. Geotemas. 13, 1511-1514.

Leyva Cabello, F., Silva Barroso, P.G., García Tortosa, F.J. (2010). Cartografía Geológica de la hoja 954 Totana, Mapa Geológico Digital de España E. 1:50.000. Instituto Geológico y Minero de España, Madrid, España.

Martínez del Olmo, W., Klimowitz, J., Hernández, E., 2006. El despegue extensional mioceno de la zona de falla de Alhama de Murcia. Boletín Geológico y Minero. 117 (3), 363-377.

Silva, P.G., 1994. Evolución Geodinámica de la depresión del Guadalentín (Murcia) desde el Mioceno Superior hasta la actualidad: Neotectónica y Geomorfología. Ph.D. Tesis, Universidad Complutense de Madrid, Spain.





References

Variability



Página 367 de 632



ID: ES761 Fault Name: Falla de Águilas

Segment Name:

Location X: -1.47692219

Location Y: 37.43738815


Filiation: IGME



Average Strike(º): 250 ± 20 LD Compiler's measurement, based on the Records number 22, 139, 140 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b), following the right-hand rule.

Dip (º): 90 ± 5 LD Records numbers 22, 139 and 140 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Rake (º): -45 LD Records numbers 22, 139 and 140 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Sense of Movement: NS LD Records numbers 22, 139 and 140 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Length (km): 15.2 ± 0.2 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a). Lenght is the sum of three distinct faults aligned in N60 direction.


Max Depth (km): 5.0 5-8 EJ 8 km is the depth of the depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005). However, the length of single faults suggests that is a secondary fault system fault,

Width (km): 5.0 AR



130 Ky LD Record number 22 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


0.040 0.04-0.09 AR Record number 22 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).






Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Scarp 2) Tilting 3) Overlaps 4) Topographic lineament 5) Hanging valleys




Comment


C*Strength Class:


Orden Visual: 170

Página 368 de 632




Unknown


Unknown






Unknown










References

Variability



Paleoearthquakes

Página 369 de 632



ID: ES762 Fault Name: Ramonete

Segment Name:

Location X: -1.42947224

Location Y: 37.54206164


Filiation: IGME







Length (km): 5.0 ± 0.05 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a). 5 km is the length onshore, fault may extend further offshore.


Max Depth (km): 5.0 5-8 EJ 8 km is the depth of the depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005). However, the short length of the fault may suggest that is a secondary fault, not

Width (km): 5.1 AR



Middle Pleistocene



Unknown


Unknown



Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Deforms Rambla de Ramonete delta fans 2) Topographic lineament 3) Scarp 4) Drainage pattern




Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 171

Página 370 de 632




Unknown


Unknown






Unknown









References

Variability



Página 371 de 632



ID: ES763 Fault Name: Bolmueva

Segment Name:

Location X: -1.34330797

Location Y: 37.56056217


Filiation: IGME







Length (km): 9.5 ± 0.2 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a). 10 km is the length onshore, fault may extend further offshore.


Max Depth (km): 8.0 EJ 8 km is the depth of the depth of the fragile-ductile transition in the Cartagena Crustal Block (García-Mayordomo, 2005).

Width (km): 16.0 AR

Area (km²): 152.00 AR


Upper Pleistocene



Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Scarp Record number 29 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


Identification Method: Geological field mapping

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 172

Página 372 de 632




Unknown






Unknown









References

Variability



Página 373 de 632



ID: ES764 Fault Name: West of Pericay - Gigantes

Segment Name:

Location X: -1.97548288

Location Y: 37.80221919


Filiation: IGME









Max Depth (km): 5.0 EJ 5 km is the estimated maximum depth of the main detachment level or thickness of the Mesozoic sedimentary cover (García-Mayordomo, 2005).

Width (km): 5.0 AR



Upper Pleistocene

EJ Observed on of the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Scarps 2) Tilting Record number 40 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 173

Página 374 de 632




Unknown






Unknown









References

Variability





ES764

Valdeinfierno events

Max mag 3.3 IGN Spatial ITGE, 1993a,b reports 3 events possibly related to the fault (record num. 40)

686

Página 375 de 632



ID: ES767 Fault Name: El Sabinar

Segment Name:

Location X: -2.15150008

Location Y: 38.20798884


Filiation: IGME




Dip (º): 85 ± 5 EJ Variable dips both west and east, according to the section of the fault. Mainly it been considered that dips westward (Record number 43 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b)).



Length (km): 5.7 ± 0.2 LD Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Max Depth (km): 5.0 EJ 5 km is the estimated maximum depth of the main detachment level or thickness of the Mesozoic sedimentary cover (García-Mayordomo, 2005).

Width (km): 5.0 AR



Holocene EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Unknown


Unknown



Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Scarps 2) Subsiding area Record number 43 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 176

Página 376 de 632




Unknown


Unknown






Unknown









References

Variability



Página 377 de 632



ID: ES768 Fault Name: Archivel

Segment Name:

Location X: -1.97021335

Location Y: 38.05099458


Filiation: IGME




Dip (º): 90 LD Record number 44 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Rake (º): -135 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).

Sense of Movement: DN EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Min Depth (km): 0 EJ Joints observed in Pliocene and Pleistocene deposits (Record number 44 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b)).

Max Depth (km): 5.0 5-11 EJ 5 km is the estimated maximum depth of the main detachment level or thickness of the Mesozoic sedimentary cover. 11 km is the depth of the fragile-ductile transition in the Prebetic Crustal Block (García-

Width (km): 5.0 AR



Middle Pleistocene



Unknown


Unknown



Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Dissection of the hydrographic network 2) Depressed area Record number 44 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


Identification Method: Geomorphological field mapping and geophysical methods

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 177

Página 378 de 632




Unknown


Unknown






Unknown









References

Variability



Página 379 de 632



ID: ES769 Fault Name: La Junquera-Mancheño

Segment Name:

Location X: -2.14367993

Location Y: 37.89777986


Filiation: IGME




Dip (º): 85 ± 5 EJ García-Mayordomo (2005)

Rake (º): -135 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).

Sense of Movement: DN EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Min Depth (km): 0 EJ Pleistocene sediments are affected by the fault.


Width (km): 5.0 AR



Early Pleistocene



0.190 0.19-0.40 EJ Using NSR, Rake and Dip


0.2 0.2-0.40 EJ Record number 45 from ITGE (1993a,b). In that file a horizontal thrown of aprox.1 km accumulated since Plio-Q times is reported. We think that must be an erratum as it would draw an unrealistic 0.40 m/ka HSR. We assume Pliocene times.


0.28 0.28-0.56 EJ Using Rake and HSR


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Fault scarps 2) fluvial dissection Record number 45 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 178

Página 380 de 632




Unknown






Unknown









References

Variability



Página 381 de 632



ID: ES770 Fault Name: Tarragoya

Segment Name:


Location Y: 37.92066944


Filiation: IGME






Sense of Movement: D LD Record number 47 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Length (km): 22.5 ± 0.2 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a). This fault likely belongs to the Crevillente Shear Zone (Sector Murcia).

Min Depth (km): 0 EJ Pleistocene sediments are affected.

Max Depth (km): 15.0 11-15 EJ This fault likely belongs to the Crevillente Shear Zone (Sector Murcia). Maximum depth is the estimation for the Crevillente Fault (see Table 4.21 in García-Mayordomo, 2005). 11 km is the depth of the F-D

Width (km): 15.0 AR

Area (km²): 337.50 AR


Early Pleistocene



Unknown


Unknown



Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Dissection of the hydrographic network 2) Tilting slopes Record number 47 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


Identification Method: Geological and geomorphological field mapping and geophysical methods

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 179

Página 382 de 632




Unknown


Unknown






Unknown









References

Variability



Página 383 de 632



ID: ES771 Fault Name: Caravaca - Singla

Segment Name:

Location X: -1.92852373

Location Y: 38.01423372


Filiation: IGME






Sense of Movement: S LD Record number 51 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Length (km): 8.6 ± 0.3 LD Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).

Min Depth (km): 0 EJ Fault scarps are observed on the DEMs.


Width (km): 5.0 AR



Upper Pleistocene



Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Conspicuous topographic lineament in remote sensing imagery and DEMs 2) Fault scarps




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 180

Página 384 de 632




Unknown






Unknown









References

Variability





ES771

Cehegín Cluster Since 1941 Max I MSK=VII / M=5.0 (1948,

Cehegín)

IGN catalogue from 1985

to 2002

Spatial association Three seismic series in 1941, 1948 and 1953. Faults Loma de Yegüas and La Encarnación are also candidates. García-Mayordomo, 2005, p.177, fig.3.13 and ITGE (1993a,b) record num. 51

687

Página 385 de 632



ID: ES772 Fault Name: Loma de Yeguas - Cañada Lengua

Segment Name:

Location X: -1.86814322

Location Y: 38.06491922


Filiation: IGME




Dip (º): 85 ± 5 EJ García-Mayordomo (2005).



Length (km): 17.5 ± 0.5 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a). This fault may belong to the Crevillente Shear Zone (Sector Murcia).

Min Depth (km): 0 EJ Fault scarps are observed on the DEMs.

Max Depth (km): 11.0 11-15 EJ This fault may belong to the Crevillente Shear Zone (Sector Murcia). Maximum depth is the estimation for the Crevillente Fault (see Table 4.21 in García-Mayordomo, 2005). 11 km is the depth of the F-D

Width (km): 11.0 AR

Area (km²): 192.68 AR


Middle Pleistocene



Unknown


Unknown



Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Fault scarps 2) Tilting slopes 3) Dissection of the hydrographic network



Identification Method: Geomorphological field mapping and geophysical methods

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 181

Página 386 de 632




Unknown


Unknown






Unknown









References

Variability





ES772


Cehegín)


to 2002

Spatial association Three seismic series in 1941, 1948 and 1953. Faults Caravaca and La Encarnación are also candidates. García-Mayordomo, 2005, p.177, fig.3.13 and ITGE (1993a,b) record num. 51

688

Página 387 de 632



ID: ES773 Fault Name: La Encarnación

Segment Name:


Location Y: 38.03335594


Filiation: IGME










Width (km): 5.8 AR



Early Pleistocene



Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Fault scarps Record number 54 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 182

Página 388 de 632




Unknown






Unknown









References

Variability





ES773


Cehegín)


to 2002

Spatial association Three seismic series in 1941, 1948 and 1953. Faults Loma de Yegüas and Caravaca are also candidates. García-Mayordomo, 2005, p.177, fig.3.13 and ITGE (1993a,b) record num. 51

689

Página 389 de 632



ID: ES774 Fault Name: Segura Medio Fault System (1/2)

Segment Name: Molina de Segura

Location X: -1.23996194

Location Y: 38.10007176


Filiation: IGME








Min Depth (km): 0.01 ± 0.005 EJ Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).

Max Depth (km): 11.0 11-5 EJ 11 km is the depth of the fragile-ductile transition in the Central Betic or Prebetic Crustal blocks (García-Mayordomo, 2005). 5 km is the estimated max. Depth of the main detachment level or thickness of

Width (km): 15.5 AR

Area (km²): 214.33 AR





Unknown


Unknown



Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Overlaps 2) Geographic lineament Record number 142 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


Identification Method: Geomorphological field mapping and geophysics

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 183

Página 390 de 632




Unknown


Unknown






Unknown









References

Variability





ES774

Segura Medio Southern Cluster

since 1883 max I=VIII (Lorquí, 1911),

max m=4.1 (Alcant,1995)


to 2002

Spatial - 1995 Alcantarilla seismic

series

García-Mayordomo, 2005, p.143, fig.3.17 and ITGE, 1993a,b (record num. 142)

690

Página 391 de 632



ID: ES775 Fault Name: Segura Medio Fault System (2/2)

Segment Name: Abarán

Location X: -1.45235143

Location Y: 38.21719428


Filiation: IGME




Dip (º): 90 (60 to 90) EJ Inferred from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).

Rake (º): -135 ± 5 LD Record number 64 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Sense of Movement: DN ± 5 LD Record number 64 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).

Length (km): 14.0 ± 1 EJ Lenght of the Abarán Fault, that belongs to the Segura Medio Fault System. Observed on the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a).


Max Depth (km): 11.0 11-5 EJ 11 km is the depth of the fragile-ductile transition in the Central Betic or Prebetic Crustal blocks (García-Mayordomo, 2005). 5 km is the estimated max. depth of the main detachment level or thickness of the

Width (km): 11.0 AR

Area (km²): 154.00 AR


Holocene LD Record number 64 from the Neotectonic, Seismotectonic and Activity of Faults Map of the Región de Murcia (ITGE, 1993a,b).


Unknown


Unknown



Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Tilting of the Upper Tortonian - Messinian materials, also affecting Quaternary river terrace deposits near Abarán village 2) Dissection of the Segura river 3) Springs at 40ºC




Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 184

Página 392 de 632




Unknown


Unknown






Unknown









References

Variability





ES775

Segura Medio Northern Cluster

Since 1908 Max I MSK=VII (Ojos, 1908)

Max M=4 (Archena, 1951)


to 2002

Spatial association García-Mayordomo, 2005, p.143, fig.3.17 and ITGE, 1993a,b (record num. 64)

691

Página 393 de 632



ID: ES776 Fault Name: Sur de la Sierra de la Demanda

Segment Name:

Location X: -3.25695636

Location Y: 42.14533047





Average Strike(º): 090 ± 2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), following the right-hand rule.

Dip (º): 60 ± 20 EJ Typical dip of normal faults.

Rake (º): -90 LD IGME and ENRESA (1998b)

Sense of Movement: N LD IGME and ENRESA (1998b)

Length (km): 20.5 ± 0.2 LD Observed on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a)

Min Depth (km): 0 LD Observed on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a)

Max Depth (km): 12.0 EJ Depths assigned to the seismicity in the region typically range between 5 and 15 km, and are always less than 25 km (IGN,2010). That's consistent with the brittle layer above a basal detachment level,

Width (km): 13.9 AR

Area (km²): 284.06 AR


Early Pleistocene (Gelasian)

2580-1800 ka LD IGME and ENRESA (1998b)


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Topographic lineament 2) Fault scarp 3) It controls the sedimentation of thick Plio-Quaternary materials

IGME and ENRESA (1998b).

Geological Set: Iberian Range (Burgos-La Rioja)


Comment


C+*Strength Class:


Paleoearthquakes

Orden Visual: 109

Página 394 de 632




Unknown






Unknown








References

Variability



Página 395 de 632



ID: ES777 Fault Name: Badules

Segment Name:

Location X: -1.19061401

Location Y: 41.11428559












Width (km): 13.9 AR

Area (km²): 146.88 AR





Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It offsets the Fundamental Erosion Surface of the Iberian Range 2) Topographic lineament


Geological Set: Iberian Range (Zaragoza-Teruel)


Comment


C+*Strength Class:


Paleoearthquakes

Orden Visual: 110

Página 396 de 632




Unknown






Unknown








References

Variability



Página 397 de 632



ID: ES778 Fault Name: Piedrahita

Segment Name:

Location X: -1.02639336

Location Y: 40.99539064











Max Depth (km): 12.0 Depths assigned to the seismicity in the region typically range between 5 and 15 km, and are always less than 25 km (IGN,2010). That's consistent with the brittle layer above a basal detachment level,

Width (km): 13.9 AR

Area (km²): 124.71 AR





Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Morphostructural boundary between Iberian Range and Ebro Depression 2) Topographic lineament




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 111

Página 398 de 632




Unknown






Unknown








References

Variability



Página 399 de 632



ID: ES780 Fault Name: Gallocanta (o Valdelacasa)

Segment Name:

Location X: -1.60694947

Location Y: 41.12178653










Min Depth (km): 0.004 LD It does not outcrop at the surface. It is covered by Middle Pleistocene-Holocene alluvial fan and glacis deposits whose thickness rarely is over 4 m (Gracia and Gutiérrez, 1999).


Width (km): 13.9 AR

Area (km²): 272.88 AR


Early Pleistocene

2580-780 ka LD Gracia (1990), Gracia (1993), Gracia and Gutiérrez (1996), IGME and ENRESA (1998b)


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It offsets the Fundamental Erosion Surface of the Iberian Range 2) Topographic lineament 3) It controls Early Pleistocene alluvial fan and glacis deposits

Gracia (1993), Gracia and Gutiérrez (1996), IGME and ENRESA (1998b).



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 112

Página 400 de 632




Unknown






Unknown


Gracia, F. J. (1990): Geomorfologia de la región de Gallocanta. Tesis Doct. Univ. de Zaragoza.

Gracia, F.J. (1993): Evolución geomorfológica de la región de Gallocanta (Cordillera Ibérica Central). Geographicalia, 30, 3-17.

Gracia, F.J. and Gutiérrez, J (1996): Neotectónica y sismicidad del valle de Jiloca y sus alrededores. Xiloca, 17, 165-206.

Gracia, F.J. and Gutiérrez, J (1999): Geomorfología Kárstica de las cuencas de Gallocanta y Jiloca (provincia de Teruel). Teruel, 87 (1), 39-68.

IGN (2010). http://www.ign.es/ign/es/IGN/SisCatalogo.jsp








References

Variability





ES780

Used 28/09/1953 41.133333, -1.583333

VIII (MSK/EMS),

4.7 M

IGN spatial correlation, isoseist analysis

Gracia and Gutiérrez (1996)715

Página 401 de 632



ID: ES781 Fault Name: Caldereros

Segment Name:

Location X: -1.64013715

Location Y: 40.80683631





Average Strike(º): 308 ± 2 LD Compiler's measurement, based on Gracia and Gutiérrez (1996), following the right-hand rule.


Rake (º): -90 LD Gracia and Gutiérrez (1996)

Sense of Movement: N LD Gracia and Gutiérrez (1996)

Length (km): 13.9 ± 0.5 LD Compiler's measurement, based on Gracia and Gutiérrez (1996)

Min Depth (km): 0 LD The fault crops out at the surface (Gracia and Gutiérrez, 1996)


Width (km): 13.9 AR

Area (km²): 192.60 AR


Early Pleistocene

2580-780 ka LD Gracia and Gutiérrez (1996)


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It offsets the Fundamental Erosion Surface of the Iberian Range 2) Topographic lineament 3) It controls early Pleistocene alluvial fan and glacis deposits

Gracia and Gutiérrez (1996).

Geological Set: Iberian Range (Guadalajara)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 113

Página 402 de 632








Unknown









References

Variability



Página 403 de 632



ID: ES782 Fault Name: Sierra Menera

Segment Name:

Location X: -1.43593925

Location Y: 40.59090576





Average Strike(º): 330 ± 2 LD Compiler's measurement, based on Gracia and Gutiérrez (1996), following the right-hand rule.


Rake (º): -90 LD Gracia and Gutiérrez (1996)

Sense of Movement: N LD Gracia and Gutiérrez (1996)

Length (km): 23.8 LD Compiler's measurement, based on Gracia and Gutiérrez (1996)

Min Depth (km): 0 LD The fault crops out at the surface (Gracia and Gutiérrez, 1996)


Width (km): 13.9 AR

Area (km²): 329.78 AR


Holocene Upper Pleistocene-Holocene

LD Colluvial deposits with anomalous dips (Gracia and Gutiérrez, 1996)


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Topographic lineament 2) It affects Pleistocene-Holocene alluvial cones

Gracia and Gutiérrez (1996).

Geological Set: Iberian Range (Guadalajara-Teruel)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 114

Página 404 de 632








Unknown









References

Variability



Página 405 de 632



ID: ES783 Fault Name: Vall d'Alba

Segment Name:

Location X: -0.06812756

Location Y: 40.16251891





Average Strike(º): 035 ± 5 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), Simon (1984) and Simon et al (2013), following the right-hand rule.


Rake (º): -90 LD IGME and ENRESA (1998b), Simon (1984) and Simon et al (2013).

Sense of Movement: N LD IGME and ENRESA (1998b), Simon (1984) and Simon et al (2013).

Length (km): 26.0 ± 0.5 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), Simon (1984) and Simon et al (2013).

Min Depth (km): 0 LD The fault crops out at the surface (Simon, 1984)

Max Depth (km): 14.0 ± 1 EJ Seismic data and deep structural reconstructions indicate that these Maestrat extensional faults have a listric geometry and are detached at a mid-crustal level, some 13-15 km deep (Roca and Guimerà,

Width (km): 16.2 AR

Area (km²): 420.31 AR



2580-1800 ka LD It affects G3 (its age has been constrained by magneto-stratigraphy in 1.9-2.6 Ma (Adrover, 1986) and it is fossilized by G2-T2 attributed to Early-Middle Pleistocene (Birot, 1959; Constante, 1975; Simon, 1984 and Simon et al., 2013).


0.020 ± 0.01 EJ Inferred from 40 m of vertical fault displacement of G3 at southwestern Torre Endomenech village (based on Simon, 1984 data, p.165).




0.023 ± 0.01 AR From VSR, Dip and Rake


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It cuts G3, the oldest pediment inset in the Fundamental Erosion Surface of the Iberian Range 2) Morphological scarp offsets G3 in the Vall d'Alba-Benlloch alluvial fan 3) Fossilized by G2-T2 deposits (Early-Middle Pleistocene)

Simon (1984)

Geological Set: Iberian Range (Maestrat)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 77

Página 406 de 632




Unknown




60106 381683 - 11672 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): slip rate represents the rate at which maximum earthquakes are released by the fault. RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown


Adrover, R. (1986): Nuevas faunas de roedores en el Mio-Plioceno continental de la región de Teruel (España). Interés bioestratigráfico y paleoecológico. Inst. Estudios Turolenses, Teruel, 423 p.

Birot, P. (1959): Esquisse morphologique des Monts Celtibériques orientaux. Bull. Comité Travaux Historiques et Scientifiques, Section Géographie I 72, 101-130.

Constante, J.L. (1975): El piedemonte costero de Vinaroz-Benicarló. Boletín de la Sociedad Castellonense de Cultura 51, 224-273.



Roca, E., Guimerà, J., 1992. The Neogene structure of the eastern Iberian margin: structural constraints on the crustal evolution of the Valencia trough (western Mediterranean). Tectonophysics 203, 203-218.

Simon, J.L. (1984): Compresión y distensión alpinas en la Cadena Ibérica Oriental. Tesis Doctoral (1982). Institutos de Estudios Turolenses. 269 p.

Simon, J.L., Pérez-Cuevas, A.J., Calvo-Cases, A. (2013): Tectonic beheading of fluvial valleys in the Maestrat grabens (eastern Spain): Insights into slip rates of Pleistocene extensional faults. Tectonophysics, 593, 73-84.






References

Variability



Página 407 de 632



ID: ES784 Fault Name: Mas dels Calduchs

Segment Name:


Location Y: 40.37423912









Length (km): 6.7 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), Simon (1984) and Simon et al (2013).

Min Depth (km): 0 LD The fault crops out at the surface (Simon, 1984).


Width (km): 16.2 AR

Area (km²): 108.31 AR



2580-1800 ka LD Simon (1984)


0.030 ± 0.01 AR Inferred from 50 m of vertical fault displacement of G3 found around the Valltorta gully (based on Simon, 1984 data, p.165). Inferred slip rate is a minimum.






Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It cuts G3 (oldest pediment inset in the Fundamental Erosion Surface of the Iberian Range, F.S.E.)

Simon (1984)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 78

Página 408 de 632




Unknown






Unknown












References

Variability



Página 409 de 632



ID: ES785 Fault Name: Villafames

Segment Name:


Location Y: 40.13175236









Length (km): 10.9 0.2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), Simon (1984) and Simon et al (2013).

Min Depth (km): 0.02 ± 0.01 EJ It does not outcrop at the surface.The thickness of the Pleistocene deposits of Maestrat grabens is not more than 30-40 m (Simon, 1984).


Width (km): 16.1 AR

Area (km²): 175.96 AR



2580-1800 ka LD It reactivates after the deposit of G3 (Simon, 1984).


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Topographic lineament, 2) It offsets G3 and likely G2, 2) Apparently fossilized by G1 alluvial fan deposits.

Simon (1984)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 79

Página 410 de 632




Unknown






Unknown











References

Variability



Página 411 de 632



ID: ES786 Fault Name: Alcossebre

Segment Name:







Average Strike(º): 045 ± 2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), Simon (1984) and Simon et al. (2013), following the right-hand rule.


Rake (º): -90 LD IGME and ENRESA (1998b), Simon (1984) and Simon et al. (2013).

Sense of Movement: N LD IGME and ENRESA (1998b), Simon (1984) and Simon et al. (2013).

Length (km): 16.6 0.2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), Simon (1984) and Simon et al. (2013).

Min Depth (km): 0.02 ± 0.01 EJ It does not outcrop at the surface. The thickness of the Pleistocene deposits of Maestrat grabens is not more than 30-40 m (Simon, 1984).


Width (km): 16.1 AR

Area (km²): 267.97 AR



2580-1800 ka LD Simon (1984): It offsets G3, apparently fossilized by G2 alluvial fan deposits.


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Its Smf (Mountain-front sinuosity index, Bull and McFadden, 1997) is 2.89, high in relation to other nearby faults, suggesting that this fault has a low degree of recent activity.

Simon et al (2013)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 80

Página 412 de 632




Unknown






Unknown











References

Variability



Página 413 de 632



ID: ES787 Fault Name: Torreblanca

Segment Name:


Location Y: 40.11299145










Min Depth (km): 0.02 ± 0.01 LD It does not outcrop at the surface. The thickness of the Pleistocene deposits of Maestrat grabens is not more than 30-40 m (Simon, 1984).


Width (km): 16.1 AR

Area (km²): 484.28 AR


<253 ky LD 253 ka is a minimum date, from Simon et al (2013).


0.280 0.04-0.30 LD Simon et al (2013) constrains a vertical slip rate between a minimum 0.04-0.07 m/ky for the last 1.9 to 2.6 Ma, and a maximum of 0.26-0.30 mm/y for the last 253.3 ± 18.0 ky (G2-T2). Preferred value here is the average.






Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Most of the documented evidence is described at the northern sector: 1) Beheaded valleys 2) Anomalous morphologies evidenced by morphometric analysis 3) It offsets G2-T2 deposits

Simon et al (2013)



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 81

Página 414 de 632




Unknown






Unknown












References

Variability



Página 415 de 632



ID: ES788 Fault Name: Villanueva de Alcolea

Segment Name:


Location Y: 40.24864251












Width (km): 16.1 AR

Area (km²): 121.07 AR


Middle Pleistocene

<253 ky LD It affects G2-T2 deposits (Simon, 1984, fig.14.2), attributed to early-middle Pleistocene (Birot, 1959; Constante, 1975) and OSL dated by Simon et al (2013).


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Topographic lineament 2) It offsets G2-T2 deposits. Simon (1984)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 82

Página 416 de 632




Unknown






Unknown













References

Variability



Página 417 de 632



ID: ES789 Fault Name: Benicarló

Segment Name:


Location Y: 40.38234023









Length (km): 12.0 ± 0.2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), Simon (1984) and Simon et al. (2013).



Width (km): 16.1 AR

Area (km²): 193.57 AR



2580-1800 ka LD It affects G3 accumulation-erosion level (Simon, 1984).


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Linear scarp 2) It offsets the G3 accumulation-erosion level Simon (1984)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 83

Página 418 de 632




Unknown






Unknown











References

Variability



Página 419 de 632



ID: ES790 Fault Name: Castellón

Segment Name:

Location X: -0.35771589

Location Y: 39.95144568





Average Strike(º): 060 ± 5 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), Simon (1984) and Simon et al. (2013), following the right-hand rule.


Rake (º): -90 LD IGME and ENRESA (1998b), Simon (1984) and Simon et al, (2013).

Sense of Movement: N LD IGME and ENRESA (1998b), Simon (1984) and Simon et al. (2013).

Length (km): 46.0 ± 0.5 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a), Simon (1984) and Simon et al. (3013).



Width (km): 16.2 AR

Area (km²): 743.63 AR


Middle Pleistocene

<253 ky LD It affects G2-T2 deposits (Simon, 1984), attributed to early-middle Pleistocene (Birot, 1959; Constante, 1975) and OSL dated by Simon et al (2013).


0.593 EJ Inferred from 150 m of vertical fault displacement in G2-T2 deposits found near the mouth of the Mijares river (based on Simon, 1984 data).




0.685 ± 0.02 AR From VSR, Dip and Rake. Uncertainty is quoted from Expert Judgment.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Topographic lineament 2) It offsets G2-T2 alluvial deposits. Simon (1984)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 84

Página 420 de 632




Unknown






Unknown














References

Variability



Página 421 de 632



ID: ES791 Fault Name: Onda

Segment Name:

Location X: -0.19714564

Location Y: 39.91203931












Width (km): 16.2 AR

Area (km²): 161.66 AR


Middle Pleistocene

<253 ky LD It affects G2-T2 deposits (Simon, 1984), attributed to early-middle Pleistocene (Birot, 1959; Constante, 1975) and OSL dated by Simon et al (2013).


0.400 EJ Inferred from 100 m of vertical fault displacement in G2-T2 deposits (Simon, 1984).






Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Topographic lineament 2) It offsets G2-T2 alluvial deposits Simon (1984)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 85

Página 422 de 632




Unknown






Unknown














References

Variability



Página 423 de 632



ID: ES792 Fault Name: Peñaescabia

Segment Name:

Location X: -0.78903142






Average Strike(º): 045 ± 5 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Simon (1984).


Rake (º): -90 LD IGME and ENRESA (1998b) and Simon (1984).

Sense of Movement: N LD IGME and ENRESA (1998b) and Simon (1984).

Length (km): 21.0 ± 0.2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Simon (1984).

Min Depth (km): 0.04 ± 0.2 LD Simon (1984).

Max Depth (km): 12.0 ± 2 EJ It corresponds to the basal detachment level, 10-15 km depth, identified by Roca and Guimerá (1992).

Width (km): 13.8 AR

Area (km²): 290.01 AR


Early Pleistocene

2580-780 ka LD Simon (1984), pp. 195.


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Fault scarp 2) It offsets G3 deposits. Simon (1984)

Geological Set: Iberian Range (Castellón)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 86

Página 424 de 632








Unknown










References

Variability



Página 425 de 632



ID: ES793 Fault Name: Caudiel

Segment Name:

Location X: -0.61299533

Location Y: 39.94513919





Average Strike(º): 040 ± 5 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Simon (1984).

Dip (º): 60 ± 20 LD Typical dip of normal faults.

Rake (º): -90 LD IGME and ENRESA (1998b) and Simon (1984).

Sense of Movement: N LD IGME and ENRESA (1998b) and Simon (1984).

Length (km): 10.5 ± 0.2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Simon (1984).

Min Depth (km): 0.4 ± 0.2 LD Simon (1984).


Width (km): 13.4 AR

Area (km²): 140.64 AR


Early Pleistocene

2580-780 ka LD Simon (1984), pp. 195.


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Fault scarp 2) It offsets G3 deposits Simon (1984)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 87

Página 426 de 632








Unknown










References

Variability



Página 427 de 632



ID: ES794 Fault Name: San Vicente

Segment Name:

Location X: -0.45905395

Location Y: 40.14650465





Average Strike(º): 240 ± 2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Simón (1984).

Dip (º): 60 ± 20 EJ Typical dip of normal fault

Rake (º): -90 LD IGME and ENRESA (1998b) and Simón (1984).

Sense of Movement: N LD IGME and ENRESA (1998b) and Simón (1984).

Length (km): 6.6 ± 0.02 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Simón (1984).

Min Depth (km): 0 LD Observed on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Simón (1984).


Width (km): 13.9 AR



Early Pleistocene

2580-780 ka LD Simon (1984)


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Fault scarp 2) It offsets detritic alluvial deposits which can be correlated to G3 glacis deposits.

Simon (1984)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 88

Página 428 de 632








Unknown










References

Variability



Página 429 de 632




Segment Name: Els Ivarsos sur

Location X: -0.06481412

Location Y: 40.17335387





Average Strike(º): 212 - 20 / + 2 LD Compiler's measurement, based on Simon (1984) and Simon et al. (2013).


Rake (º): -90 LD Simon (1984) and Simon et al. (2013).

Sense of Movement: N LD Simon (1984) and Simon et al. (2013).

Length (km): 9.0 ± 0.2 EJ Compiler's measurement, based on Simon (1984) and Simon et al. (2013).

Min Depth (km): 0 LD Simon (1984) and Simon et al. (2013).


Width (km): 13.9 AR

Area (km²): 124.71 AR


Early Pleistocene

2580-780 ka LD Simon (1984) and Pérez and Simón (1989)


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Marked fluvial anomaly at Els Estrests de Rodamonte, where the Rambla de la Viuda gully captures the Pla de Vilafamés endorheic area.

Simon (1984) and Pérez and Simón (1989)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 75

Página 430 de 632








Unknown


Pérez, A.J., and Simón, J.L. (1989): Cambios en el trazado de la red fluvial producidos por la tectónica cuaternaria en el sistema de fosas del Maestrat. Actas II Reunión del Cuaternario Ibérico, El Cuaternario de España y Portugal, vol. 2, 707-715. ITGE-Asociación Española para el Estudio del Cuaternario, Madrid (publ. 1993).








References

Variability



Página 431 de 632



ID: ES796 Fault Name: Les Useres

Segment Name:

Location X: -0.17656786

Location Y: 40.15839174





Average Strike(º): 050 ± 2 LD Compiler's measurement, based on Simón (1984) and Simón et al. (2013).


Rake (º): -90 LD Simón (1984) and Simón et al. (2013).

Sense of Movement: N LD Simón (1984) and Simón et al. (2013).

Length (km): 7.0 ± 0.5 LD Compiler's measurement, based on Simón (1984) and Simón et al. (2013).

Min Depth (km): 0 LD Simón (1984) and Simón et al. (2013).


Width (km): 13.9 AR



Early Pleistocene

2580-780 ka Simón (1984)


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Fault scarp 2) It offsets G3 deposits Simón (1984)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 89

Página 432 de 632








Unknown









References

Variability



Página 433 de 632



ID: ES797 Fault Name: Andarax Valley and El Alquián Fault System

Segment Name:

Location X: -2.50098402

Location Y: 37.06361025





Average Strike(º): 133 ± 12 LD Compiler's measurement, based on Pedrera et al. (2012). To apply right hand rule criteria dip is considered towards W. The downthrown block is frequently the western one (Sanz de Galdeano et al., 2010).


Rake (º): -90 LD Pedrera et al. (2012). In some cases, near the locality of Tabernas, these NW-SE faults present oblique displacements and even pure horizontal dextral movements (Sanz de Galdeano et al., 2010).

Sense of Movement: N LD Pedrera et al. (2012). In some cases, near the locality of Tabernas, these NW-SE faults present oblique displacements and even pure horizontal dextral movements (Sanz de Galdeano et al., 2010).

Length (km): 36.0 ± 2 LD Compiler's measurement, based on Pedrera et al. (2012). This system is formed by a set of faults with lengths between 2 and 8 km (Cuevas de los Úbeda Fault). The fault zone shows a width from 5 to 10 km.

Min Depth (km): 0 LD Pedrera et al. (2012); Sanz de Galdeano et al. (2010); Marín-Lechado et al. (2005).

Max Depth (km): 8.0 ± 2 LD Given value is the depth of the fragile crust in the area. García-Mayordomo (2005), table 4.20.

Width (km): 9.2 AR

Area (km²): 332.55 AR


Holocene LD This system presents a very clear active geomorphologic imprint. The epicentres of the Gergal 2002 seismic series aligned with the general trend of the fault system, suggesting the current activity of these faults (Sanz de Galdeano et al., 2010).


0.500 LD Uplift rates at the southern mountain front are higher than 0.5 m/ky in the Quaternary (Giaconia et al., 2012).


0 AR HSR=0, assumed pure dip-slip faulting.




Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) The system show young echeloned scarps SW of Sierra Alhamilla 2) Pliocene-Quaternary sediments are faulted 3) From Gergal to Cabo de Gata, the fault system controls the Andarax valley geometry and the rectilinear coast line 4) Wedge infill 5)

Earthquakes related to the Cuevas de los Úbeda Fault (Marín-Lechado et al., 2005); Martínez-Díaz and Hernández-Enrile (2004); Pedrera et al. (2006); Sanz de Galdeano et al. (2010); Pedrera et al. (2012)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 196

Página 434 de 632




Unknown


Unknown






Unknown


Cesca, S., 2005. Inversión del tensor momento sísmico de terremotos superficiales a distancias regionales. Thesis. Univ. Complutense. Madrid, 289 pp., Unpublished.

D Amico,V., D. Albarello, and Mantovanil, E. (1999): A distribution free analysis of magnitud-intensity relationships: an application to the Mediterranean region. Phys. Chem. Earth 24,517-521.


Giaconia, F., Booth-Rea, G., Martínez-Martínez, J. M., Azañón, J. V. Pérez-Peña., M. Pérez-Romero J., Villegas, I. (2012): Geomorphicevidence of active tectonics in the Sierra Alhamilla (eastern Betics, SE Spain). Geomorphology 145-146, 90–106. doi:10.1016/j.geomorph.2011.12.043.

Marín-Lechado, C., Galindo-Zaldívar, J., Rodríguez-Fernández, L.R., Serrano, I., and Pedrera, A. (2005): Active faults, seismicity and stresses in an internal boundary of a tectonic arc (Campo de Dalías and Níjar, southeastern Betic Cordilleras, Spain). Tectonophysics, 396, 81– 96.

Martínez-Díaz, J.J., Hernández-Enrile, J.L. (2004): Neotectonics and morphotectonics of the southern Almería region (Betic Cordillera–Spain) kinematic implications. Int. J. Earth Sci. 93, 189–206. doi:10.1007/s00531-003-0379-y.

Pedrera, A., Marín-Lechado, C., Galindo-Zaldívar, J., Rodríguez-Fernández, L.R., Ruiz-Constán, A. (2006): Fault and fold interactionduring the development of the Neogene-Quaternary Almería-Níjar basin (SE Betic Cordilleras). In: Moratti, G., Chalouan, A. (eds). Tectonics of the Western Mediterranean and North Africa. Geological Society, London, Special Publications, 262, 217–230.

Pedrera, A., Galindo-Zaldívar, J., Marín-Lechado, C., García-Tortosa, F.J., Ruano, P., López Garrido, A.C., Azañón, J.M., Peláez, J.A., and Giaconia, F. (2012): Recent and active faults and folds in the central-eastern Internal Zones of the Betic Cordillera. Journal of Iberian




References

Variability





ES797

Gergal 04/02/2002 -2.53, 37.09 V (EMS-98 scale)/Mw 4.6

IGN Spatial correlation It had more than 30 aftershocks during a month. Cesca (2005) indicated a Mw= 4.6 and has proposed two possible focal mechanisms for the main shock; Sanz de Galdeano et al. (2010) related the seismic series with this fault system.

716

ES797

Nacimiento 11/06/1894 -2.67, 37.12 VII (EMS-98 scale), Ms 4.7

IGN spatial correlation Ms 4.7 from maximum intensity, using the D'Amico et al (1999) relationship (Pedrera et al, 2012)

717

Página 435 de 632



Geology, 38 (1), 191-208.

Sanz de Galdeano, C., Shanovb, S., Galindo-Zaldívara, J., Radulovb, A., and Nikolovb. G. (2010): A new tectonic discontinuity in the Betic Cordillera deduced from active tectonics and seismicity in the Tabernas Basin. Journal of Geodynamics, 50, 57–66.



Página 436 de 632



ID: ES798 Fault Name: Eastern Gador Range Fault System

Segment Name:

Location X: -2.72645367

Location Y: 36.93369947





Average Strike(º): 125 120 to 130 LD Compiler's measurement, based on Pedrera et al. (2012). To apply right hand rule criteria dip is considered towards W. The downthrown block is frequently the western one.


Rake (º): -90 LD Pedrera et al. (2012)

Sense of Movement: N LD Pedrera et al. (2012)

Length (km): 20.0 ± 2 LD Compiler's measurement, based on Pedrera et al. (2012). This system formed by a set of faults with lengths between 2 and 8 km. The fault zone shows a width from 1 to 6 km.

Min Depth (km): 0 LD Pedrera et al. (2012).

Max Depth (km): 8.0 ± 2 LD Given value is the depth of the fragile crust in the area. García-Mayordomo (2005), table 4.20.

Width (km): 9.2 AR

Area (km²): 184.75 AR


Holocene LD This system presents the clearest active geomorphologic (Pedrera et al., 2012 and Marín-Lechado, 2010)


0.500 0.3 to 0.7 LD Based on the regional uplift over the last 245,000 years (Marín-Lechado et al., 2010).


0 AR HSR=0, assumed pure dip-slip faulting.


0.577 0.346 to 0.808 AR From VSR, Dip and Rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) They present young echeloned scarps 2) Drainage network anomalies

Pedrera et al. (2012) and Marín-Lechado et al. (2010)



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 197

Página 437 de 632








Unknown



Marín-Lechado, C., Galindo-Zaldívar, J., Gil, A.J., Borque, M.J., de Lacy, M.C., Pedrera, A., López-Garrido, A.C., Alfaro, P., García-Tortosa, F., Ramos, M.I., Rodríguez-Caderot, G., Rodríguez-Fernández, J., Ruiz-Constán, A., and Sanz de Galdeano-Equiza, C. (2010): Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain). Sensors, 10, 3504-3518; doi:10.3390/s100403504.

Pedrera, A., Galindo-Zaldívar, J., Marín-Lechado, C., García-Tortosa, F.J., Ruano, P., López Garrido, A.C., Azañón, J.M., Peláez, J.A., and Giaconia, F. (2012): Recent and active faults and folds in the central-eastern Internal Zones of the Betic Cordillera. Journal of Iberian Geology, 38 (1), 191-208.






References

Variability



Página 438 de 632



ID: ES799 Fault Name: Balanegra

Segment Name:

Location X: -2.90420183

Location Y: 36.76633002





Average Strike(º): 150 ± 5 EJ Compiler's measurement, Marín-Lechado et al. (2010). To apply right hand rule criteria dip is considered towards W.


Rake (º): -135 LD Martínez-Díaz and Hernádez-Enrile (2004); Marín-Lechado et al. (2005); Marín-Lechado et al. (2010)

Sense of Movement: DN LD Martínez-Díaz and Hernádez-Enrile (2004); Marín-Lechado et al. (2005); Marín-Lechado et al. (2010)

Length (km): 9.0 EJ Compiler's measurement, based on Marín-Lechado et al. (2010). The Balanegra Fault Zone comprises two main parallel faults along with other minor synthetic faults, producing a staircase morphology.

Min Depth (km): 0 LD Martínez-Díaz and Hernádez-Enrile (2004); Marín-Lechado et al. (2005); Marín-Lechado et al. (2010)

Max Depth (km): 8.0 ± 2 EJ According to Marín-Lechado et al. (2005), the normal faulting with local strike-slip regimes occur within the upper crust. So, the given maximum value is the depth of the fragile crust (García-Mayordomo,

Width (km): 9.2 AR



Holocene LD Shallow instrumental seismicity shows NW–SE oriented lineations of epicentres that align with the fault zone (Martínez-Díaz and Hernádez-Enrile, 2004; Marín-Lechado et al., 2005)


0.065 0.05-0.08 LD The vertical relative slip rates that result from the present topographic height of Quaternary marine terraces. It was calculated from Late Pleistocene (Martínez-Díaz and Hernádez-Enrile, 2004).


0.075 0.058-0.092 AR From NSR and Rake


0.106 0.082-0.131 AR From VSR, Dip and Rake


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Rectilinear scarps with staircase morphology that influence the drainage network 2) Holocene asymmetric clastic wedges 3) They cut Holocene sediments 4) Seismites in Quaternary sediments 5) They control the coastline of the Campo de Dalías

Martínez-Díaz and Hernádez-Enrile (2004); Marín-Lechado et al. (2005); Marín-Lechado et al. (2010); Pedrera et al. (2012)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 198

Página 439 de 632




Unknown


6.36 ± 0.37 ER Magnitude from length using Stirling et al. (2002) equation derived from the instrumental dataset. Marín-Lechado et al. (2005) estimates a Mw of 5.5 using Wells and Coppersmith (1994) and a fault length of 8 km.




Unknown



Variability





ES799

Adra Series December 1994 to January

1995

near Adra VII (MSK), Mb=4.9 and

Mb=5.0 mainshocks

Andalusian Seismic Network

(RSA)

Spatial correlation, aftershocks distribution

The spatial distribution of the series and the most recent seismic activity (792 events) defines an approximately NNW-SSE elongated region limited to the North and South by the two mainshocks (Marín-Lechado et al., 2005, 2010)

718

ES799

South Adra 22/09/1522 -2.866; 36.433

IX (MSK) Martínez-Díaz (2000)

Spatial correlation Marín-Lechado et al. (2010)719

ES799

Adra 21/01/1804 -3.000; 36.701

VIII (MSK) Martínez-Díaz (2000)


ES799

Southwest Adra 25/08/1804 -4.183, 40.645

IX (MSK) Martínez-Díaz (2000)


ES799

Adra 16/06/1910 -3.367; 36.667

VII (MSK) Martínez-Díaz (2000)


ES799

Adra 16/06/1910 -3.367; 36.667

VIII (MSK) Martínez-Díaz (2000)


Página 440 de 632





Marıín-Lechado, C., Galindo-Zaldívar, J., Rodrıíguez-Fernández, L.R., Serrano, I., Pedrera, A. (2005): Active faults, seismicity and stresses in an internal boundary of a tectonic arc (Campo de Dalías and Níjar, southeastern Betic Cordilleras, Spain). Tectonophysics, 396, 81– 96.

Marín-Lechado, C., Galindo-Zaldívar, J., Gil, A.J., Borque, M.J., de Lacy, M.C., Pedrera, A., López-Garrido, A.C., Alfaro, P., García-Tortosa, F., Ramos, M.I., Rodríguez-Caderot, G., Rodríguez-Fernández, J., Ruiz-Constán, A., and Sanz de Galdeano-Equiza, C. (2010): Levelling Profiles and a GPS Network to Monitor the Active Folding and Faulting Deformation in the Campo de Dalias (Betic Cordillera, Southeastern Spain). Sensors, 10, 3504-3518; doi:10.3390/s100403504.

Martínez-Díaz, J.J. (2000): Análisis sismotectónico de la serie sísmica de Adra: mecanismos de terremotos compuestos como respuesta a la interacción entre fallas activas en el sureste de la Cordillera Bética. Rev. Soc. Geol. Esp. 2000, 13, 31-43.

Martínez-Díaz, J.J, and Hernández-Henrile, J.L. (2004): Neotectonics and morphotectonics of the southern Almería region (Betic Cordillera-Spain) kinematic implications. Int J Earth Sci (Geol Rundsch), 93, 189–206. DOI 10.1007/s00531-003-0379-y

Pedrera, A., Galindo-Zaldívar, J., Marín-Lechado, C., García-Tortosa, F.J., Ruano, P., López Garrido, A.C., Azañón, J.M., Peláez, J.A., and Giaconia, F. (2012): Recent and active faults and folds in the central-eastern Internal Zones of the Betic Cordillera. Journal of Iberian Geology 38 (1), 191-208.





References

Página 441 de 632



ID: ES800 Fault Name: Loma del Viento

Segment Name:

Location X: -2.63813655

Location Y: 36.71772615





Average Strike(º): 300 ± 15 LD To apply right hand rule criteria dip is considered towards NNE. Segmented fault comprising six onshore hard-linked and soft-linked segments with an average strike varying between N105°E and N135°E (Marín-Lechado et al. 2004; Pedrera et al., 2012a,b).

Dip (º): 80 70 to 90 LD The average dip is 80° toward the NNE, though some sub-segments are vertical and others dip 80° toward the SSW (Marín-Lechado et al. 2004; Pedrera et al., 2012a).

Rake (º): -135 LD Marín-Lechado et al. (2004); Pedrera et al. (2012a); Pedrera et al. (2012b).

Sense of Movement: DN LD Marín-Lechado et al. (2004); Pedrera et al. (2012a); Pedrera et al. (2012b).

Length (km): 8.0 ± 0.2 LD Pedrera et al. (2012a).

Min Depth (km): 0 LD Pedrera et al. (2012a).

Max Depth (km): 8.0 ± 2 LD According to Marín-Lechado et al. (2005), the normal faulting with local strike-slip regimes occur within the upper crust. So, the given maximum value is the depth of the fragile crust (García-Mayordomo,

Width (km): 8.1 AR



Holocene LD Association to current instrumental seismicity is very likely (Pedrera et al., 2012a).


0.049 ± 0.021 AR From NSR, dip and rake


0.049 ± 0.021 AR From NSR and rake


0.07 ± 0.03 LD Pedrera et al. (2012a) evaluates the min/max age of the affected formation (~3.6 to ~1.8 Ma) and calculates a min/max fault offset (90 to 100 m). They thus arrived at a long-term slip rate of 0.07±0.03 mm/y.


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Fault scarp 2) Associated deposit with wedge geometry 3) The marine terraces show a staircase layout and are characterized by vertical aggradation on the hanging-wall, revealing Pleistocene fault activity

Marín-Lechado et al. (2004); Pedrera et al. (2012a)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 199

Página 442 de 632




Unknown


Unknown






Unknown



Marín-Lechado, C., Galindo-Zaldívar, J., Rodríguez-Fernández, L.R., González-Lodeiro, F. (2004): Faulted hybrid joints: an example from the Campo de Dalías (Betic Cordilleras, Spain). Journal of Structural Geology 26, 2025–2037.

Marıín-Lechado, C., Galindo-Zaldívar, J., Rodrıíguez-Fernández, L.R., Serrano, I., Pedrera, A. (2005): Active faults, seismicity and stresses in an internal boundary of a tectonic arc (Campo de Dalías and Níjar, southeastern Betic Cordilleras, Spain). Tectonophysics, 396, 81– 96.

Pedrera, A., Marín-Lechado, C., Stich, D., Ruiz-Constán, A., Galindo-Zaldívar, J., Rey-Moral, C., and Mancilla, F.L. (2012a): Nucleation, linkage and active propagation of a segmented Quaternary normal-dextral fault: the Loma del Viento fault (Campo de Dalías, Eastern Betic Cordillera, SE Spain). Tectonophysics, 522–523 (2012), 208–217.

Pedrera, A., Galindo-Zaldívar, J., Marín-Lechado, C., García-Tortosa, F.J., Ruano, P., López Garrido, A.C., Azañón, J.M., Peláez, J.A., and Giaconia, F. (2012b): Recent and active faults and folds in the central-eastern Internal Zones of the Betic Cordillera. Journal of Iberian Geology 38 (1), 191-208.






References

Variability





ES800

Offshore Loma del Viento fault

November 2010

-2.591; 36.713

Mw 3.5 to 4.2 IGN Spatial correlation Correlation is probable. Moment tensor analysis revealed a strike-slip fault with a rightlateral, slightly oblique focal plane striking ~N125°E and hypocenter depths of 12 km (Pedrera et al., 2012a)

724

Página 443 de 632



ID: ES801 Fault Name: Almanzora Corridor Fault Zone

Segment Name:

Location X: -2.43803077

Location Y: 37.40771162





Average Strike(º): 080 75 to 130 EJ Compiler's measurement, Pedrera et al. (2012). To apply right hand rule criteria dip is considered towards W. The western fault zone shows a WNW-ESE to NW-SE variable strike. The central and eastern zones show ENE-WSW strike.

Dip (º): 70 30 to 90 EJ From the high dips of strike-slip faults to the low dips of reverse faults (Pedrera et al., 2012).

Rake (º): -180 90 to -90 LD At the western fault zone, the faults are normal, and at the central and eastern part, the fault zone shows WNW-ESE trending dextral faults and ENE-WSW oriented open folds, fault-propagation folds, and reverse faults (Pedrera et al., 2012).

Sense of Movement: D N to R LD At the western fault zone, the faults are normal, and at the central and eastern part, the fault zone shows WNW-ESE trending dextral faults and ENE-WSW oriented open folds, fault-propagation folds, and reverse faults (Pedrera et al., 2012).

Length (km): 23.0 ± 2 EJ Compiler's measurement, Pedrera et al. (2012).

Min Depth (km): 0 LD Pedrera et al. (2012).

Max Depth (km): 11.0 9-11 LD According to Marín-Lechado et al. (2005), the normal faulting with local strike-slip regimes occur within the upper crust. Given maximum value is the depth of the fragile crust in the area (García-Mayordomo,

Width (km): 11.7 AR

Area (km²): 269.24 AR


Holocene LD Pedrera et al. (2012)


0.014 LD Calculated for the fault-propagation folds of the Molata from mid-Pleistocene to Present (Pedrera et al., 2009).


0.007 LD Calculated for the fault-propagation folds of the Molata from the mid-Pleistocene to Present (Pedrera et al., 2009).


0.015 ± 0.01 EJ From the Molata's VSR and HSR estimations above. Uncertainty is from Expert Judgment.


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Western fault zone (normal faults) deforms Quaternary sediments and shows a steep scarp. 2) The folds and related faults show a syn-tectonic geometry of the growth strata. 3) The fault zone controls the drainage network of the Almanzora River

Pedrera et al. (2012)



Comment


A+*Strength Class:


Orden Visual: 200

Página 444 de 632




Unknown


Unknown






Unknown



Pedrera, A., Galindo-Zaldívar, J., Ruiz-Bustos, A., Rodríguez-Fernández, J., Ruíz- Constán, A. (2009): The role of small-scale fold andfault development in seismogenic zones: example of the Western Huércal-Overa basin (Eastern Betic Cordillera, Spain). J. Quat. Sci. 24, 581–592, doi:10.1002/jqs.1246

Pedrera, A., Galindo-Zaldívar, J., Marín-Lechado, C., García-Tortosa, F.J., Ruano, P., López Garrido, A.C., Azañón, J.M., Peláez, J.A., and Giaconia, F. (2012): Recent and active faults and folds in the central-eastern Internal Zones of the Betic Cordillera. Journal of Iberian Geology 38 (1), 191-208.

Silva, P., Rodríguez-Pascua, M.A., Giner-Robles, J.L., Roquero, E., Pérez-López, R., Huerta, P., and Bardají, T. (2014). Anatomy of an earthquake: geological anlalysis of the Huércal-Overa AD 1863 event (Almería, SE Spain). Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, Esapña, 151-154.






References

Variability



Paleoearthquakes



ES801

Huércal-Overa AD 1863

10th June 1863 AD

VIII (ESI-07 scale)

Silva et al. (2014)

Aftershocks distribution Silva et al. (2014)725

Página 445 de 632



ID: ES802 Fault Name: Torre Carbonero-Marilópez

Segment Name:

Location X: -6.515

Location Y: 36.94181774





Average Strike(º): 075 ± 2 LD Compiler's measurement, based on Rodríguez-Ramírez et al. (2014). To apply right hand rule criteria dip is considered towards W.


Rake (º): -90 LD Rodríguez-Ramírez et al. (2014).

Sense of Movement: N LD Rodríguez-Ramírez et al. (2014).

Length (km): 13.0 ± 0.5 EJ Compiler's measurement, based on Rodríguez-Ramírez et al. (2014).

Min Depth (km): 0.3 > 0.3 EJ According to Rodríguez-Ramírez et al. (2014), this fault does not outcrop at the surface but it controls the estuarine infilling and its geomorphological configuration during the Holocene, and should

Max Depth (km): 4.0 ± 0.5 EJ This fault can be related to the Pliocene-Quaternary listric faults rooted in the Allochthonous Complex of the Guadalquivir, like other faults of the Gulf of Cadiz (Vazquez et al.,2010).The base of the

Width (km): 4.3 AR



c. 2000 cal yr BP

LD Rodríguez-Ramírez et al. (2014).


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Geomorphological anomalies: anomalous drainage, subdued morphologies, erosive forms, patches of vegetation caused by weaknesses and changes of humidity in the ground. 2) Stratigraphical evidences

Rodríguez-Ramírez et al. (2014). Other plausible non-tectonic causes for these anomalies are not discussed in the paper.

Geological Set: Guadalquivir Basin (Huelva)


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 254

Página 446 de 632








Unknown


Medialdea, T. (2007): Estructura y evolución tectónica del Golfo de Cádiz. Instituto Geológico y Minero de España. Serie: Tesis Doctorales Nº8. 328 pp.

Rodríguez-Ramírez, A., Flores-Hurtado, E., Contreras, C., Villarías-Robles, J.J.R., Jiménez-Moreno, G., Pérez-Asensio, J.N., López-Sáez, J.A., Celestino-Pérez, S., Cerrillo-Cuenca, E., and León A. (2014): The role of neo-tectonics in the sedimentary infilling and geomorphological evolution of the Guadalquivir estuary (Gulf of Cadiz, SW Spain) during Holocene. Geomorphology, 219, 126-140.


Vázquez, J.T.,Fernández-Puga, M.C., Medialdea, T., Díaz del Río, V., Fernández-Salas, L.M., Llave, E., Lobo, F.J., Lopes, F.C., Maldonado, A., Somoza, L. and Palomino, D. (2010): Fracturación normal durante el Cuaternario Superior en la Plataforma Continental Septentrional del Golfo de Cádiz (SO de Iberia). Resúmenes de la 1ª Reunión Ibérica sobre Tectónica Activa y Paleosismología, Sigüenza, España (2010).





References

Variability



Página 447 de 632



ID: ES803 Fault Name: Torre Marilópez

Segment Name:

Location X: -6.37028018

Location Y: 37.04112315









Length (km): 8.0 ± 0.5 LD Compiler's measurement, based on Rodríguez-Ramírez et al. (2014).



Width (km): 4.3 AR



c. 2000 cal yr BP



Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Geomorphological anomalies: peculiar drainages, subdued morphologies, erosive forms, patches of vegetation caused by weaknesses and changes of humidity in the ground. 2) Stratigraphical evidences


Geological Set: Guadalquivir Basin (Sevilla)


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 255

Página 448 de 632








Unknown









References

Variability



Página 449 de 632



ID: ES804 Fault Name: Madre de las Marismas

Segment Name:

Location X: -6.40217364

Location Y: 36.96101858









Length (km): 8.0 ± 0.5 LD Compiler's measurement, based on Rodríguez-Ramírez et al. (2014).



Width (km): 4.3 AR



c. 2000 cal yr BP



Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Geomorphological anomalies: peculiar drainages, subdued morphologies, erosive forms, patches of vegetation caused by weaknesses and changes of humidity in the ground. 2) Stratigraphical evidences


Geological Set: Guadalquivir Basin (Huelva)


Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 256

Página 450 de 632








Unknown









References

Variability



Página 451 de 632



ID: ES806 Fault Name: Barbate Fault System

Segment Name:

Location X: -5.90005342

Location Y: 36.15822848





Average Strike(º): 300 ± 10 LD Compiler's measurement, based on Zazo et al. (2008). The system shows a N-S fault. To apply right hand rule criteria dip is considered towards N (dip sense of the most faults)

Dip (º): 90 to 60 EJ Typical dip of strike-slip faults. The N-S fault shows a 60º dip, typical dip of a normal fault (Zazo et al., 2008)

Rake (º): -180 to -90 LD Zazo et al. (2008).

Sense of Movement: D to N LD Zazo et al. (2008).

Length (km): 12.5 ± 0.5 LD Compiler's measurement, based on Zazo et al. (2008).

Min Depth (km): 0 LD Zazo et al. (2008).


Width (km): 4.0 AR



Holocene LD Zazo et al. (2008).


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It controls the deposits of the alluvial fans and the drainage network 2) it controls the present topographic elevations of the OIS 5c marine sediments and the morphology of the inner continental shelf.

Zazo et al. (2008)

Geological Set: Guadalquivir Basin (Cádiz)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 258

Página 452 de 632








Unknown





Zazo, C.; Mercier, N.; Lario, J.; Roquero, E.; Goy, J.L.; Silva, P.G.; Cabero, A.; Borja, F.; Dabrio, C.J.; Bardaji, T.; Soler, V.; Garcia-Blazquez, A.; Luque, L. (2008). Palaeoenvironmental evolution of the Barbate-Trafalgar coast (Cadiz) during the last 140 ka: tectonics, climate and sea-level interactions. Geomorphology, 100 (1-2): 212-222.




References

Variability



Página 453 de 632



ID: ES808 Fault Name: Teruel

Segment Name:

Location X: -1.10450951

Location Y: 40.35397889





Average Strike(º): 170 ± 20 LD Compiler's measurement, based on Lafuente et al. (2011) and Ezquerro et al. (2012).

Dip (º): 60 to 80 LD Lafuente et al. (2011).

Rake (º): -90 LD Lafuente et al. (2011) and Ezquerro et al. (2012).

Sense of Movement: N LD Lafuente et al. (2011) and Ezquerro et al. (2012).

Length (km): 6.0 ± 0.3 LD Compiler's measurement, based on Lafuente et al. (2011) and Ezquerro et al. (2012).

Min Depth (km): 0 LD Lafuente et al. (2011) and Ezquerro et al. (2012).


Width (km): 13.9 AR



Upper Pleistocene

LD Ezquerro et al. (2012).


0.057 0.053 to 0.061 AR Calculated according to the vertical slip values given by Lafuente et al. (2011).




0.061 0.057 to 0.065 AR Calculated according to the net slip values given by Lafuente et al. (2011).


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) It offsets Quaternary deposits 2) fault scarp Lafuente et al. (2011) and Ezquerro et al. (2012)



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 108

Página 454 de 632








Unknown


Ezquerro, L., Lafuente, P., Pesquero, Mª. D., Alcalá, L., Arlegui, L.E., Liesa, C.L., Luque, L., Rodríguez-Pascua, M.A., Simón, J.L. (2012). Una cubeta endorreica residual plio-pleistocena en la zona de relevo entre las fallas de Concud y Teruel: implicaciones paleogeográficas. Revista de la Sociedad Geológica de España, 25, 157-173.

IGN (2010). http://www.ign.es/ign/es/IGN/SisCatalogo.jsp

Lafuente, P., Arlegui, L.E., Casado, I., Ezquerro, L., Liesa, C.L., Pueyo, Ó., Simón, J.L. (2011). Geometría y cinemática de la zona de relevo entre las fallas neógeno-cuaternarias de Concud y Teruel (Cordillera Ibérica). Revista de la Sociedad Geológica de España, 24, 109-125.







References

Variability



Página 455 de 632



ID: ES809 Fault Name: Rius Cabanes

Segment Name: Rius Colomers


Location Y: 42.62284339

Name of Compiler(s): Ortuño, M.

Filiation: Universitat de Barcelona



Average Strike(º): 304 ± 5 OD Geomorphological mapping in Ortuño (2008)

Dip (º): 85 ± 5 OD According to the rectilinear trace

Rake (º): -90 OD Normal fault according to the displacement of glacial surfaces. It could have some minor lateral component


Length (km): 3.1 ± 0.01 OD Two parts are distinguished, the NW part (2,48 km) and the SE part (0,78 km). Total length of the system is given according to a rectilinear distance from origin.

Min Depth (km): 0 OD Inferred from the surface displacement

Max Depth (km): 12.0 LD Maximum value (12 km) comes from the seismogenic depth inferred to the area by Souriau and Pauchet (1998) by analyzing the instrumental seismicity.

Width (km): 12.0 AR



Upper Pleistocene

EJ The action of the glaciers during the LGM has modified the glacial surfaces and the scarp. The glacial landform displaced should have been originated during the glaciation previous to the LGM and not before, as inferred from its good preservation.


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Displacement of glacial surfaces that form the glacial cirques of the Aiguastortes National Park (Colomers cirque).

The glacial retro-excavation has probably enhanced the apparent vertical displacement, which averages 40 m. Analysis of the along-trace variation of the slip show that fault displacement increases towards the centre of the trace (Ortuño, 2008).


Identification Method: Geomorphological field mapping and analysis of microseismicity

Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 18

Página 456 de 632




EJ Part of the offset seems to be apparent and results from the glacial overdeepening. Part of the offset could be active faulting related to glacial elastic rebound of the uppermost crust (Ortuño, 2008).






1373 LD This fault system could have caused the historical Ribagorça earthquake (Ortuño, 2008).


Olivera, C. y Fleta, J., 1996. Analysis of Microearthquakes (1986-1993) in Vielha Area, Axial Zone of the Central Pyrenees.European Seismological Commision, XXV General Assembley, Reykjavik, Iceland. 288-293.


Souriau, A. y Pauchet, H., 1998. A new synthesis of Pyrenean seismicity and its tectonic implications. Tectonophysics, 290, 221-244.





References

Variability





ES809


3th March 1373

42º38’ N, 0º41’E


Olivera et al., (2006)

The faults are within the epicentral area

Historic earthquake (Olivera et al., 2006) that might be produced by this fault (Ortuño, 2008)

702

ES809

Microseismicity 1977-2005 Maladeta massif

M = 2-4 Institut Cartogràfic

de Catalunya

(ICC)

epicentre and hipocentre spatial

distribution

Microseismicity in the area is relatively intense in the period 1986-1993 (Olivera and Fleta, 1996) and 1986-1996 (Souriau and Pauchet, 1998).. Epicentres of 3>M>4 earthquakes are aligned with the system for the period 1977-2005 (Ortuño, 2008).

703

Página 457 de 632



ID: ES810 Fault Name: Rius-Cabanes

Segment Name: Rius-Cabidornats


Location Y: 42.63720463









Length (km): 8.3 ± 0.01 OD Three parts are distinguished, the NW (3,64 km), the central (1,24) and the SE part (3,45 km). Total length of the system is given according to a rectilinear distance from origin.



Width (km): 12.0 AR



Upper Pleistocene



Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 19

Página 458 de 632










1373 EJ This fault system could have caused the historical Ribagorça earthquake (Ortuño, 2008).


Olivera, C. y Fleta, J., 1996. Analysis of Microearthquakes (1986-1993) in Vielha Area, Axial Zone of the Central Pyrenees. European Seismological Commision, XXV General Assembley, Reykjavik, Iceland. 288-293.







References

Variability





ES810


3th-March-1373

42º38’ N, 0º41’E





704

ES810

Microseismicity 1986-2005 maladeta Massif

M = 2-4 Institut Cartogràfic

de Catalunya

(ICC)


distribution


706

Página 459 de 632



ID: ES811 Fault Name: Rius-Cabanes

Segment Name: Gerber-Cabanes


Location Y: 42.62243479









Length (km): 5.7 ± 0.01 OD Two segments are distinguished, the NW segment (1,75 km) and the SE segment (4 km). Total length of the system is given according to a rectilinear distance from origin.



Width (km): 12.0 AR



Upper Pleistocene



Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 20

Página 460 de 632










1373 EJ This fault system could have caused the historical Ribagorça earthquake (Ortuño, 2008).


Olivera, C. y Fleta, J., 1996. Analysis of Microearthquakes (1986-1993) in Vielha Area, Axial Zone of the Central Pyrenees. European Seismological Commision, XXV General Assembley, Reykjavik, Iceland. 288-293.







References

Variability





ES811


3th march 1373

42º38’ N, 0º41’E





705

ES811

Microseismicity 1986-2005 maladeta massif

M =2-4 Institut Cartografic

de Catalunya

(ICC)


distribution


707

Página 461 de 632



ID: FR001 Fault Name: Tech

Segment Name:


Location Y: 42.54298512

Name of Compiler(s): Martín Banda, R.

Filiation: IGME



Average Strike(º): 254 ± 10 LD Briais et al (1990); Calvet (1985); Carte géologique de la France 1/1.000.000; NEOPAL -Déformations récentes et paléoséismes- (BRGM)

Dip (º): 60 ± 5 EJ

Rake (º): -90 ± 10 LD Briais et al (1990); Calvet (1985); NEOPAL -Déformations récentes et paléoséismes- (BRGM)

Sense of Movement: N N-R LD Briais et al (1990); Calvet (1985); NEOPAL -Déformations récentes et paléoséismes- (BRGM); Philip et al. (1992)

Length (km): 40.0 ± 3 LD Briais et al (1990); Carte géologique de la France 1/1.000.000; NEOPAL -Déformations récentes et paléoséismes- (BRGM). Lacan and Ortuño (2012) consider active a much shorter section, 20 km length.


Max Depth (km): 10.0 10-20 km EJ Estimated depth of the seismogenic crust

Width (km): 11.5 AR

Area (km²): 461.88 AR


Upper Pleistocene

Holocene? LD Briais et al (1990); NEOPAL -Déformations récentes et paléoséismes- (BRGM)


0.100 0.06-0.16 LD Briais et al (1990); NEOPAL -Déformations récentes et paléoséismes- (BRGM)


0 EJ Assumed pure dip slip.


0.115 0.069-0.185 AR From dip, rake and VSR.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

The presence of an E-W topographic linear scarp which affect the Würmian terrace.

Briais et al (1990); NEOPAL -Déformations récentes et paléoséismes- (BRGM). Lacan and Ortuño (2012).

Geological Set: Pyrenees Orientales (France)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 28

Página 462 de 632




Unknown


7.00 ± 0.37 ER Using NEOPAL estimation of length and Stirling et al (2002) equation for instrumental data.




1428 AD LD This fault could have caused the historical Queralbs (Girona) earthquake (Briais et al., 1990).


BRIAIS A. ARMIJO R. WINTER T. TAPPONNIER P. HERBECQ A. (1990). Morphological evidence for Quaternary normal faulting and seismic hazard in the Eastern Pyrenees. Annales Tectonicae, IV, 1, 19-42.

CALVET M. (1985). Néotectonique et mise en place des reliefs dans l'est de Pyrénées : l'exemple du horst des Albères. Revue de Géologie dynamique et de géographie physique, 26, 119-130.

CALVET M. (1999). Rythmes et vitesse d'évolution morphogénétique dans un orogène alpin. Le cas des Pyrénées orientales franco-espagnoles. Z. Geomorph, 118, 91-105.

CALVET M. (1999). Régimes des contraintes et volumes de relief dans l'est des Pyrénées. Géomorphologie :relief, processus environnement, n°3, 253-278.

CLAUZON G. (1990). Restitution de l'évolution géodynamique néogène du bassin du Roussillon, et de l'unité adjacente des Corbières d'après les données écostratigraphiques et paléogéographique. Paléobiologie continentale, Montpellier, XVII, 1990, 125-155.

COINTRE M. (1987). Etude néotectonique des Pyrénées orientales. DEA Univ. de Montpellier (USTL).

DENSMORE A. L., ELLIS M. A, ANDERSON, S. R. (1998). Landsliding and the évolution of normal fault-bounded mountains, JGR, 103, B7, 15,203-15,219.

ELLIS M. A, DENSMORE A. L, ANDERSON, S. R (1999). Development of mountainous topography in the Basin Ranges, USA, Basin Research, 11, 21-41.

Lacan, P. and Ortuño, M. (2012). Active Tectonics of the Pyrenees: A review. Journal of the Iberian Geology, 38 (1) 9-30.

MAUREL O, BRUNEL M, MONIE P (2002). Exhumation Cénozoique des massifs du Canigou et de Mont-Louis (Pyrénées orientales, France), C. R. Géosciences, 334, p941-948.

NEOPAL (2011) Base de données nationale des déformations récentes et des paléoséismes.BRGM. Www.neopal.net

PHILIP H., BOUSQUET J.C., ESCUER J., FLETA J., GOULA X. ET GRELLET B. (1992). Présence de failles inverses d'âge quaternaire dans l'est des Pyrénées : implications sismotectoniques, C. R. Acad. Sci. Paris, 314, 1239-1245.

STIRLING, M.; Rhoades, D. & Berryman, K. (2002): Comparison of earthquake scaling relations derived from data of the instrumental and preinstrumental era. Bulletin of the Seismological Society of America, 92: 812-830.

VERGES J., MILLAN H., ROCA E, MUNOZ J.A., MARZO M., CIRES J., DEN BEZEMER T., ZOETEMEIJER R., CLOETINGH S (1995).




References

Variability





FR001

Queralbs (Girona) 2/02/1428 2.1667, 42.3500

IX - X (MSK) IGN and www.sisfran

ce.net

Briais et al. (1990) in NEOPAL.NET

Briais et al. (1990) in NEOPAL.NET679

Página 463 de 632



Eastern Pyrenees and related foreland basins: pre- syn- and post-collisional crustal-scale cross-section, Marine and Petroleum Geology, vol 12, No 8, pp 893-915.


Página 464 de 632



ID: FR005 Fault Name: Herrére

Segment Name:

Location X: -0.65735172

Location Y: 43.13827536

Name of Compiler(s): Lacan, P., García-Mayordomo, J. and Martín-Banda, R.

Filiation: UNAM-México, IGME and UCM

Email: [email protected].


Average Strike(º): 090 ± 10 LD Dubos-salee et al. (2007), Lacan et Ortuño (2012)

Dip (º): 90 ± 20 LD Dubos-salee et al. (2007), Lacan et Ortuño (2012)

Rake (º): 180 ± 20 LD Dubos-salee et al. (2007), Lacan et Ortuño (2012)

Sense of Movement: D LD Dubos-salee et al. (2007), Lacan et Ortuño (2012)

Length (km): 16.5 to 30 LD Compiler's measurement, based on Dubos-salee et al. (2007), Lacan et Ortuño (2012)

Min Depth (km): 5 LD Dubos-salee et al. (2007), Lacan et Ortuño (2012)

Max Depth (km): 25.0 LD Dubos-salee et al. (2007), Lacan et Ortuño (2012)

Width (km): 20.0 AR

Area (km²): 330.00 AR


18 ky ± 2 kyr LD Niviére et al. (subbmited)


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Indirect geomorphic evidences, seismicity (1980 Arudy, M = 5.1). (Dubos-salee et al., 2007; Lacan, 2008; Lacan et al., 2012). Comité de pilotage Néopal (2008) argues that the recent activity is not yet demostrated.

Lacan et al. (2012), Dubos-salee et al. (2007), Comité de pilotage Néopal (2008).

Geological Set: North Western Pyrenees

Identification Method: Geophysical/Geomorphological field mapping

Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 32

Página 465 de 632




6.61 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw could reach to 6.9 if the maximum length (30 km) is considered. Mw is 6.50 according to Dubos-Salee et al. (2007).




Unknown


Comité de pilotage Néopal (2008) Visite de terrain: rapport de mission sur le terrain dans les Pyrenees Centrales du Comite de Pilotage de la base NEOPAL le jeudi 23 octobre 2008. Available on-line at www.neopal.net/donneesDownLoad.asp

Courjault-Radé, P., Darrozes, J., Gaillot, P. (2009): The M=5.1 1980 Arudy earthquake sequence (western Pyrenees, France): a revisited multi-scale integrated seismologic, geomorphologic and tectonic investigation. Int. J. Earth Sci. Doi: 10.1007/s00531-008-0320-5.

Dubos-Sallée, N., Nivière, B., Lacan, P., Hervouët, Y. (2007): A structural model for the seismicity of the Arudy (1980) epicentral area (Western Pyrenees, France). Geophys. J. Int. 171, 259-270, doi: 10.1111/j.1365-246X.2007.03499.x.

Lacan, P. (2008): Activité Sismotectonique Plio-Quaternaire de l’Ouest des Pyrénées. PhD. Thesis. Université de Pau et des Pays de l’Adour: 284 p.

Lacan, P., Ortuño, M. (2012), Active Tectonics of the Pyrenees: A review, Journal of Iberian Geology 38(1), 9-30. DOI: 10.5209/rev_JIGE.2012.v38.n1.39203

Lacan, P., Nivière, B., Rousset, D., Sénéchal, P. (2012): Late Pleistocene folding above the Mail Arrouy Thrust, North-Western Pyrenees (France). Tectonophysics 541-543, 57-68. doi: 10.1016/j.tecto.2012.03.022.

Nivière, B., Lacan, P., Regard, V., Delmas, M., Calvet, M. (submitted): Cosmogenic dating of an alluvial terrace in the foothills of the western Pyrenees. Implication on the late glacial chronology, Submitted to Geomorphology.


Source Comment



References

Variability



Página 466 de 632



ID: FR008 Fault Name: Mail Arrouy

Segment Name:

Location X: -0.66451531

Location Y: 43.11511279

Name of Compiler(s): Lacan, P., García-Mayordomo, J. and Martín-Banda, R.

Filiation: UNAM-México, IGME and UCM

Email: [email protected].


Average Strike(º): 110 ± 10 LD Dubos-salee et al. (2007), Lacan et al. (2012), Lacan et Ortuño (2012)

Dip (º): 30 ± 20 LD Dubos-salee et al. (2007), Lacan et al. (2012), Lacan et Ortuño (2012)

Rake (º): 90 ± 10 LD Dubos-salee et al. (2007), Lacan et al. (2012), Lacan et Ortuño (2012)

Sense of Movement: R LD Dubos-salee et al. (2007), Lacan et al. (2012), Lacan et Ortuño (2012)

Length (km): 30.0 ± 5 LD Dubos-salee et al. (2007), Lacan et al. (2012), Lacan et Ortuño (2012)

Min Depth (km): 5 LD Dubos-salee et al. (2007), Lacan et al. (2012), Lacan et Ortuño (2012)

Max Depth (km): 20.0 LD Dubos-salee et al. (2007), Lacan et al. (2012), Lacan et Ortuño (2012)

Width (km): 30.0 AR

Area (km²): 900.00 AR


18 kyr ± 2 kyr LD Niviére et al. (subbmited).


0.250 0 to 0.5 LD Lacan et al. (2012).




0.5 to 1.000 AR From VSR, dip and rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Fluvial terraces folded, subsurface geophysics, seismicity (Dubos-salee et al., 2007; Lacan, 2008; Lacan et al., 2012). Comité de pilotage Néopal (2008) argues that the recent activity is not yet demostrated.

Lacan et al. (2012), Dubos-salee et al. (2007), Comité de pilotage Néopal (2008).

Geological Set: North Western Pyrenees


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 35

Página 467 de 632




6.85 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.50 according to Dubos-salee et al. (2007).




since 18000 LD Lacan et al. (2012); Niviére et al. (subbmited).


Comité de pilotage Néopal (2008) Visite de terrain: rapport de mission sur le terrain dans les Pyrenees Centrales du Comite de Pilotage de la base NEOPAL le jeudi 23 octobre 2008. Available on-line at www.neopal.net/donneesDownLoad.asp

Courjault-Radé, P., Darrozes, J., Gaillot, P. (2009): The M=5.1 1980 Arudy earthquake sequence (western Pyrenees, France): a revisited multi-scale integrated seismologic, geomorphologic and tectonic investigation. Int. J. Earth Sci. Doi: 10.1007/s00531-008-0320-5.

Gagnepain-Beyneix, J., Haessler, H., Modiano, T. (1982): The Pyrenean earthquake of February 29, 1980: an example of complex faulting, Tectonophysics 85, 273-290. doi:10.1016/0040-1951(82)90106-8.

Lacan, P. (2008): Activité Sismotectonique Plio-Quaternaire de l’Ouest des Pyrénées. PhD. Thesis. Université de Pau et des Pays de l’Adour: 284 p.

Lacan, P., Ortuño, M. (2012), Active Tectonics of the Pyrenees: A review, Journal of Iberian Geology 38(1), 9-30. DOI: 10.5209/rev_JIGE.2012.v38.n1.39203

Lacan, P., Nivière, B., Rousset, D., Sénéchal, P. (2012): Late Pleistocene folding above the Mail Arrouy Thrust, North-Western Pyrenees (France). Tectonophysics 541-543, 57-68. doi: 10.1016/j.tecto.2012.03.022.

Nivière, B., Lacan, P., Regard, V., Delmas, M., Calvet, M. (submitted): Cosmogenic dating of an alluvial terrace in the foothills of the western Pyrenees. Implication on the late glacial chronology, Submitted to Geomorphology.



Source Comment



References

Variability



Página 468 de 632



ID: ME001 Fault Name: Golfo de Rosas

Segment Name:

Location X: 2.9736

Location Y: 42.3458


Filiation: ICM-CSIC



Average Strike(º): 135 LD Roca (1992); Perea (2006). Strike changes from north being 134 until (3.194, 42.185), 142 until (3.573, 41.824).




Length (km): 76.0 ± 1 LD Perea (2006)



Width (km): 15.6 AR

Area (km²): 1184.72 AR


Plio-Quaternary

LD Roca (1992); Perea (2006).


0.030 0.030-0.070 LD Displacement on the Plio-Quaternary seismic reflectors:140m/5Ma and 2Ma (Perea, 2006).




0.035 0.035-0.081 AR From VRS, dip and rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Faults affecting identified Plio-Quaternary seismic reflectors. Roca (1992); Perea (2006).

Geological Set: Mediterranean Sea (Onshore-offshore East Girona)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 260

Página 469 de 632




7.24 ± 0.37 ER Magnitude from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 7.30 using Wells and Coppersmith (1994) surface rupture length relationship for normal faults (Perea, 2006; Perea et al., 2006).


64618 231929-7779 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Perea et al. (2006) obtained 95,000 yrs considering Mw 7.30 from W&C'94 and 0.030 m/ka. The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown














References

Variability



Página 470 de 632



ID: ME002 Fault Name: Amposta Western Fault

Segment Name:

Location X: 0.397

Location Y: 40.284


Filiation: ICM-CSIC



Average Strike(º): 027 LD Roca (1992); Perea (2006).







Width (km): 15.6 AR

Area (km²): 280.59 AR


Plio-Quaternary

LD Roca (1992); Perea (2006).








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential


Geological Set: Mediterranean Sea (Offshore East Castellón-Tarragona


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 263

Página 471 de 632




6.64 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.50 using Wells and Coppersmith (1994) surface rupture length relationship for normal faults (Perea, 2006; Perea et al., 2006).


53314 366766-9761 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Perea et al. (2006) obtained 38000 yrs considering Mw 6.50 from W&C'94 and 0.020 m/ka. The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown











Source Comment



References

Variability



Página 472 de 632



ID: ME003 Fault Name: Amposta Central Fault

Segment Name:

Location X: 0.431

Location Y: 40.217


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 545.60 AR


Plio-Quaternary

LD Roca (1992); Perea (2006).








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential




Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 264

Página 473 de 632








Unknown











Source Comment



References

Variability



Página 474 de 632



ID: ME004 Fault Name: Amposta Eastern Quaternary Fault

Segment Name:

Location X: 0.691

Location Y: 40.443

Name of Compiler(s): García-Mayordomo, J., Fernández, F., Bohoyo, F., Maestro, A.

Filiation: IGME



Average Strike(º): 175 ± 5 LD This is the strike of the Quaternary trace of the Amposta Eastern Fault. The geometry and dimensions of the fault have changed since Pliocene (Fernández et al, 2014).

Dip (º): 30 ± 10 LD Representative value. It is a listric fault, so dip varies with depth, but it also varies along strike. For the central and southern parts from an average 42º (top) to 17º (bottom), and for the northern 60 to 40º (Fernández et al, 2014).

Rake (º): -90 ± 10 LD Assumed pure normal fault, based on Roca (1992 and 1996), Roca and Guimerà (1992), Perea (2006), Perea et al (2006), Fernández et al (2014).

Sense of Movement: N N to ND LD Roca (1992 and 1996); Roca and Guimerà (1992); Perea (2006); Perea et al (2006); Perea et al (2012); Fernández et al (2014). Under the current stress regime it may have a dextral component.

Length (km): 16.0 +2 LD Length of the Quaternary fault trace (Fernández et al, 2014). The Quaternary fault trace may extend further to the south, but the lack of available seismic lines prevents confirming it.

Min Depth (km): 0.1 0.1-1.6 LD Closest distance to surface as interpreted in seismic profiles (Fernández et al, 2014)

Max Depth (km): 3.1 3-15 LD The fault seems to attenuate into the Mesozoic cover (Fernández et al, 2014), although it could be rooted in a deeper fault in the crystalline basement. Perea et al (2006) estimated 15 km based on

Width (km): 6.0 4-7.4 AR Width varies along strike, Fernández et al (2014) measured 4 to 7.4 km.

Area (km²): 96.00 ±6 AR Fernández et al (2014) measured a total of 96±6 km2 of fault area affecting Quaternary.


Middle Pleistocene

Pleistocene-Holocene

LD Roca (1992); Perea (2006), Perea et al (2006), Perea et al (2012), Fernández et al (2014). The fault activity very likely reaches Upper Pleistocene and may be Holocene. No numeric dating available.


0.105 0.08-0.13 AR From NSR, dip and rake. Perea (2006) estimated 0.04-0.10 m/ky assuming a vertical offset of 193 m in the last 5 or 3 Ma.




0.21 0.16-0.26 LD Fernández et al (2014). Previous estimation from Perea´s (2006) VSR resulted in 0.115-0.046 m/ky.

Identification


Quaternary Activity

Variability Source

Comment

Fault offsets Quaternary units (Arenas del Ebro) and reflectors (Ebro marker). It reaches very close to the surface (100 m).

Roca (1992), Perea (2006), Perea et al (2006), Perea et al (2012), Fernández et al (2014)



Comment


A+*Strength Class:


Orden Visual: 265

Página 475 de 632




Unknown


Unknown


Unknown


6.59 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Fernández et al (2014) estimate an average Mw 6.1±0.3 from length and rupture area using Wesnousky (2008) and Yen an Ma (2011).


14430 67976-3247 AR Considering the Maximum Earthquake Model (Wesnousky, 1986): RI = Mo f(Mw±d) / Mo f(SR±d). Perea et al. (2006) obtained 53,000 yrs considering Mw 7.10 from W&C'94 and 0.040 m/ky. The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown


Fernández, F., Bohoyo, F., Maestro, A. and García-Mayordomo, J. (2014) Nuevas aportaciones sobre las características geométricas del sistema de fallas Amposta Oriental-Montsià Norte (Margen Catalano-Valenciano, España). Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología (Iberfault), Lorca, España, pp. 105-108.










Wesnousky, S. G. (2008). Displacement and geometrical characteristics of earthquake surface ruptures: Issues and implications for seismic hazard analysis and the process of earthquake rupture. Bulletin of the Seismological Society of America, 98(4): 1609–1632.

Yen, Y.-T., and K.-F. Ma (2011). Source-scaling relationship for M 4.6–8.1 earthquakes, specifically for earthquakes in the collision zone of Taiwan. Bulletin of the Seismological Society of America, 101(2): 464–481.




References

Variability



Paleoearthquakes

Página 476 de 632



ID: ME005 Fault Name: Cabo de Cullera Western Fault

Segment Name:

Location X: -0.175

Location Y: 39.158


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 436.48 AR


Plio-Quaternary

LD Roca (1992); Perea (2006).








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential


Geological Set: Mediterranean Sea (Offshore East Valencia)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 266

Página 477 de 632








1396 AD LD This fault could have caused the historical Tabernas earthquake (Perea, 2006)


López Marinas, J.M. (1982): ¿Uno o dos terremotos catastróficos a fines del siglo XIV en el Reino de Valencia? Rev.Inst.Estudios Alicantinos, 36, 59-72.










Source Comment



References

Variability





ME005

Tabernas earthquake

18/12/1396 -0.3203, 39.1657

IMSK = IX / Mw = 6.7

López Marinas (1982)

Spatial correlation and macroseismic data

analysis

Perea (2006) propose this fault or "Centro-Occidental del Cabo de Cullera" as the possible sources of this earthquake. Mw is obtained from Boxer (Gasperini, 1999).

605

Página 478 de 632



ID: ME006 Fault Name: Cabo de Cullera Central-Western Fault

Segment Name:

Location X: -0.134

Location Y: 39.186


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 389.71 AR


Plio-Quaternary

LD Roca (1992); Perea (2006).








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential




Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 267

Página 479 de 632








1396 AD LD This fault could have caused the historical Tabernas earthquake (Perea, 2006)


López Marinas, J.M. (1982): ¿Uno o dos terremotos catastróficos a fines del siglo XIV en el Reino de Valencia? Rev.Inst.Estudios Alicantinos, 36, 59-72.










Source Comment



References

Variability





ME006

Tabernas earthquake

18/12/1396 -0.3203, 39.1657

IMSK = IX / Mw = 6.7

López Marinas (1982)

Spatial correlation and macroseismic data

analysis

Perea (2006) propose this fault or "Occidental del Cabo de Cullera" as the possible sources of this earthquake. Mw is obtained from Boxer (Gasperini, 1999).

606

Página 480 de 632



ID: ME007 Fault Name: Cabo de Cullera Central-Eastern Fault

Segment Name:

Location X: 0.007

Location Y: 39.463


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 748.25 AR


Plio-Quaternary

LD Roca (1992); Perea (2006).








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential




Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 268

Página 481 de 632








Unknown











Source Comment



References

Variability



Página 482 de 632



ID: ME008 Fault Name: Cabo de Cullera Eastern Fault

Segment Name:

Location X: 0.062

Location Y: 39.392


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 249.42 AR


Plio-Quaternary

LD Roca (1992); Perea (2006).








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential




Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 269

Página 483 de 632








Unknown











Source Comment



References

Variability



Página 484 de 632



ID: ME009 Fault Name: Southwest of Columbretas Basin

Segment Name:

Location X: 0.242

Location Y: 39.291


Filiation: ICM-CSIC










Width (km): 15.6 AR

Area (km²): 155.88 AR


Plio-Quaternary

LD Roca (1992); Perea (2006).








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential




Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 270

Página 485 de 632








Unknown











Source Comment



References

Variability



Página 486 de 632



ID: ME010 Fault Name: Alborán Ridge North

Segment Name:

Location X: -3.117

Location Y: 36.037

Name of Compiler(s): Estrada, F., Vázquez, J.T. and Ercilla, G.

Filiation: ICM (Barcelona); IEO (Málaga)



Average Strike(º): 080 ± 5 LD Álvarez-Gómez et al. (2011); Estrada et al. (2014)

Dip (º): 60 ± 20 LD Álvarez-Gómez et al. (2011); Estrada et al. (2014)

Rake (º): 45 ± 25 LD Álvarez-Gómez et al. (2011); Estrada et al. (2014)

Sense of Movement: SR LD Álvarez-Gómez et al. (2011); Estrada et al. (2014)

Length (km): 37.4 ± 5 LD Álvarez-Gómez et al. (2011); Estrada et al. (2014)

Min Depth (km): 0 + 0.5 LD Álvarez-Gómez et al. (2011); Estrada et al. (2014)

Max Depth (km): 11.0 + 5 / - 2 LD Álvarez-Gómez et al. (2011)

Width (km): 12.7 9/25 AR

Area (km²): 475.04 288-1050 AR


Quaternary s.l. LD Estrada et al. (2014)


Unknown


Unknown



1.02 LD Álvarez-Gómez et al. (2011)


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Faulting, folding and tilting of Plio-Quaternary sediments. Estrada et al. (2014)

Geological Set: Alboran Sea (Offshore Africa)


Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 271

Página 487 de 632




6.94 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.7 (6.5-7.0) using Wells y Coppersmith (1994) from Area - Mw relationship (Alvarez-Gomez et al., 2010).




Unknown


Álvarez-Gómez, J. A., Aniel-Quiroga, Í., González, M., Olabarrieta, M., Carreño, E., 2011. Scenarios for earthquake-generated tsunamis on the Alboran Sea, Western Mediterranean. Marine Geology, 284:55-73.

Estrada, F. Ercilla, G., Alonso, B., 1997. Pliocene-Quaternary Tectonic-sedimentary Evolution of the Northeastern Alboran Sea (SW Mediterranean Sea). S. Cloetingh and M. Fernández (Eds.) Origin of Sedimentary Basins., Spc. Vol. Tectonophysics 282, 423-442.

Estrada, F., J.T. Vázquez, G. Ercilla, B. Alonso, E. d’Acremont, C. Gorini, M. Gómez, M.C. Fernández-Puga, A. Ammar y B. El Moumni, 2014. Recent tectonic inversion of the Central Alboran Zone. IBERFAULT, Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España.

Martínez-García, P., Soto, J.I. & Comas, M. (2011). Recent structures in the Alboran Ridge and Yusuf fault zones based on swath bathymetry and sub-bottom profiling: evidence of active tectonics. Geo-Mar. Lett., 31, 16–39. doi:10.1007/s00367-010-0212-0.

Martínez-García, P., Comas, M., Soto, J.I., Lonergan, L. & Watts, A.B. (2013). Strike-slip tectonics and basin inversion in the WesternMediterranean: the Post-Messinian evolution of the Alboran Sea. Basin Research (2013) 25, 1–27, doi: 10.1111/bre.12005.

Pérez-Belzuz, F., 1999. Geología del Margen y Cuenca de Mar de Alborán Durante el Plio-Cuaternario: Sedimentación y Tectónica, PhD Thesis, CSIC, Universidad de Barcelona.


Vázquez, J.T., 2001. Estructura del margen septentrional del Mar de Alboran. PhD Thesis, Universidad Complutense de Madrid

Vázquez, J.T., F. Estrada, R. Vegas, G. Ercilla, E. d’Acremont, L.M. Fernández-Salas, B. Alonso, M.C. Fernández-Puga, M. Gómez-Ballesteros, Ch. Gorini, P. Bárcenas, D. Palomino, 2014. Quaternary tectonics influence on the Adra continental slope morphology (Northern Alboran Sea). IBERFAULT, Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España.

Source Comment



References

Variability



Página 488 de 632



ID: ME012 Fault Name: Alborán Ridge South

Segment Name:

Location X: -2.68580392

Location Y: 36.00089458

Name of Compiler(s): García-Mayordomo, J. and Álvarez-Gómez, J.A.

Filiation: IGME, UCM



Average Strike(º): 242 ± 5 LD Álvarez-Gomez et al. (2011); Martínez-García et al. (2011, 2013)

Dip (º): 60 ± 20 LD Álvarez-Gomez et al. (2011); Martínez-García et al. (2011, 2013) indicates subvertical dip.

Rake (º): 70 ± 20 LD Álvarez-Gomez et al. (2011); Martínez-García et al. (2011, 2013)

Sense of Movement: RS LD Álvarez-Gomez et al. (2011); Martínez-García et al. (2011) indicates a dominant strike-slip character.

Length (km): 93.0 ± 5 LD Álvarez-Gomez et al. (2011); Martínez-García et al. (2011), fig. 11 suggests that the fault trace may be divided in two sections.

Min Depth (km): 0 + 0.5 LD Álvarez-Gomez et al. (2011); Martínez-García et al. (2011, 2013)

Max Depth (km): 11.0 + 5 / - 2 LD Álvarez-Gomez et al. (2011)

Width (km): 12.7 9/25 AR

Area (km²): 1181.26 804/2450 AR


Lower Pleistocene

Holocene LD Martínez-García et al. (2011, 2013). The age of deposits affected by the fault are probably younger than Lower Pleistocene (1.8-0.8 ma).


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Faulting, folding and tilting of Quaternary sediments, scarps. Martínez-García et al. (2011, 2013)



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 272

Página 489 de 632








Unknown




Martínez-García, P., Comas, M., Soto, J.I., Lonergan, L. & Watts, A.B. (2013). Strike-slip tectonics and basin inversion in the Western Mediterranean: the Post-Messinian evolution of the Alboran Sea. Basin Research (2013) 25, 1–27, doi: 10.1111/bre.12005.





References

Variability



Página 490 de 632



ID: ME013 Fault Name: Jebha Offshore

Segment Name:

Location X: -3.71974632




Email: joseantonio.alvarezgomez@


Average Strike(º): 242 ± 5 LD Álvarez-Gomez et al. (2011)

Dip (º): 60 ± 20 LD Álvarez-Gomez et al. (2011)

Rake (º): 70 ± 20 LD Álvarez-Gomez et al. (2011). Martínez-García et al. (2011) interprets a predominant strike-slip character.

Sense of Movement: RS LD Álvarez-Gomez et al. (2011). Martínez-García et al. (2011) interprets a predominant strike-slip character.

Length (km): 58.0 ± 5 LD Álvarez-Gomez et al. (2011)

Min Depth (km): 0 + 0.5 LD Álvarez-Gomez et al. (2011)

Max Depth (km): 11.0 + 5 / - 2 LD Álvarez-Gomez et al. (2011)

Width (km): 12.7 10.1/25 AR

Area (km²): 736.70 592/1568 AR


Quaternary s.l. EJ Assumed from Martínez et al. (2011, 2013) and Calvert et al. (1997) descriptions and interpretations, among others. Benmakhlouf et al. (2012) founds no Quaternary activity on the onshore part of the Jebha Fault.


2.420 1.87-2.97 EJ From Vernant et al. (2010) CHEF and KTMA GPS stations at both sides of the fault, results 1.1 mm/yr on N141. A shortening of 1.08 considering fault strikes N60º and dips 60-70º, draws a dip-slip and dextral components of 2.2-3.2 and 0.21 mm/yr, respect.


0.26 0.21-0.31 EJ From NSR and a calculated rake of 174º, reverse with a bit of a dextral component. This is not consistent with the general interpretation of the fault as reverse or reverse with sinistral component.


2.68 2.17-3.18 EJ From dip, rake and VSR. This is likely an overestimation as the fault may be more strike-slip type, with a high dip (80-90º), rather than reverse and dip=60-70.




Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Recent deformation structures along southern Xauen Bank, association to seismicity.

Calvert et al. (1997), Chalouan et al. (1997, 2006), Comas et al. (1999), Martínez-García et al. (2011, 2013), Álvarez-Gómez et al. (2011). This fault is interpreted as the offshore continuation of the Jebha Fault (Morocco).



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 273

Página 491 de 632








Unknown



Benmakhlouf, M., Galindo-Zaldívar, J., Chalouan, A., de Galdeano, C. S., & López-Garrido, A. C. (2012). Inversion of transfer faults: the Jebha–Chrafate fault (Rif, Morocco). Journal of African Earth Sciences, 73, 33-43.

Calvert, A., Gomez, F., Seber, D., Barazangi, M., Jabour, N., Ibenbrahim, A., & Demnati, A. (1997). An integrated geophysical investigation of recent seismicity in the Al-Hoceima region of North Morocco. Bulletin of the Seismological Society of America, 87(3), 637-651.

Chalouan, A., Saji, R., Michard, A., & Bally, A. W. (1997). Neogene tectonic evolution of the southwestern Alboran Basin as inferred from seismic data off Morocco. AAPG bulletin, 81(7), 1161-1184.

Chalouan, A., Galindo-Zaldívar, J., Akil, M., Marín-Lechado, C., Chabli, A., Ruano, P., ... & Gourari, L. (2006). Tectonic wedge escape in the southwestern front of the Rif Cordillera (Morocco). Geological Society of London.

Comas, M. C., & Soto, J. I. (1999). 25. Brittle deformation in the metamorphic basement at site 976: implications for middle Miocene extensional tectonics. In Proceedings of the Ocean Drilling Program: Scientific results (Vol. 161, p. 331). The Program.




Vernant, P., Fadil, A., Mourabit, T., Ouazar, D., Koulali, A., Davila, J. M., ... & Reilinger, R. (2010). Geodetic constraints on active tectonics of the Western Mediterranean: Implications for the kinematics and dynamics of the Nubia-Eurasia plate boundary zone. Journal of Geodynamics, 49(3), 123-129.




References

Variability



Página 492 de 632



ID: ME014 Fault Name: Tofiño Bank

Segment Name:

Location X: -4.26613863

Location Y: 35.54977067





Average Strike(º): 078 ± 5 LD Álvarez-Gómez et al., 2011

Dip (º): 45 ± 20 LD Álvarez-Gómez et al., 2011

Rake (º): 75 + 15 / - 20 LD Álvarez-Gómez et al., 2011

Sense of Movement: RS LD Álvarez-Gómez et al., 2011

Length (km): 49.0 ± 5 LD Álvarez-Gómez et al., 2011

Min Depth (km): 0 + 0.5 LD Álvarez-Gómez et al., 2011

Max Depth (km): 11.0 + 5 / - 2 LD Álvarez-Gómez et al., 2011

Width (km): 15.6 12.137/37.8 AR

Area (km²): 762.26 534/2044 AR


Quaternary s.l. LD Calvert et al. (1997); Chalouan et al. (1997); Martínez-García et al. (2011)


0.600 <0.6 LD Chalouan et al. (1997). This value must be regarded as a maximum.


0.227 <0.227 AR From NSR and assumed rake. This value must be regarded as a maximum.


0.878 <0.878 AR From VSR, dip and assumed rake. This value must be regarded as a maximum.


1.3 LD Álvarez-Gómez et al., 2011


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Prominent morphologic submarine topography, actively uplifted during Quaternary; Tilting and folding of Quaternary sediments.

Calvert et al. (1997); Chalouan et al. (1997); Martínez-García et al. (2011)



Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 274

Página 493 de 632








Unknown



Calvert, A., Gomez, F., Seber, D., Barazangi, M., Jabour, N., Ibenbrahim, A., & Demnati, A. (1997). An integrated geophysical investigation of recent seismicity in the Al-Hoceima region of North Morocco. Bulletin of the Seismological Society of America, 87(3), 637-651.

Chalouan, A., Saji, R., Michard, A., & Bally, A. W. (1997). Neogene tectonic evolution of the southwestern Alboran Basin as inferred from seismic data off Morocco. AAPG bulletin, 81(7), 1161-1184.

Martínez-García, P., Soto, J. I., & Comas, M. (2011). Recent structures in the Alboran Ridge and Yusuf fault zones based on swath bathymetry and sub-bottom profiling: evidence of active tectonics. Geo-Marine Letters, 31(1), 19-36.


Source Comment



References

Variability



Página 494 de 632



ID: ME015 Fault Name: Carboneras (2/2)

Segment Name: Southern


Location Y: 36.29203001

Name of Compiler(s): Moreno, X., Gràcia, E. and Masana, E.

Filiation: UTM-CSIC and RISKNAT-UB



Average Strike(º): 058 ± 2 LD Measured on multibeam bathymetric data (Moreno, 2010).

Dip (º): 90 ± 10 LD Calculated from seismic profiles (Moreno, 2010).

Rake (º): 0 EJ

Sense of Movement: S EJ Coherently with observations in the northern segment

Length (km): 36.0 ± 4 OD In surface and in High-res seismics, this segment is observed as at least two different segments with a stepover around (-2,941; 36,283), but more observation at seismogenic depth should be done to prove if this is significant to the seismic behaviour.

Min Depth (km): 0 LD Moreno, 2010.

Max Depth (km): 11.0 LD Lower depth of the instrumental seismicity according to IGN online seismic data base (Moreno, 2010).

Width (km): 11.0 AR

Area (km²): 396.00 AR


Holocene LD Faulted Holocene reflections can be observed in TOPAS profiles. The age of reflections is estimated from sedimentation rates obtained from sediment core analysis (Moreno, 2010).


0.040 LD This is a long-term value obtained from multichannel seismic profiles. We haven't considered more recent vertical offsets because the uncertainty caused by horizontally displacing an irregular topography (Moreno, 2010).


1.1 <1.100 EJ No linear feature offsets are observed and thus, no estimations of the strike-slip rate can be done. As expert judgement, the strike slip-rate should be similar to the one observed for the northern segment (<1.1 mm/y), but this needs to be confirmed.


1.1 0.5 <1.100 EJ Assumed pure strike-slip.


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Surface expression, Pressure Ridges, vertically offset quaternary reflection in seismic profiles

Moreno (2010).

Geological Set: Alboran Sea (Offshore Almería)


Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 193

Página 495 de 632




6.93 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.9 (± 0.3) using W&C'94 empirical relationship between Mw and max SRL for strike-slip faults. If considering smaller segments, the Mw would decrease.




Unknown

Extended Information: EXTENDED_INFORMATION\ME015.rar

Gràcia, E., Pallas, R., Soto, J. I., Comas, M., Moreno, X., Masana, E., Santanach, P., Diez, S., García, M., and Dañobeitia, J. (2006). Active faulting offshore SE Spain (Alboran Sea): Implications for earthquake hazard assessment in the Southern Iberian Margin. Earth and Planetary Science Letters 241, 734-749.


Masana, E., Gràcia, E., MARTINEZ DIAZ, J.J., Moreno, X., ORTUÑO, M., Perea, H., KHAZARADZE, G., Pallàs, R., Rodés, A., QUERALT, P., COLL, M, Bartolomé, R., GARCIA-MELENDEZ, E., RUANO, P., STEPANCIKOVA, P., DANOBEITIA, J.J., SANTANACH, P. (2010). Characterizing the seismic potential of the Eastern Betics Shear Zone (EBSZ), a major source of earthquakes in Southeastern Iberia. En: Contribución de la Geología al Análisis de la Peligrosidad Sísmica (J.M. Insúa y F.Martín-González, eds.), pp. 101-104. IBERFAULT, Sigüenza (Guadalajara), 27-29 Octubre 2010.

Moreno, X. (2010). Neotectonic and Paleoseismic Onshore-Offshore integrated study of the Carboneras Fault (Eastern Betics, SE Iberia). Doctoral Thesis, Barcelona University.

Moreno, X., Masana, E., Gràcia, E., Bartolomé, R., and Piqué-Serra, O. (2008). Estudio paleosismológico de la Falla de Carboneras: Evidencias tierra-mar de actividad tectónica reciente. GeoTemas 10, 1035-1038.

Moreno, X., Masana, E., Gràcia, E., Bartolomé, R., Rodés, A., and Pallàs, R. (2010). Onshore-Offshore active tectonics along the Carboneras Fault Zone (Eastern Betic Cordilleras). In "Contribución de la Geología al Análisis de la Peligrosidad Sísmica." (J. M. Insua-Arévalo, and F. Martín-González, Eds.), pp. 105-107, Sigüenza (Guadalajara, Spain).







References

Variability



Página 496 de 632



ID: ME016 Fault Name: Adra

Segment Name:

Location X: -3.039

Location Y: 36.625

Name of Compiler(s): Gràcia, E., Bartolomé, R., Lo Iacono, C., Moreno, X. and Masana, E.

Filiation: Unitat de Tecnologia Marina - CSIC / U. Barcelona



Average Strike(º): 130 LD Gràcia et al., 2012.

Dip (º): 80 ± 10 LD Gràcia et al., 2012.

Rake (º): -135 LD Gràcia et al., 2012.

Sense of Movement: DN LD Gràcia et al., 2012.

Length (km): 18.5 18.5-9.4 LD Gràcia et al., 2012.

Min Depth (km): 0 LD Gràcia et al., 2012.

Max Depth (km): 15.0 LD Gràcia et al., 2012.

Width (km): 15.2 AR

Area (km²): 281.78 AR


Holocene LD The fault reaches up to the surface, as demonstrated by MCS and TOPAS profiles. The age of the seafloor sediments is of Holocene age based on sediment cores (Gràcia et al., 2012).


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Surface expression, offset Quaternary horizons, seismicity (1910 Adra earthquake) (Stich et al., 2003; Gràcia et al., 2012).

Gràcia et al., 2012.

Geological Set: Alboran Sea (Offshore Almería)


Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 275

Página 497 de 632




6.48 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.47-6.18 if calculated according to Wells & Coppersmith (1994) rupture area relationship (Gràcia et al., 2012).




1910 AD LD This fault very likely caused the historical Adra 1910 earthquake (Stich et al., 2003; Gràcia et al., 2012)

Extended Information: EXTENDED_INFORMATION\ME016.rar


Gràcia, E., Bartolome, R., Lo Iacono, C., Moreno, X., Stich, D., Martínez-Diaz, J.J., Bozzano, G., Martínez-Loriente, S., Perea, H., Diez, S., Masana, E., Dañobeitia, J.J., Tello, O., Sanz, J.L., Carreño, E. & EVENT-SHELF Team (2012). Acoustic and seismic imaging of the Adra Fault (NE Alboran Sea) in search of the source of the 1910 Adra earthquake, Nat. Hazards Earth Syst. Sci., 12, 3255-3267, doi:10.5194/nhess-12-3255-2012.

Stich et al., 2003. Source parameters of the Mw 6.1 1910 Adra Earthquake (southern Spain). Geophys. J. Int., 155, 539-546.



Source Comment



References

Variability





ME016

Adra 1910 1910 Mw=6.1 Stich et al. (2003), Geophys. J. Int., 155, 539-546.

673

Página 498 de 632



ID: ME017 Fault Name: Yussuf (1/2)

Segment Name: Western

Location X: -2.823

Location Y: 36.078


Filiation: IGME



Average Strike(º): 104 ± 5 LD Mauffret et al. (1992), Martínez-García et al. (2011, 2013), Perea et al. (2012)

Dip (º): 90 ± 10 LD Martínez-García et al. (2011), Perea et al. (2012)

Rake (º): 170 ± 10 LD Álvarez-Gómez et al. (2011),

Sense of Movement: D LD Martínez-García et al. (2011, 2013), Perea et al. (2012)

Length (km): 94.8 ± 5 LD Gràcia et al. (2014)

Min Depth (km): 0 LD Surface expression and scarps. Martínez-García et al. (2011, 2013), Perea et al. (2012)

Max Depth (km): 11.0 EJ Lower depth of the instrumental seismicity according to IGN online seismic data base. The complete depth of the fault is lithospheric.

Width (km): 11.0 AR

Area (km²): 1042.80 AR


Holocene LD Mauffret et al. (1992), Martínez-García et al. (2011, 2013), Perea et al. (2012)


Unknown


Unknown





Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Prominent submarine lineament, high slope gradients, sea floor expression, offset present-day sediments and Quaternary horizons

Mauffret et al. (1992), Martínez-García et al. (2011, 2013), Perea et al. (2012)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 277

Página 499 de 632




7.33 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 7.37 (± 0.3) according to Wells & Coppersmith (1994) from L/Mw relationship.




Unknown

Extended Information: EXTENDED_INFORMATION\ME017-ME020.rar


Bartolomé, R., Gràcia, E., Lo Iacono, C., Martínez-Loriente, S., Moreno, X., Perea, H., Masana, E., EVENT-DEEP TEAM (2010). Seismic imaging of active faults in the Southern Alboran Sea (SE Iberian Margin): First results of the 2010 EVENT-DEEP cruise. En: Contribución de la Geología al Análisis de la Peligrosidad Sísmica (J.M. Insúa y F.Martín-González, eds.), pp. 155-158. IBERFAULT, Sigüenza (Guadalajara), 27-29 Octubre 2010.


Gràcia, E. et al. (2014) Seismic hazard of active faults in the Alboran sea inferred from submarine paleosismology. Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología (IBERFAULT), Lorca, España, 101-104.



Mauffret A, Maldonado A, Campillo AC (1992) Tectonic framework of the eastern Alboran and western Algerian basins, westernMediterranean. Geo Mar Lett 12(2/3):104–110. doi:10.1007/ BF02084919

Perea, H., Gràcia, E., Bartolomé, R., Ranero, C.R., Lo Iacono, C., Martínez- Loriente, S., Moreno, X.and EVENT-DEEP and TOPOMED-GASSIS teams (2012) The strike-slip Yussuf fault system (Alboran Sea): Multi-scale seismic imaging and evidences of Quaternary activity. Abstract in PANAF meeting, Istambul, October 8- 10, 2012.






References

Variability



Página 500 de 632



ID: ME018 Fault Name: Yussuf (2/2)


Location X: -2.128

Location Y: 35.883


Filiation: IGME



Average Strike(º): 001 ± 5 LD Mauffret et al. (1992), Martínez-García et al. (2011, 2013), Perea et al. (2012)

Dip (º): 90 ± 10 LD Martínez-García et al. (2011), Perea et al. (2012)

Rake (º): 170 ± 10 LD Álvarez-Gómez et al. (2011),

Sense of Movement: D LD Martínez-García et al. (2011, 2013), Perea et al. (2012)


Min Depth (km): 0 LD Surface expression and scarps. Martínez-García et al. (2011, 2013), Perea et al. (2012)

Max Depth (km): 11.0 EJ Lower depth of the instrumental seismicity according to IGN online seismic data base. The complete depth of the fault is lithospheric.

Width (km): 11.0 AR

Area (km²): 1084.60 AR


Holocene LD Mauffret et al. (1992), Martínez-García et al. (2011, 2013), Perea et al. (2012)


Unknown


Unknown





Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Prominent submarine lineament, high slope gradients, sea floor expression, offset present-day sediments and Quaternary horizons

Mauffret et al. (1992), Martínez-García et al. (2011, 2013), Perea et al. (2012)

Geological Set: Alboran Sea (Offshore Argelia)


Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 278

Página 501 de 632








Unknown








Mauffret A, Maldonado A, Campillo AC (1992) Tectonic framework of the eastern Alboran and western Algerian basins, westernMediterranean. Geo Mar Lett 12(2/3):104–110. doi:10.1007/ BF02084919

Perea, H., Gràcia, E., Bartolomé, R., Ranero, C.R., Lo Iacono, C., Martínez- Loriente, S., Moreno, X.and EVENT-DEEP and TOPOMED-GASSIS teams (2012) The strike-slip Yussuf fault system (Alboran Sea): Multi-scale seismic imaging and evidences of Quaternary activity. Abstract in PANAF meeting, Istambul, October 8- 10, 2012.






References

Variability



Página 502 de 632



ID: ME019 Fault Name: Al-Idrisi (1/2)

Segment Name: Northern

Location X: -3.68717631

Location Y: 35.63777476


Filiation: IGME



Average Strike(º): 030 ± 2 LD Gràcia et al. (2014), Martínez-García et al. (2011, 2013)

Dip (º): 75 ± 10 LD Álvarez-Gómez et al. (2011), Martínez-García et al. (2011, 2013)

Rake (º): 10 LD Álvarez-Gómez et al. (2011)

Sense of Movement: S LD Álvarez-Gómez et al. (2011), Martínez-García et al. (2011, 2013)


Min Depth (km): 0 LD Martínez-García et al. (2011, 2013)

Max Depth (km): 11.0 11-15 EJ Assumed the same value as in other similar faults in the area.

Width (km): 11.4 AR

Area (km²): 620.65 AR


<0.79 ma Holocene LD Martínez-García (2013). Very likely Holocene as the fault reaches up to the surface.


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

Surface expression, offset Quaternary horizons. Gràcia et al. (2014), Martínez-García et al. (2011, 2013)



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 279

Página 503 de 632








Unknown










Source Comment



References

Variability



Página 504 de 632



ID: ME020 Fault Name: Al-Idrisi (2/2)

Segment Name: Southern

Location X: -3.74400324

Location Y: 35.45305063


Filiation: IGME



Average Strike(º): 008 ± 2 LD Martínez-García et al. (2011, 2013), Gràcia et al. (2014)

Dip (º): 75 ± 10 LD Álvarez-Gómez et al. (2011), Martínez-García et al. (2011, 2013)

Rake (º): 10 LD Álvarez-Gómez et al. (2011)

Sense of Movement: S LD Álvarez-Gómez et al. (2011), Martínez-García et al. (2011, 2013)

Length (km): 17.2 17-50 LD Gràcia et al. (2014). Very likely the fault zone extends southwards into the seismic cluster of Al-Hoicema and even onshore along Trougout fault (d'Acremont et al., 2014)

Min Depth (km): 0 LD Martínez-García et al. (2011, 2013)

Max Depth (km): 11.0 11-15 LD Assumed the same value as in other similar faults in the area.

Width (km): 11.4 AR

Area (km²): 195.87 AR


<0.79 ma Holocene LD Martínez-García et al. (2011, 2013).Very likely Holocene as the fault reaches up to the surface. Southward extension of the fault may be related to scarps produced by the Al-Hoicema seismic events (d'Acremont et al., 2014).


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Surface expression, offset Quaternary horizons, likely relation to Al-Hoicema earthquake series

Martínez-García et al. (2011, 2013), Bartolomé et al. (2013), Gràcia et al. (2014), d'Acremont et al. (2014).



Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 280

Página 505 de 632




6.62 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.51 (± 0.3) according to Wells & Coppersmith (1994) from L/Mw relationship. Mw could much larger as the fault very likely extends southwards.




Unknown




d'Acremont, E., M.-A. Gutscher, A. Rabaute, Mercier de Lépinay, M. Lafosse, J.Poort, A.Ammar, A. Tahayt, P. Le Royc, J. Smit, D. Do Couto, R. Cancouët, C. Prunier, G. Ercilla, C. Gorini (2014). High-resolution imagery of active faulting offshore Al Hoceima, Northern Morocco. Tectonophysics, 632:160–166.










References

Variability



Página 506 de 632



ID: ME021 Fault Name: Bajo Segura Offshore

Segment Name:

Location X: -0.65245019

Location Y: 38.09164464

Name of Compiler(s): Perea, H., García-Mayordomo, J., Alfaro, P., Martín-Banda, R.

Filiation: ICM-CSIC, IGME, UA, IGME



Average Strike(º): 082 +4/-3 EJ García-Mayordomo (2005) based on Bajo Segura Onshore Fault characteristics and Alfaro et al. (2002).

Dip (º): 60 30-70 LD Dips to the south in SCS sparker and commercial MCS profiles in Alfaro et al. (2002) and Perea et al. (2012).

Rake (º): 90 LD Alfaro et al., 2002; Perea et al., 2012

Sense of Movement: R R-ANT LD Alfaro et al., 2002; Perea et al., 2012

Length (km): 29.3 EJ 10-30 km is the length of single faults included in the shear zone of the segment. Total length of the segment can be 60 km (ITGE, 1994). See García-Mayordomo (2005) Table 3.12 and p.167-168.

Min Depth (km): 1 1-2 LD Apparently sealed by unit I1, that generally shows little thickness in the area (Perea et al., 2012)


Width (km): 12.7 AR

Area (km²): 372.16 AR


>20 ka <20 ka LD Some fault strands might also offset or fold horizon H1 (20 ka) (Perea et al., 2012).


0.100 <0.1 m/ka EJ Estimated from Guardamar anticline onshore.




0.2 <0.2 m/ka EJ Estimated from Guardamar segment of Bajo Segura Onshore Fault (Alfaro et al., 2012). SR is probably lower as it seems that SR is lowering from the West (Hurchillo anticline) to the East (Guardamar anticline) and seawards.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Offsets and folds Quaternary sediments as seen in SCS Sparker profiles. The deformation zone is approx. 5 km wide including faults and folds.

Alfaro et al., 2002; Perea et al., 2012

Geological Set: Mediterranean Sea (Offshore East Alicante) Internal zo

Identification Method: Marine geophysical research

Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 139

Página 507 de 632




Unknown




9256 Unstated AR Considering the Maximum Earthquake Model (W'86): RI = Mo f(6.8±0.37) / Mo f(SR=0.2). RI should be longer than Bajo Segura Onshore, as slip rate decreases from W to E (Alfaro et al. 2012). The occurrence of smaller, damaging earthquakes may be much shorter


Unknown


Alfaro, P., Delgado, J., A. Estévez, Soria, J.M. y Yébenes, A. (2002a). Onshore and offshore compressional tectonics in the eastern Betic Cordillera (SE Spain). Marine Geology, 186, 337-349.



Geology, 38(1): 271-284.


I.T.G.E. (1994a). Mapa Geológico de la Plataforma Continental Española y Zonas Adyacentes a escala 1:200.000. Hoja nº 72-73, Elche-Alicante.

Perea, H., Gràcia, E., Alfaro, P., Bartolomé, R., Lo Iacono, C., Moreno, X., Masana, E., and EVENT-SHELF Team (2012): Quaternary active tectonic structures in the offshore Bajo Segura basin (SE Iberian Peninsula – Mediterranean Sea), Natural Hazards and Earth System Science, 12: 3151-3168, doi:10.5194/nhess-12-3151-2012, 2012.






References

Variability



Página 508 de 632



ID: ME023 Fault Name: Santa Pola

Segment Name: Santa Pola Offshore

Location X: -0.46850274


Name of Compiler(s): Perea, H., García-Mayordomo, J. and Martín-Banda, R.

Filiation: ICM-CSIC, IGME



Average Strike(º): 089 ± 2 LD Perea et al. (2012)

Dip (º): 60 30-70 LD Dips to the south in SCS sparker and commercial MCS profiles in Alfaro et al. (2002) and Perea et al. (2012).

Rake (º): 90 ± 10 EJ Fault motion might have lateral component as well.

Sense of Movement: R R-ANT LD Alfaro et al. (2002) and Perea et al. (2012). Strike-Slip fault with vertical movement (Perea et al., 2014).

Length (km): 36.2 ± 5 LD The fault zone is approx. 5 km wider and there is also folding.

Min Depth (km): 0 0.05 LD The fault does not outcrop but it is very close (meters) to the surface of the sea bottom (Sparker seismic profiles in Perea et al., 2012)

Max Depth (km): 8.0 LD Fault is rooted in the betic basement. We assume maximum depth as the depth the seismogenic crust in the Cartagena block (see table 4.19 and figs. 4.25-4.27 in García-Mayordomo, 2005).

Width (km): 9.2 AR

Area (km²): 334.40 AR


<144 ka 247-135 ka LD The fault offsets horizon H3 (247 ka) and layers under horizon H2 (135 ka) (Perea et al., 2012)


0.040 LD Perea et al. (2014)




0.046 EJ Assuming pure reverse kinematics (rake=90º), dip and VSR=0.04


2.7 0.35-2.7 OD Original data not published yet (H. Perea, pers. Com.)


6 6-10 OD Original data not published yet (H. Perea, pers. com.)


EJ No evidence.

Identification


Quaternary Activity

Variability Source

Comment


Perea et al. (2012)

Geological Set: Alicante Offshore, internal zone of the Betic Range.

Identification Method: Marine geophysical research (SCS Sparker)

Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 140

Página 509 de 632




6.90 ± 0.37 ER Magnitude from length using Stirling et al (2002) equation derived from the instrumental dataset. According to Perea et al. (2014) the Mw varies between 5.9 and 7.1 using Wells and Coppersmith (1994) relationships.


60536 Unstated LD Considering the Maximum Earthquake Model (Wesnousky, 1986). Perea et al. (2014) estimates 3,000-50,000 yrs considering Mw 5.9-7.1 from W&C'94 and 0.040 m/ka. The occurrence of smaller, damaging earthquakes may be much shorter.


Unknown





Perea, H., Gràcia, E., Martínez-Loriente, S., and Bartolomé, R. (2014). Submarine paleoseismology on the Santa Pola fault (Bajo Segura Basin, Western Mediterranean): Derivating direct on-fault paleoearthquakes. Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España, 121-124.






References

Variability



Página 510 de 632



ID: ME024 Fault Name: La Marina

Segment Name: La Marina Offshore



Name of Compiler(s): Perea, H., García-Mayordomo, J., Martín-Banda, R.

Filiation: UTM-CSIC, IGME



Average Strike(º): 082 ± 2 LD Perea et al. (2012).

Dip (º): 60 30-70 LD As seen in SCS sparker and commercial MCS profiles in Alfaro et al. (2002) and Perea et al. (2012).

Rake (º): 90 LD Alfaro et al. (2002) and Perea et al. (2012).

Sense of Movement: R R-ANT LD Alfaro et al. (2002) and Perea et al. (2012).

Length (km): 38.8 ± 1 LD Perea et al. (2012).

Min Depth (km): 0 0.05 LD The fault does not outcrop but is very close (meters) to the surface of the sea bottom (Sparker seismic profiles in Perea et al., 2012).

Max Depth (km): 8.0 LD Fault is rooted in the betic basement. We assume maximum depth as the depth the seismogenic crust in the Cartagena block (see table 4.19 and figs. 4.25-4.27 in García-Mayordomo, 2005).

Width (km): 9.2 AR

Area (km²): 358.42 AR


<135 ka 135-20 ka LD Some fault strands might also offset or fold horizon H1 (20 ka) (Perea et al., 2012).


Unknown


Unknown



Unknown


Unknown


EJ No evidence

Identification


Quaternary Activity

Variability Source

Comment


Perea et al. (2012)

Geological Set: Alicante Offshore, internal zone of the Betic Range.

Identification Method: Marine geophysical research (SCS Sparker)

Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 141

Página 511 de 632








Unknown









References

Variability



Página 512 de 632



ID: ME025 Fault Name: Barcelona

Segment Name:


Location Y: 41.43310306





Average Strike(º): 058 ± 2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Perea (2006).


Rake (º): -90 LD IGME and ENRESA (1998b) and Perea (2006).

Sense of Movement: N LD IGME and ENRESA (1998b) and Perea (2006).

Length (km): 52.0 ± 0.5 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Perea (2006).

Min Depth (km): 0

Max Depth (km): 15.0 ± 5 EJ By comparison to similar records in the area.

Width (km): 17.3 AR

Area (km²): 900.67 AR


Quaternary LD ITGE (1989)


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

It offsets Plio-Quaternary reflectors IGME and ENRESA (1998b).

Geological Set: Catalan Coastal Ranges and northern border of the Val

Identification Method: Marine geophysical methods

Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 261

Página 513 de 632








Unknown






Source Comment



References

Variability



Página 514 de 632



ID: ME026 Fault Name: Delta del Ebro

Segment Name:


Location Y: 40.59845423





Average Strike(º): 028 ± 2 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Perea (2006).


Rake (º): -90 LD IGME and ENRESA (1998b) and Perea (2006).

Sense of Movement: N LD IGME and ENRESA (1998b) and Perea (2006).

Length (km): 52.0 ± 0.5 LD Compiler's measurement, based on the Neotectonic Map of Spain, scale 1:1.000.000 (IGME and ENRESA, 1998a) and Perea (2006).



Width (km): Unknown



Quaternary LD ITGE (1989)


Unknown


Unknown



Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential

It offsets Plio-Quaternary reflectors IGME and ENRESA (1998b).

Geological Set: Catalan Coastal Ranges and northern border of the Val


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 262

Página 515 de 632








Unknown






Source Comment



References

Variability



Página 516 de 632



ID: ME027 Fault Name: Seco de Palos Fault Zone

Segment Name:


Location Y: 37.48887825





Average Strike(º): 014 10-16 (max 48) LD Compiler's measurement, based on Acosta et al. (2013).

Dip (º): 90 EJ Based on Acosta et al. (2013).

Rake (º): 0 LD Acosta et al. (2013).

Sense of Movement: S LD Acosta et al. (2013).

Length (km): 40.0 18 to 40 LD 40 km length of the longest strand. 18 km and 32 km length of the other strands in the fault zone (18 km width). Compiler's measurement, based on Acosta et al. (2013).

Min Depth (km): 0 LD Acosta et al. (2013).

Max Depth (km): 8.0 EJ Given value is the depth of the fragile crust. The fault depth is mantelic. García-Mayordomo (2005), table 4.21.

Width (km): 8.0 AR

Area (km²): 320.00 AR


Holocene LD Acosta et al. (2013)




0.05 <0.05 m/ka EJ By comparison with other active faults in the area (Table 3.30 y Fig. 3.29 in García-Mayordomo, 2005).


0.05 ± 0.01 AR From HSR and rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It offsets Quaternary reflectors Acosta et al. (2013).



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 188

Página 517 de 632




6.80 6.6 to 6.9 ER Magnitude from length using Stirling et al (2002) equation derived from the instrumental dataset and 40-18 km length.




Unknown


Acosta J., Fontán A., Muñoz A., Muñoz-Martín, A., Rivera, J., and Uchupi, E. (2013). The morpho-tectonic setting of the Southeast margin of Iberia and the adjacent oceanic Algero-Balear Basin. Marine and Petroleum Geology, 45:17-41.







References

Variability



Página 518 de 632



ID: ME028 Fault Name: Don Juan Fault Zone

Segment Name:


Location Y: 38.16081517





Average Strike(º): 120 ± 2 LD Compiler's measurement, based on Acosta et al. (2013).

Dip (º): 90 85-90 LD Acosta et al. (2013).

Rake (º): 180 LD Acosta et al. (2013).

Sense of Movement: D LD Acosta et al. (2013).

Length (km): 60.0 38 to 60 LD 60 km length of the longest strand. 38 km length of the other strand in the fault zone (12.5 km width). Compiler's measurement, based on Acosta et al. (2013).

Min Depth (km): 0 LD Acosta et al. (2013).

Max Depth (km): 8.0 EJ Given value is the depth of the fragile crust. The fault depth is mantelic. García-Mayordomo (2005), table 4.21.

Width (km): 8.0 AR

Area (km²): 480.00 AR


Holocene LD Acosta et al. (2013).








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

It offsets Quaternary reflectors Acosta et al. (2013).



Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 189

Página 519 de 632




7.00 6.9 to 7.1 ER Magnitude from length using Stirling et al (2002) equation derived from the instrumental dataset and the lengths of two strands.




Unknown









References

Variability



Página 520 de 632



ID: ME029 Fault Name: Las Moreras - Escarpe de Mazarrón (1/3)

Segment Name: Sierra de las Moreras - Cabo Tiñoso

Location X: -1.41273146

Location Y: 37.60068182

Name of Compiler(s): García Mayordomo, J. and Martín Banda, R.

Filiation: IGME and Universidad Complutense de Madrid

Email: [email protected]; raq


Average Strike(º): 104 + 2 / - 1 LD García-Mayordomo (2005); Acosta et al. (2013). To apply right hand rule criteria dip is considered towards S.

Dip (º): 90 LD García-Mayordomo (2005) Table 4.21.

Rake (º): 180 LD Acosta et al. (2013)

Sense of Movement: D D to R LD García-Mayordomo (2005); Acosta et al. (2013); Echeverria et al. (2013) based on GPS data suggests reverse fault kinematics for this fault.

Length (km): 31.6 ± 0.02 LD Compiler's measurement, based on Acosta et al. (2013).

Min Depth (km): 0 LD This is the onshore continuation of Escarpe de Mazarrón offshore structure (García-Mayordomo, 2005, p.169.; Acosta et al., 2013).


Width (km): 8.0 AR

Area (km²): 252.96 AR


Middle Pleistocene

LD Bardají (1999) in García-Mayordomo (2005), p. 169.




0.05 <0.05 m/ka EJ By comparison with other active faults in the area (Table 3.30 y Fig. 3.29 in García-Mayordomo, 2005)


0.05 AR From HSR and rake


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Activity of the fault is related to the uplift of Sierra de las Moreras during Lower and Middle Pleistocene (Bardají, 1999).

Bardají (1999) in García-Mayordomo (2005), p. 169.



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 185

Página 521 de 632




6.87 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.80 (± 0.3) according to García Mayordomo (2005) based on: SRL(31.6 km) vs Mw, from Wells and Coppersmith (1994) and sample "All".




Unknown



Bardají, T. (1999). Evolución geodinámica de las cuencas neógenas del litoral de Murcia y Almería durante el cuaternario. Tesis Doctoral, Universidad Complutense de Madrid, 457 pp.

Comas, M.C., Soto, J.I. y Woodside, J.M. (2000). Structure and related seafloor morphology of the Palomares and Mazarrón margins (Western Mediterranean). En: European Geophysical Society, 25th General Assembly, Katlenburg-Lindau, Germany, abstract.

Coppier, G., Griveaud, P., Larouzière, F. (1989). Example of Neogene tectonic indentation in the Eastern Betic Cordilleras: the Arc of Aguilas (Southeastern Spain). Geodinamica Acta, 3(1), 37-51.

Díaz del Río, V. (1991). El margen continental Bético Mediterráneo. Extremo Bético Oriental. Cuenca de Murcia-Escarpe de Mazarrón. Publicaciones Especiales del Instituto Español de Oceanografía, 6, pp. 239.



Griveaud, P. Coppier, G., Montenat, C. y Ott d’Estevou, Ph. (1990). Le Néogène des Sierras d'Aguilas. En: Montenat, C. (ed.), Les Bassins néogènes du domaine Bétique oriental(Espagne), Documents et Travaux de l’Institut Geologique Albert de Lapparent, 12-13, 221-238.

I.T.G.E. (1990). Mapa Geológico de la Plataforma Continental Española y Zonas Adyacentes a escala 1:200.000. Hoja nº 79-79E, Murcia.






References

Variability



Página 522 de 632




Segment Name: Cabo Tiñoso - West Cabo de Palos

Location X: -1.16977967

Location Y: 37.53185591

Name of Compiler(s): García-Mayordomo, J. and Martín-Banda, R.

Filiation: IGME and Universidad Complutense de Madrid

Email: [email protected]; raq


Average Strike(º): 102 + 20 / - 1 LD Compiler's measurement, based on Acosta et al. (2013) and García-Mayordomo (2005). To apply right hand rule criteria dip is considered towards S.

Dip (º): 90 LD García-Mayordomo (2005) table 4.21.

Rake (º): 180 LD Acosta et al. (2013)

Sense of Movement: D LD García-Mayordomo (2005) and Acosta et al. (2013)

Length (km): 27.0 ± 0.4 LD Compiler's measurement, based on Acosta et al. (2013).

Min Depth (km): 0 LD García-Mayordomo (2005) and Acosta et al. (2013).


Width (km): 8.0 AR

Area (km²): 347.20 AR


Holocene LD Several of the offshore seismic events are associated with the Mazarrón Escarpment indicating that the scarp is tectonically active (Acosta et al., 2013).




0.05 <0.05 m/ky EJ By comparison with other active faults in the area (Table 3.30 y Fig. 3.29 in García-Mayordomo, 2005).




Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Offshore Quaternary marine deposits 2) The mass wasting probably triggered by recent seismic events. These events are scattered throughout the margin.

ITGE (1990), Díaz del Río (1991), García-Mayordomo (2005), p. 169; Acosta et al. (2013).

Geological Set: Betic Range (Murcia offshore)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 186

Página 523 de 632




6.81 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.7 (± 0.3) according to García Mayordomo (2005) based on: SRL(27 km) vs Mw, from Wells and Coppersmith (1994) and sample "All".




Unknown
















References

Variability



Página 524 de 632




Segment Name: East Cabo de Palos

Location X: -0.695

Location Y: 37.505

Name of Compiler(s): García-Mayordomo, J. and Martín-Banda, R.

Filiation: IGME



Average Strike(º): 066 + 2 / - 1 LD Compiler's measurement, based on Acosta et al. (2013). To apply right hand rule criteria dip is considered towards S.

Dip (º): 90 LD García-Mayordomo (2005); Acosta et al. (2013).

Rake (º): 0 Acosta et al. (2013).

Sense of Movement: S LD Acosta et al. (2013).

Length (km): 41.0 10-30 to 45 LD 41 km is the total length of the segment. Note that 23.5 km is the max length of single faults included in the shear zone of the segment (8 km width) (Acosta et al., 2013).

Min Depth (km): 0 LD García-Mayordomo (2005); Acosta et al. (2013).


Width (km): 8.0 AR

Area (km²): 330.40 AR


Holocene LD Several of the offshore seismic events are associated with the Mazarrón Escarpment indicating that the scarp is tectonically active (Acosta et al., 2013).








Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

1) Offshore Quaternary marine deposits 2) The mass wasting probably triggered by recent seismic events. These events are scattered throughout the margin.

ITGE (1990), Díaz del Río (1991), García-Mayordomo (2005), p. 169; Acosta et al. (2013).

Geological Set: Betic Range (Murcia offshore)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 187

Página 525 de 632




6.75 ± 0.37 ER Mw from maximum single fault length (23.5 km) using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.9 (± 0.3) according to García Mayordomo (2005) based on: SRL(41 km) vs Mw from W&C (1994).




Unknown
















References

Variability



Página 526 de 632



ID: ME032 Fault Name: Averroes (also known as Djibouti)

Segment Name:

Location X: -3.363

Location Y: 36.285

Name of Compiler(s): Estrada, F., Vázquez, J.T. and Ercilla, G.

Filiation: ICM (Barcelona); IEO (Málaga)



Average Strike(º): 120 ± 5 LD Measured on multibean bathymetric data (Estrada et al., 1997; Pérez Belzuz, 1999; Estrada et al., 2014; Martínez-García et al., 2011, 2013; Perea et al., 2014).

Dip (º): 23 ± 3 OD Calculated from seismic profiles

Rake (º): 135 EJ Assumed value for a reverse-dextral kinematics.

Sense of Movement: RD LD Estrada et al., 1997; Pérez Belzuz, 1999; Estrada et al., 2014; Martínez-García et al., 2011, 2013; Perea et al., 2014.

Length (km): 44.0 LD Measured on multibeam bathymetric data (Estrada et al., 2014)

Min Depth (km): 0 LD Outcrops at the sea bottom (Estrada et al., 2014)

Max Depth (km): 10.0 EJ It is assumed the same value as in other faults in the area, that is based on the depth distribution of instrumental seismicity from IGN database (cf. Álvarez-Gómez et al., 2010)

Width (km): 25.6 AR

Area (km²): 1126.09 AR


Quaternary OD Probably Holocene, seismics inconclusive


0.040 0.05-0.03 EJ Considering a generic Plio-Quaternary marker (2600 ky) and 140-90 m offset.


1.69 EJ Considering a generic Plio-Quaternary marker (2600 ky) and 4.4 km offset.


1.69 AR From HSR, VSR and dip


Unknown


Unknown


EJ

Identification


Quaternary Activity

Variability Source

Comment

Lateral and vertical displacements, bathymetry and seismic profiles, associated minor scale structures (faults & folds), lateral displacement of volcanic edifice.

Estrada et al., 1997; Pérez Belzuz, 1999; Estrada et al., 2014; Martínez-García et al., 2011, 2013; Perea et al., 2014.

Geological Set: Alboran Sea (Offshore South Granada)


Comment


A+*Strength Class:


Paleoearthquakes

Orden Visual: 276

Página 527 de 632








Unknown


Estrada, F. Ercilla, G., Alonso, B., 1997. Pliocene-Quaternary Tectonic-sedimentary Evolution of the Northeastern Alboran Sea (SW Mediterranean Sea). S. Cloetingh and M. Fernández (Eds.) Origin of Sedimentary Basins., Spc. Vol. Tectonophysics 282, 423-442.

Estrada, J.T. Vázquez, G. Ercilla, B. Alonso, E. d’Acremont, C. Gorini, M. Gómez, M.C. Fernández-Puga, A. Ammar y B. El Moumni, 2014. Recent tectonic inversion of the Central Alboran Zone. IBERFAULT, Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España.


Martínez-García, P., Comas, M., Soto, J.I., Lonergan, L. & Watts, A.B. (2013). Strike-slip tectonics and basin inversion in the WesternMediterranean: the Post-Messinian evolution of the Alboran Sea. Basin Research (2013) 25, 1–27, doi: 10.1111/bre.12005.

Perea, H., E. Gràcia, R. Bartolomé, L. Gómez de la Peña, S. Martínez-Loriente, X Moreno, B. De Mol, Tello, O., Ballesteros, M. and EVENT-DEEP cruise party (2014). Evidences of Quaternary Active Faults Across the Djibouti High and the Adra Ridge (Alboran Sea). IBERFAULT, Resúmenes de la 2ª Reunión Ibérica sobre Fallas Activas y Paleosismología, Lorca, España.

Pérez-Belzuz, F., 1999. Geología del Margen y Cuenca de Mar de Alborán Durante el Plio-Cuaternario: Sedimentación y Tectónica, PhD Thesis, CSIC, Universidad de Barcelona.




References

Variability



Página 528 de 632



ID: PO001 Fault Name: Vidigueira-Moura

Segment Name: Vidigueira-Moura

Location X: -7.386

Location Y: 38.175

Name of Compiler(s): Brum da Silveira, A. and Cabral, J.

Filiation: Lisbon University - FCUL / IDL



Average Strike(º): 275 ± 5 LD Related data also presented in Brum da Silveira, 1990, 2002 and published in Cabral and Ribeiro, 1988, Brum da Silveira et al., 2009

Dip (º): 45 ± 15 LD Related data also presented in Brum da Silveira, 1990, 2002 and published in Brum da Silveira et al., 2009

Rake (º): 135 ± 15 LD Related data also presented in Brum da Silveira, 1990, 2002 and published in Brum da Silveira et al., 2009

Sense of Movement: RD LD Related data also presented in Brum da Silveira, 1990, 2002 and published in Brum da Silveira et al., 2009

Length (km): 39.0 ± 1 LD Related data also presented in Brum da Silveira, 1990, 2002 and published in Brum da Silveira et al., 2009

Min Depth (km): 0 LD Fault outcrops at the surface ( Brum da Silveira et al., 2009).

Max Depth (km): 20.0 ± 5 EJ Related data also presented in Brum da Silveira, 1990, 2002 and published in Brum da Silveira et al., 2009; regional low magnitude seismicity down to ~16 km

Width (km): 28.3 AR Related data also presented in Brum da Silveira, 1990, 2002 and published in Brum da Silveira et al., 2009

Area (km²): 1103.09 AR


84 ky ± 6 ky OD River terrace, preliminary OSL age dating


0.070 0.060 - 0.076 LD Correlation of erosion surface in upper block with unconformity surface at base of alluvial fan in lower block; 150-190m/2.5 Ma; Brum da Silveira et al., 2009


0.095 0.085-0.106 AR From estimated NSR and rake


0.135 0.12-0.15 LD Net-slip on the fault is considered assuming an average dip of the fault surface of 45° N and an average rake of 135º; Brum da Silveira et al., 2009


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Well preserved fault scarp, clear topographic lineament in remote sensing imagery and DEMs

Related data also presented in Brum da Silveira, 1990, 2002 and published in Brum da Silveira et al., 2009

Geological Set: Iberian Massif (Portugal)


Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 289

Página 529 de 632




Unknown


6.96 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.93 using W&C (1994) surface rupture length relationship for "all faults" set, assuming rupture along entire fault length in the maximum earthquake.


6953 28077-1744 AR Considering the MEM (Wesnousky, 1986): slip rate represents the rate at which maximum earthquakes are released by the fault. RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter. Previous estimate was 4450 yrs.


Unknown


Alves, C.O. (1971): A Bacia de Marmelar. Aplicação de métodos sedimentológicos ao estudo da evolução do relevo. Finisterra, 6: 218–245.

Araújo, A., Espinha Marques, J., Brum da Silveira, A., Cabral, J., Ribeiro, A. (1998): Cartografia geológica de pormenor das estruturas frágeis da região de Alqueva. In: Chaminé, H.I., Guerner Dias, A., Ribeiro, M.A., Sodré Borges, F. (Eds.), 4° Conferência Anual GGET'98, Porto, 1998. Geólogos, 2: 141–145.

Brum da Silveira, A. (1990): Neotectónica e Sismotectónica da Região Vidigueira–Moura. MSc Thesis, Univ. Lisboa, 204 pp.

Brum da Silveira, A (2002): Neotectónica e Sismotectónica de um Sector do Alentejo Oriental. PhD Thesis, Univ. Lisboa, 339 pp.

Brum da Silveira, A., Araújo, A. (1989): A Falha do Alqueva: evidências de actividade neotectónica. Encontro sobre Sismologia e Engenharia Sísmica. Comunicações. Sociedade Portuguesa de Engenharia Sísmica, L.N.E.C. Lisboa, 431–440.

Brum da Silveira, A., Cabral, J., Araújo, A., Espinha Marques, J. (1997): Estudo Neotectónico e Sismotectónico da Falha de Alqueva. ICAT, FCUL, Unpublished Report for Empresa de Desenvolvimento e Infraestruturas do Alqueva - EDIA, S. A., Lisboa, 119 pp.

Brum da Silveira, A., Cabral, J., Araújo, A., Espinha Marques, J. (1998): A falha de Alqueva (Alentejo): um exemplo de falha activa normal em regime tectónico compressivo. In: Chaminé, H.I., Guerner Dias, A., Ribeiro, M.A., Sodré Borges, F. (Eds.), 4° Conferência Anual GGET'98, Porto, 1998, Geólogos, 2: 141–145.

Brum da Silveira, A., Cabral, J., Ribeiro, A. (1998): Caracterização sismotectónica da falha activa de Alqueva (Alentejo). Actas do V Congresso Nacional de Geologia 1998, Lisboa. Comunicações 84 (1): D65–D68.

Brum da Silveira, A., Cabral, J., Perea, H., Ribeiro, A. (2009): Evidence for coupled reverse and normal active faulting in W Ibéria. The Vidigueira–Moura and Alqueva faults (SE Portugal). Tectonophysics, 474: 184–199.

Cabral, J. (1995): Neotectónica em Portugal Continental. Memórias do Instituto Geológico e Mineiro, vol. 31, 265 pp.

Cabral, J., Ribeiro, A. (1988): Carta Neotectónica de Portugal Continental, Escala 1:1.000.000. Dep. Geol. Fac. Ciênc. de Lisboa, Serv.Geol. de Portugal, Gab. Prot. Seg. Nuclear. Lisboa, Instituto Geológico e Mineiro, Lisboa.

Carvalho, A.M.G., Alves, C.O. (1970): Nota sobre os depósitos terciários de Moura. Finisterra 5 (10): 282–291.Carvalhosa, A.B., Carvalho, A.M.G. (1970): Carta Geológica de Portugal à escala 1/50000. Notícia explicativa da folha 43-B Moura. Serv. Geol. Portugal, Lisboa.

Feio, M. (1946): Os terraços do Guadiana a jujante do Ardila. Com. Serv. Geol. Portugal, 27: 3–84.

Feio, M. (1949): A Serra de Portel. Bol. Soc. Geol. Portugal, 8: 101–106.

Feio, M. (1951): A evolução do relevo do Baixo Alentejo e Algarve. Com. Serv. Geol. Portugal, 32 (2): 303–504.

Oliveira, J.T., Oliveira, V., Manuppella, G., Zbyszewski, G., Antunes, M.T., Monteiro, J.H. (Coords.) (1988): Carta Geológica de Portugal, escala 1:200.000, Folha 8. Serviços Geológicos de Portugal, Lisboa.

Oliveira, J.T., Pereira, E., Ramalho, M.M., Antunes, M.T., Monteiro, J.H. (Coords.) (1992): Carta Geológica de Portugal, Escala 1:500.000. Serviços Geológicos de Portugal, Lisboa.

Ribeiro, A., Kullberg, M.C., Kullberg, J.C., Manuppella, G., Phipps, S., 1990. A review of Alpine tectonics in Portugal: foreland detachment in basement and cover rocks. Tectonophysics, 184: 357–366.




References

Variability



Página 530 de 632



Ribeiro, A., Cabral, J., Baptista, R., Matias, L., 1996. Stress pattern in Portugal mainland and the adjacent Atlantic region, West Iberia. Tectonics, 15 (2): 641–659.




Página 531 de 632



ID: PO002 Fault Name: Ponsul (complete)

Segment Name: Ponsul



Name of Compiler(s): Dias, R. and Cabral, J.

Filiation: LNEG, Portugal, and Lisbon University - FCUL / IDL



Average Strike(º): 235 + 5 / - 30 LD Fault trace is undulated. In some areas it presents large sinuosities separating NE trending right-hand stepping en-echelon segments. Related data published in Cabral and Ribeiro, 1988, Dias and Cabral, 1989.

Dip (º): 55 + 35 / - 30 LD Very different dips observed at outcrop (from 25ºNW to ~90º), mostly between 35º and 55ºNW. Related data published in Dias and Cabral, 1989.

Rake (º): 100 ± 10 LD Related data published in Dias and Cabral, 1989.

Sense of Movement: R AR Related data published in Dias and Cabral, 1989.

Length (km): 115.0 ± 5 LD Length of the Portuguese sector, comprising 4 segments, is 82km. Fault continues in Spain for more 36km, along a 5th segment (Moraleja segment). Related data published in Dias and Cabral, 1989.

Min Depth (km): 1 ± 1 LD Fault outcrops at the surface

Max Depth (km): 25.0 ± 5 EJ Inferred from maximum depth of (scarce and low magnitude) regional seismicity and rheological models of lithosphere.

Width (km): 29.3 AR

Area (km²): 3369.34 AR


140 ky ± 10 ky OD Estimated correction of OSL age of T4 terrace sediments of the Tagus river (129 +/- 8 ky, in Cunha et al., 2008) (Cunha, personal communication). Deformation inferred from vertical offset of top of T4 from one side of the fault to the other side.


0.020 0.014 - 0.027 EJ Min- 50m displacement of basal surface of sediments of Falagueira Formation (3.6-2.6 Ma); max- 8m displacement of basal surface of T4 terrace of Tagus river (~295 ky, Cunha, pers. Comm.). (See also Dias and Cabral, 1989, 1991, Cunha et al., 2005, 2008)




0.025 0.017 - 0.033 AR Net-slip on the fault assuming average dip of fault surface of 55° N, rake of slip lines of 100º and the above referred vertical slip rates.


Unknown

Identification


Quaternary Activity

Variability Source

Comment


Related data published in Dias and Cabral, 1989, 1991; Cunha et al., 2005, 2008.



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 290

Página 532 de 632




Unknown


Unknown


7.41 ± 0.37 ER Mw from max. Length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 7.47 using W&C'94 from SRL relationship for "all faults" set, assuming rupture along the entire fault (115 km, Mw). (segms. From Dias and Cabral, 1989).


57397 302956-12115 AR Considering the MEM (Wesnousky, 1986): slip rate represents the rate at which maximum earthquakes are released by the fault. RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter. Previous estimate was 63530 yr.


Unknown




Cunha, P.P., Martins, A.A., Daveau, S., Friend, P.F. (2005): Tectonic control of the Tejo river fluvial incision during the late Cenozoic, in Ródão – central Portugal (Atlantic Iberian border). Geomorphology, 64: 271–298.

Cunha, P.P., Martins, A.A., Huot, S., Murray, A., Raposo, L. (2008): Dating the Tejo River lower terraces in the Ródão area (Portugal) to assess the role of tectonics and uplift. Geomorphology, 102: 43–54.Dias, R. P., Cabral, J. (1989): Neogene and Quaternary reactivation of the Ponsul fault in Portugal. Comum. Serv. Geol. Portugal, 75: 3-28.

Dias, R. P., Cabral, J. (1991): Neogene and Quaternary reactivation of the Ponsul river fault (Central Portugal). Publication I.G.N., Série Monografia, 8: 269-282. Madrid.







References

Variability



Página 533 de 632



ID: PO003 Fault Name: Ponsul (1/4)

Segment Name: Arneiro-Coxerro







Average Strike(º): 203 ± 5 LD Related data published in Cabral and Ribeiro, 1988, Dias and Cabral, 1989.

Dip (º): 55 + 35 / - 30 LD Variable dips observed at outcrop along the fault. Values are the same used for the all fault. Related data published in Dias and Cabral, 1989.

Rake (º): 100 ± 10 OD Values are the same used for the all fault. Related data published in Dias and Cabral, 1989.

Sense of Movement: R LD Related data published in Dias and Cabral, 1989.

Length (km): 12.0 ± 1 LD Related data published in Dias and Cabral, 1989.

Min Depth (km): 1 ± 1 LD Fault outcrops at the topographic surface

Max Depth (km): 25.0 ± 5 EJ Values are the same used for the all fault. Inferred from maximum depth of (scarce and low magnitude) regional seismicity and rheological models of lithosphere.

Width (km): 29.3 AR

Area (km²): 351.58 AR


140 ky ± 10 ky OD Estimated correction of OSL age of T4 terrace sediments of the Tagus river (129 +/- 8 ky, in Cunha et al., 2008) (Cunha, personal communication). Deformation inferred from vertical offset of top of T4 from one side of the fault to the other side.


0.020 0.014 - 0.027 EJ Min- 50m displacement of basal surface of sediments of Falagueira Formation (3.6-2.6 Ma); max- 8m displacement of basal surface of T4 terrace of Tagus river (~295 ky, Cunha, pers. Comum). (See also Dias and Cabral, 1989, 1991, Cunha et al., 2005, 2008)




0.025 0.017 - 0.033 EJ Net-slip on the fault assuming average dip of fault surface of 55° N, rake of slip lines of 100º and the above referred vertical slip rates.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


B*Strength Class:


Paleoearthquakes

Orden Visual: 291

Página 534 de 632




Unknown


6.48 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 6.33 using W&C'94 SRL relationship for "all faults" set, assuming rupture along the entire fault segment (12 km, Mw). (segms. From Dias and Cabral, 1989).




Unknown





Cunha, P.P., Martins, A.A., Huot, S., Murray, A., Raposo, L. (2008): Dating the Tejo River lower terraces in the Ródão area (Portugal) to assess the role of tectonics and uplift. Geomorphology, 102: 43–54.

Dias, R. P., Cabral, J. (1989): Neogene and Quaternary reactivation of the Ponsul fault in Portugal. Comum. Serv. Geol. Portugal, 75: 3-28.








References

Variability



Página 535 de 632




Segment Name: Arneiro-Monte dos Inventos












Min Depth (km): 1 ± 1 LD Fault outcrops at the topographic surface.


Width (km): 29.3 AR

Area (km²): 439.48 AR


OD No young deposits (Quaternary) have been found affected by the fault segment.


0.020 0.017-0.027 EJ Values are the same used for the all fault and other segments. Min- 50m displacement of basal surface of sediments of Falagueira Formation (3.6-2.6 Ma); max- 8m displacement of basal surface of T4 terrace of Tagus river (~295 ky).




0.025 0.017-0.033 AR Values are the same used for the all fault and other segments. Net-slip on the fault assuming average dip of fault surface of 55° N, rake of slip lines of 100º and the above referred vertical slip rates.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 292

Página 536 de 632




Unknown






Unknown














References

Variability



Página 537 de 632




Segment Name: Monte dos Inventos - Idanha a Nova














Width (km): 29.3 AR

Area (km²): 966.85 AR




0.020 0.017-0.027 EJ Values are the same used for the all fault and other segments. Min- 50m displacement of basal surface of sediments of Falagueira Formation (3.6-2.6 Ma); max- 8m displacement of basal surface of T4 terrace of Tagus river (~295 ky).




0.025 0.017-0.033 AR Values are the same used for the all fault and other segments. Net-slip on the fault assuming average dip of fault surface of 55° N, rake of slip lines of 100º and the above referred vertical slip rates.


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 293

Página 538 de 632




Unknown






Unknown














References

Variability



Página 539 de 632




Segment Name: Idanha a Nova - Monfortinho - Moraleja








Dip (º): 55 + 35 /- 30 LD Variable dips observed at outcrop along the fault. Values are the same used for the all fault. Related data published in Dias and Cabral, 1989.


Sense of Movement: R AR Related data published in Dias and Cabral, 1989.


Min Depth (km): 1 ± 1 Fault outcrops poorly at the topographic surface; difficult to trace.

Max Depth (km): 25.0 ± 5 Values are the same used for the all fault. Inferred from maximum depth of (scarce and low magnitude) regional seismicity and rheological models of lithosphere.

Width (km): 29.3 AR

Area (km²): 1435.63 AR


Unknown


Unknown


Unknown



Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Poor geomorphic evidence; topographic expression tends to decrease eastwards, often as a faint flexure on the regional planar morphology.

The poor geomorphic expression apparentely indicates a decrease of tectonic activity relatively to the western segments; very faint evidence of Quaternary activity, or even evidence of inactivity. Accordingly, no further parameters will be presented.



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 294

Página 540 de 632




Unknown






Unknown












References

Variability



Página 541 de 632



ID: PO007 Fault Name: Manteigas-Vilariça-Bragança (complete)

Segment Name: Manteigas-Vilariça-Bragança

Location X: -6.717

Location Y: 41.98

Name of Compiler(s): Cabral, J.




Average Strike(º): 200 ± 10 LD Related data presented in Cabral, 1989, 1995, Cabral and Ribeiro, 1988, Ribeiro et al., 1996, Rockwell et al., 2009.s). Fault is relatively sinuous (major bend at Bornes), and presents some step-overs (Vilariça, Longroiva)

Dip (º): 88 + 2 / - 13 LD Related data presented in Cabral, 1989, 1995, Rockwell et al., 2009.

Rake (º): 5 ± 15 LD Related data also presented in Cabral, 1989, 1995, Cabral and Ribeiro, 1988, Rockwell et al., 2009.

Sense of Movement: S LD Related data also presented in Cabral, 1989, 1995, Cabral and Ribeiro, 1988, Ribeiro et al., 1996, Rockwell et al., 2009.

Length (km): 215.0 ± 10 LD Related data also presented in Cabral, 1989, 1995, Cabral and Ribeiro, 1988, Ribeiro et al., 1996, Rockwell et al., 2009.


Max Depth (km): 25.0 ± 5 EJ Inferred from maximum depth of the (low magnitude) regional seismicity and rheological models of lithosphere. Related data in Amaral, 2004.

Width (km): 24.0 AR

Area (km²): 5163.15 AR


11 ky ± 1.8 ky LD OSL age of highest unit displaced in Vale Meão trench (See Manteiga-Vilariça-Bragança segment) (Rockwell et al. 2009)


0.000 EJ VSR=0, assumed pure strike-slip faulting.See Manteiga-Vilariça-Bragança segment.


0.3 +0.2/-0.1 LD Horizontal slip rates from channel offsets in Quaternary sediments (Cabral, 1989, 1995, Rockwell et al., 2009). See Manteiga-Vilariça-Bragança segment.


0.301 +0.201/-0.1 AR From HSR and rake


2.5 ± 0.5 LD Estimated from paleoseismic data (Rockwell et al., 2009)

Identification


Quaternary Activity

Variability Source

Comment

Clear topographic lineament in remote sensing imagery and DEMs in central segment; presents depressed and elevated areas interpreted as strike slip basins and pushups, with well preserved fault scarps; in one sector apparently deflects

Related data also presented in Cabral, 1989, 1995, Cabral and Ribeiro, 1988, Ribeiro et al., 1996, Rockwell et al., 2009.



Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 295

Página 542 de 632




3-4 in 23 ky; 2-3 in

LD Data and interpretation from Rockwell et al., 2009. Events inferred from vertical and horizontal offsets of fluvial and colluvial sediments in trenches, and one offset rill.


Unknown


7.67 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 7.2 (± 0.1) from sediment offsets observed (Rockwell et al., 2009), and from fault segmentation model (fault segment length, SRL), using W&C'94 relationships.


7588 40784-1268 AR Considering the MEM (Wesnousky, 1986): slip rate represents the rate at which maximum earthquakes are released by the fault. RI = Mo f(Mw±d) / Mo f(SR±d). The occurrence of smaller, damaging earthquakes may be much shorter.


8000 ± 3000 LD The most recent surface slip occurred between ~ 4.8 and 11 ky, but is most likely close to the older end of this range, indicating that there is an open interval of ~ 5–11 ka (Rockwell et al., 2009)


Amaral, I.C.F.V. (2004) Monitorização da Actividade Sísmica no Território do Parque Arqueológico do Vale do Côa. Relatório de estágio profissionalizante da licenciatura em Ciências Geofísicas na variante Geofísica Interna. Departamento de Física da Faculdade de Ciências. Universidade de Lisboa, 223pp

Cabral, J. (1989): An example of intraplate neotectonic activity, Vilariça basin, Northeast Portugal. Tectonics, 8 (2). 285-303.

Cabral, J. (1995). Neotectónica em Portugal Continental. Mem. Inst. Geol. E Min., 31, Lisboa, 265 pp.

Cunha, P.P. and Pereira, D.I. (2000). Evolução cenozóica da área de Longroiva-Vilariça (NE Portugal). Ciências da Terra (UNL), 14, 89-198.Cunha, P.P., Pimentel, N. and Pereira, D.I. (2000). A assinatura tectono-sedimentar do auge da compressão bética em Portugal: a descontinuidade sedimentar Valesiano terminal-Turoliano. Ciências da Terra (UNL), 14, 61-72.

De Vicente, G., Vegas, R., Cabral J., Van Wees, J. D., Olaiz, A. (2008) Corredores de desgarre cenozoicos en la Península Ibérica (Cenozoic strike-slip corridors of the Iberian Península). Actas VII Cong. Geol. Esp., Univ. De Las Palmas de Gran Canaria, 14-18 Julio, 2008, Editores: Francisco José Pérez Torrado, María del Carmen Cabrera Santana, Geo-Temas, Vol. 10, 333-336.

Pereira, D.I. (1997). Sedimentologia e estratigrafia do Cenozóico de Tras-os-Montes oriental (NE Portugal). Tese de Doutoramento, Univ. Do Minho, 341 pp.

Marques, F.O., Mateus, A., Tassinari, C. (2002). The Late-Variscan fault network in Central-Northern Portugal. Tectonophysics 359, 255–270.




References

Variability





PO007

Moncorvo 1751-12-19 41.20 -7.00 Intensity 5+/-1 Oliveira, 1986

Spatial correlation Oliveira, C.S. (1986): A Sismicidade Histórica e a Revisa~o do Catálogo Sísmico. Proc. 36/11/7368, I e D, Estruturas, Relatório 99/86 - NDA, LNEC, Lisboa, 192 pp.

614

PO007

Moncorvo 1858-03-19 41.20 -7.00 3 -0/+1 Oliveira, 1986

Spatial correlation Oliveira, C.S. (1986): A Sismicidade Histórica e a Revisa~o do Catálogo Sísmico. Proc. 36/11/7368, I e D, Estruturas, Relatório 99/86 - NDA, LNEC, Lisboa, 192 pp.; various references to strong destruction are not suported.

615

Página 543 de 632



Ribeiro, A. (1974). Contribution à L’étude Tectonique de Tras-os-Montes Oriental. Mem. Serv. Geol. Portugal, 24. Lisboa, 168 pp.

Ribeiro, A., Kullberg, M.C., Kullberg, J.C., Manuppella, G., Phipps, S. (1990). A review of Alpine tectonics in Portugal: Foreland detachment in basement and cover rocks. Tectonophysics, 184, 357-366.


Rockwell, T., Fonseca, J., Madden, C., Dawson, T., Owen, L.A., Vilanova, S., Figueiredo, P. (2009). Paleoseismology of the Vilariça Segment of the Manteigas-Bragança Fault in Northeastern Portugal. Geol. Soc. London, Special Publication, 316, 237-258



Página 544 de 632



ID: PO008 Fault Name: Manteigas-Vilariça-Bragança (1/2)

Segment Name: Bornes – Portelo

Location X: -6.717

Location Y: 41.98





Average Strike(º): 202 ± 5 LD Corresponds to N segment. Mapped trace branched and anastomosed. Related data presented in Cabral, 1989, 1995, Cabral and Ribeiro, 1988, Ribeiro et al., 1996, Rockwell et al., 2009.s).

Dip (º): 88 + 2 / - 13 LD Values are the same used for the all fault. Related data presented in Cabral, 1989, 1995, Rockwell et al., 2009.

Rake (º): 5 ± 15 LD Values are the same used for the all fault. Related data presented in Cabral, 1989, 1995, Rockwell et al., 2009.


Length (km): 57.0 ± 3 LD From Calabor, at the NNE, to Bornes, at the SSW. Related data also presented in Cabral, 1989, 1995, Cabral and Ribeiro, 1988, Ribeiro et al., 1996, Rockwell et al., 2009.


Max Depth (km): 25.0 ± 5 EJ Values are the same used for the all fault. Inferred from maximum depth of the (low magnitude) regional seismicity and rheological models of lithosphere. Related data in Amaral, 2004.

Width (km): 24.0 AR

Area (km²): 1368.83 AR




0.000 EJ VSR=0, assumed pure strike-slip faulting. See Manteiga-Vilariça-Bragança segment.


0.3 +0.2/-0.1 LD Values are the same used for the all fault and the other segments. Horizontal slip rates from channel offsets in Quaternary sediments (Cabral, 1989, 1995, Rockwell et al., 2009). See Manteiga-Vilariça-Bragança segment.


0.301 +0.201/-0.1 AR From HSR and rake. V


2.5 ± 0.5 LD Values are the same used for the all fault and other segments. Estimated from paleoseismic data (Rockwell et al., 2009). See Manteiga-Vilariça-Bragança segment.

Identification


Quaternary Activity

Variability Source

Comment

Segment presents poor geomorphic evidence. Some control on topography; W side is higher (Nogueira and Montesinho ranges).




Comment


C*Strength Class:


Paleoearthquakes

Orden Visual: 296

Página 545 de 632




Unknown


Unknown


7.12 ± 0.37 ER Mw is 7.12 (± 0.1) estimated from fault segmentation model (fault segment length, SRL), using Wells and Coppersmith (1994) relationships.




Unknown




Cabral, J. (1995). Neotectónica em Portugal Continental. Mem. Inst. Geol. e Min., 31, Lisboa, 265 pp.

Cunha, P.P. and Pereira, D.I. (2000). Evolução cenozóica da área de Longroiva-Vilariça (NE Portugal). Ciências da Terra (UNL), 14, 89-198.

Cunha, P.P., Pimentel, N. and Pereira, D.I. (2000). A assinatura tectono-sedimentar do auge da compressão bética em Portugal: a descontinuidade sedimentar Valesiano terminal-Turoliano. Ciências da Terra (UNL), 14, 61-72.

De Vicente, G., Vegas, R., Cabral J., Van Wees, J. D., Olaiz, A. (2008) Corredores de desgarre cenozoicos en la Península Ibérica (Cenozoic strike-slip corridors of the Iberian Península). Actas VII Cong. Geol. Esp., Univ. de Las Palmas de Gran Canaria, 14-18 Julio, 2008, Editores: Francisco José Pérez Torrado, María del Carmen Cabrera Santana, Geo-Temas, Vol. 10, 333-336.

Pereira, D.I. (1997). Sedimentologia e estratigrafia do Cenozóico de Trás-os-Montes oriental (NE Portugal). Tese de Doutoramento, Univ. do Minho, 341 pp.


Ribeiro, A. (1974). Contribution à L’étude Tectonique de Trás-os-Montes Oriental. Mem. Serv. Geol. Portugal, 24. Lisboa, 168 pp.Ribeiro, A., Kullberg, M.C., Kullberg, J.C., Manuppella, G., Phipps, S. (1990). A review of Alpine tectonics in Portugal: Foreland detachment in basement and cover rocks. Tectonophysics, 184, 357-366.









References

Variability



Página 546 de 632



ID: PO009 Fault Name: Manteigas-Vilariça-Bragança (2/2)

Segment Name: Longroiva – Bornes

Location X: -6.932

Location Y: 41.521





Average Strike(º): 197 ± 5 LD Related data presented in Cabral, 1989, 1995, Cabral and Ribeiro, 1988, Ribeiro et al., 1996, Rockwell et al., 2009.s). Fault segment is sinuous with a major bend at Bornes.

Dip (º): 88 + 2 / - 13 LD Values are the same used for the all fault. Related data presented in Cabral, 1989, 1995, Rockwell et al., 2009. Related data also presented in Cabral, 1989, 1995, Rockwell et al., 2009.

Rake (º): 5 ± 15 LD Values are the same used for the all fault. Related data presented in Cabral, 1989, 1995, Rockwell et al., 2009. At N end, probably has higher rake (bounding thrust of Bornes push-up).


Length (km): 67.0 ± 3 LD From Bornes, at the NNE, to Longroiva, at the SSW. Related data also presented in Cabral, 1989, 1995, Cabral and Ribeiro, 1988, Ribeiro et al., 1996, Rockwell et al., 2009.

Min Depth (km): 1 ± 1 LD Fault outcrops at the topographic surface

Max Depth (km): 25.0 ± 5 EJ Values are the same used for the all fault. Inferred from maximum depth of the (low magnitude) regional seismicity and rheological models of lithosphere. Related data in Amaral, 2004.

Width (km): 24.0 AR

Area (km²): 1608.98 AR


11 ky ± 1.8 LD OSL age of highest unit displaced in Vale Meão trench (Vilariça) (Rockwell et al. 2009)




0.3 +0.2/-0.1 LD Horizontal slip rates from channel offsets in Quaternary sediments (Cabral, 1989, 1995, Rockwell et al., 2009)


0.301 +0.201/-0.1 AR From HSR and rake


2.5 ± 0.5 LD Estimated from paleoseismic data (Rockwell et al., 2009)

Identification


Quaternary Activity

Variability Source

Comment

Clear topographic lineament in remote sensing imagery and DEMs in central segment; presents depressed and elevated areas interpreted strike slip basins and a pushup, with well preserved fault scarps; in one sector apparently deflects




Comment


A*Strength Class:


Paleoearthquakes

Orden Visual: 297

Página 547 de 632




3-4 in 23 ky; 2-3 in

LD Data and interpretation from Rockwell et al., 2009. Events inferred from vertical and horizontal offsets of fluvial and colluvial sediments in trenches, and one offset rill.


Unknown


7.18 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 7.2 (± 0.1) from sediment offsets observed (Rockwell et al., 2009), and from fault segmentation model (fault segment length, SRL), using W&C'94 relationships.


6000 ± 1000 LD From paleoseismic data (Rockwell et al., 2009). High likelihood of clustering of events in time, with return period <2ky between three events in the 14.5-11 ky interval. From MME (Wesnousky, 1986) results: 4623 yrs (24848-772).


8000 ± 3000 LD The most recent surface slip occurred between ~ 4.8 and 11 ky, but is most likely close to the older end of this range, indicating that there is an open interval of ~ 5–11 ka (Rockwell et al., 2009)




Cabral, J. (1995). Neotectónica em Portugal Continental. Mem. Inst. Geol. e Min., 31, Lisboa, 265 pp.

Cunha, P.P. and Pereira, D.I. (2000). Evolução cenozóica da área de Longroiva-Vilariça (NE Portugal). Ciências da Terra (UNL), 14, 89-198.

Cunha, P.P., Pimentel, N. and Pereira, D.I. (2000). A assinatura tectono-sedimentar do auge da compressão bética em Portugal: a descontinuidade sedimentar Valesiano terminal-Turoliano. Ciências da Terra (UNL), 14, 61-72.

De Vicente, G., Vegas, R., Cabral J., Van Wees, J. D., Olaiz, A. (2008) Corredores de desgarre cenozoicos en la Península Ibérica (Cenozoic strike-slip corridors of the Iberian Península). Actas VII Cong. Geol. Esp., Univ. de Las Palmas de Gran Canaria, 14-18 Julio, 2008, Editores: Francisco José Pérez Torrado, María del Carmen Cabrera Santana, Geo-Temas, Vol. 10, 333-336.

Pereira, D.I. (1997). Sedimentologia e estratigrafia do Cenozóico de Trás-os-Montes oriental (NE Portugal). Tese de Doutoramento, Univ. do Minho, 341 pp.


Ribeiro, A. (1974). Contribution à L’étude Tectonique de Trás-os-Montes Oriental. Mem. Serv. Geol. Portugal, 24. Lisboa, 168 pp.

Ribeiro, A., Kullberg, M.C., Kullberg, J.C., Manuppella, G., Phipps, S. (1990). A review of Alpine tectonics in Portugal: Foreland detachment in basement and cover rocks. Tectonophysics, 184, 357-366.








References

Variability



Página 548 de 632



ID: PO010 Fault Name: Porto-Tomar

Segment Name:


Location Y: 40.0369

Name of Compiler(s): Cabral J., Besana-Ostman G.M., Nemser E.S. and Martín Banda, R.

Filiation: Lisbon University; ICIST (Portugal); IGME



Average Strike(º): 350 ± 5 OD Martín Banda based on Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Dip (º): 75 ± 15 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Rake (º): 15 ± 15 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Sense of Movement: S AR

Length (km): 130.8 ± 10 LD Martín Banda based on Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Min Depth (km): 1 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Max Depth (km): 17.5 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Width (km): 17.1 AR

Area (km²): 2233.87 AR


Quaternary s.l. EJ Taken for granted, as the fault is included in the Share-Database (2011)






0.21 0.02-0.4 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Compiled information is not yet available. Work in progress (LNEG-Lisbon).

Taken for granted, as the fault is included in the Share-Database (2011)

Geological Set: Orla Ocidental - Iberian Massif (Portugal)

Identification Method: Geological/geomorphological field mapping

Comment


Not rated*Strength Class:


Paleoearthquakes

Orden Visual: 298

Página 549 de 632




7.46 ± 0.37 ER Mw from length using Stirling et al (2002) equation derived from the instrumental dataset. Mw is 7.60 according to Share-Database (2011). Estimations highly speculative as database lacks information on Quaternary evidence (work in progress, LNEG-Lisbon).


Lack of compiled information on Quaternary activity evidence (work in progress, LNEG-Lisbon) prevents from producing any estimation at this moment.


Unknown


SHARE-Database (2011). The European Database of Seismogenic Faults: http://diss.rm.ingv.it/share-edsf/index.html





References

Variability



Página 550 de 632



ID: PO011 Fault Name: Penacova-Régua-Verín fault

Segment Name:

Location X: -8.3327

Location Y: 40.1626





Average Strike(º): 026 ± 10 OD Martín Banda based on Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Dip (º): 83 ± 7 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Rake (º): 85 ± 15 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Sense of Movement: R AR

Length (km): 221.7 ± 10 LD Martín Banda based on Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Min Depth (km): 1 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Max Depth (km): 19.5 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)

Width (km): 18.6 AR

Area (km²): 4132.03 AR








0.275 0.05 - 0.5 EJ Cabral, Besana-Ostman and Nemser (SHARE-Database, 2011)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment





Comment




Paleoearthquakes

Orden Visual: 299

Página 551 de 632








Unknown







References

Variability



Página 552 de 632



ID: PO012 Fault Name: Seia - Lousa Fault

Segment Name:

Location X: -8.3815

Location Y: 40.0057





Average Strike(º): 056 ± 10 OD Martín Banda based on SHARE-Database (2011)

Dip (º): 60 ± 15 EJ SHARE-Database (2011)

Rake (º): 15 ± 15 EJ SHARE-Database (2011)


Length (km): 106.9 ± 5 OD Martín Banda based on SHARE-Database (2011)

Min Depth (km): 1 EJ SHARE-Database (2011)

Max Depth (km): 19.5 EJ SHARE-Database (2011)

Width (km): 21.4 AR

Area (km²): 2284.26 AR








0.14 0.07 - 0.21 EJ Share-Database (2011)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 300

Página 553 de 632








Unknown




Source Comment



References

Variability



Página 554 de 632



ID: PO013 Fault Name: Nazare/Caldas da Rainha - Vimeiro (complete)

Segment Name:

Location X: -9.3656

Location Y: 39.1343








Sense of Movement: SR AR




Width (km): 17.1 AR

Area (km²): 2764.47 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential



Geological Set: Orla Ocidental - Iberian Massif (Portugal)


Comment




Paleoearthquakes

Orden Visual: 301

Página 555 de 632








Unknown




Source Comment



References

Variability



Página 556 de 632



ID: PO014 Fault Name: Ota

Segment Name:

Location X: -8.996

Location Y: 39

Name of Compiler(s): Carvalho J., Nemser E.S. and Martín Banda, R.

Filiation: LNEG; ICIST (Portugal); IGME




Dip (º): 83 ± 8 OD SHARE-Database (2011)

Rake (º): 45 ± 15 OD SHARE-Database (2011)


Length (km): 35.6 ± 3 LD Martín Banda based on SHARE-Database (2011)



Width (km): 17.6 AR

Area (km²): 628.33 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential



Geological Set: Orla Ocidental (Portugal)


Comment




Paleoearthquakes

Orden Visual: 302

Página 557 de 632








Unknown




Source Comment



References

Variability



Página 558 de 632



ID: PO015 Fault Name: Azambuja (complete)

Segment Name:



Name of Compiler(s): Cabral J., Nemser E.S. and Martín Banda, R.











Width (km): 18.6 AR

Area (km²): 524.00 AR








0.06 0.05 -0.07 EJ Share-Database (2011)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 303

Página 559 de 632








Unknown




Source Comment



References

Variability



Página 560 de 632



ID: PO016 Fault Name: Lower Tagus Valley (complete)

Segment Name:

Location X: -9.1097

Location Y: 38.7141

Name of Compiler(s): Besana-Ostman G.M., Nemser E.S. and Martín Banda, R.

Filiation: ICIST (Portugal); IGME

Email: glenda.besana-ostman@ist.







Min Depth (km): 0 OD SHARE-Database (2011)


Width (km): 18.8 AR

Area (km²): 2012.87 AR




0.040 0.02 - 0.06 AR From NSR, dip and rake, assumed pure dip-slip faulting.






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 304

Página 561 de 632








Unknown




Source Comment



References

Variability



Página 562 de 632



ID: PO017 Fault Name: Vila Franca de Xira (complete)

Segment Name:



Name of Compiler(s): Cabral J., Carvalho J., Nemser E.S. and Martín Banda, R.

Filiation: Lisbon University; LNEG; ICIST (Portugal); IGME










Width (km): 18.1 AR

Area (km²): 751.58 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 305

Página 563 de 632








Unknown




Source Comment



References

Variability



Página 564 de 632



ID: PO018 Fault Name: Lower Tagus Valley Fault Zone (complete)

Segment Name:



Name of Compiler(s): Cabral, J., Nemser E.S. and Martín Banda, R.











Width (km): 18.1 AR

Area (km²): 867.39 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 306

Página 565 de 632








Unknown




Source Comment



References

Variability



Página 566 de 632



ID: PO019 Fault Name: Pinhal Novo Fault

Segment Name:

Location X: -8.8787













Width (km): 18.6 AR

Area (km²): 754.53 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 307

Página 567 de 632








Unknown




Source Comment



References

Variability



Página 568 de 632



ID: PO020 Fault Name: Porto Alto

Segment Name:

Location X: -8.55

Location Y: 38.92

Name of Compiler(s): Carvalho J., Nemser E.S. and Martín Banda, R.

Filiation: LNEG; ICIST (Portugal); IGME




Dip (º): 83 ± 8 LD SHARE-Database (2011)

Rake (º): 145 ± 35 LD SHARE-Database (2011)

Sense of Movement: DR AR




Width (km): 12.1 AR

Area (km²): 150.47 AR






0.197 0.123-0.270 AR From NSR and rake.




Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 308

Página 569 de 632








Unknown




Source Comment



References

Variability



Página 570 de 632



ID: PO021 Fault Name: Aljezur-S. Teotónio Fault Sistem (complete)

Segment Name:

Location X: -8.8995


Name of Compiler(s): Dias R.P., Cabral J., Besana-Ostman G.M., Nemser E.S. and Martín Banda, R.

Filiation: LNEG; Lisbon University; ICIST (Portugal); IGME



Average Strike(º): 020 + 1 / - 9 OD Martín Banda based on SHARE-Database (2011)







Width (km): 19.9 AR

Area (km²): 982.85 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential



Geological Set: Orla Algarvía - Iberian Massif (Portugal)


Comment




Paleoearthquakes

Orden Visual: 309

Página 571 de 632








Unknown




Source Comment



References

Variability



Página 572 de 632



ID: PO022 Fault Name: Barao de S. Joao (complete)

Segment Name:

Location X: -8.765

Location Y: 37.1537

Name of Compiler(s): Dias R.P., Cabral J., Nemser E.S. and Martín Banda, R.







Sense of Movement: RD AR




Width (km): 19.9 AR

Area (km²): 272.20 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential



Geological Set: Orla Algarvía (Portugal)


Comment




Paleoearthquakes

Orden Visual: 310

Página 573 de 632








Unknown




Source Comment



References

Variability



Página 574 de 632



ID: PO023 Fault Name: Espiche-Odiáxere (complete)

Segment Name:

Location X: -8.8402

Location Y: 37.0603







Rake (º): -135 ± 15 OD SHARE-Database (2011)

Sense of Movement: DN AR




Width (km): 19.9 AR

Area (km²): 503.93 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 311

Página 575 de 632








Unknown




Source Comment



References

Variability



Página 576 de 632



ID: PO024 Fault Name: Lagos

Segment Name:

Location X: -8.6898

Location Y: 37.0846









Length (km): 7.7 ± 0.5 LD Martín Banda based on SHARE-Database (2011)



Width (km): 7.7 AR







0.052 0.003 - 0.1 AR From NSR and rake




Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 312

Página 577 de 632








Unknown




Source Comment



References

Variability



Página 578 de 632



ID: PO025 Fault Name: Portimao

Segment Name:

Location X: -8.5428

Location Y: 37.1171












Width (km): 11.1 AR

Area (km²): 134.30 AR




0.051 0.003 - 0.099 AR From NSR, dip and rake






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 313

Página 579 de 632








Unknown




Source Comment



References

Variability



Página 580 de 632



ID: PO026 Fault Name: Baleeira

Segment Name:

Location X: -8.2631






Average Strike(º): 302 -13 OD Martín Banda based on SHARE-Database (2011)







Width (km): 19.9 AR

Area (km²): 275.99 AR




0.030 0.02 - 0.04 EJ Assumed pure dip-slip faulting.






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 314

Página 581 de 632








Unknown




Source Comment



References

Variability



Página 582 de 632



ID: PO027 Fault Name: Albufeira

Segment Name:

Location X: -8.2617

Location Y: 37.083












Width (km): 19.6 AR

Area (km²): 246.84 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 315

Página 583 de 632








Unknown




Source Comment



References

Variability



Página 584 de 632



ID: PO028 Fault Name: S. Marcos-Quarteira (complete)

Segment Name:

Location X: -8.4875

Location Y: 37.4625








Sense of Movement: NS AR




Width (km): 20.4 AR

Area (km²): 1123.85 AR






0.036 0.001 - 0.071 AR From NSR and rake




Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 316

Página 585 de 632








Unknown




Source Comment



References

Variability



Página 586 de 632



ID: PO029 Fault Name: Loulé

Segment Name:

Location X: -8.1666

Location Y: 37.1316





Average Strike(º): 089 - 15 / + 1 OD Martín Banda based on SHARE-Database (2011)







Width (km): 19.9 AR

Area (km²): 312.43 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 317

Página 587 de 632








Unknown




Source Comment



References

Variability



Página 588 de 632



ID: PO030 Fault Name: Carcavai (complete)

Segment Name:

Location X: -7.0865

Location Y: 37.058

Name of Compiler(s): Dias R.P., Cabral J., Ressurreição R., Nemser E.S. and Martín Banda R.











Width (km): 19.9 AR

Area (km²): 438.29 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 318

Página 589 de 632








Unknown




Source Comment



References

Variability



Página 590 de 632



ID: PO031 Fault Name: S. Estevao (complete)

Segment Name:


Location Y: 37.0437








Sense of Movement: N AR




Width (km): 19.6 AR

Area (km²): 796.62 AR




0.025 0.02 - 0.03 EJ Assumed pure dip-slip faulting.






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 319

Página 591 de 632








Unknown




Source Comment



References

Variability



Página 592 de 632



ID: PO032 Fault Name: Nazare/Caldas da Rainha - Vimeiro (SW segment)

Segment Name: Caldas De Rainha - Vimeiro

Location X: -9.3656

Location Y: 39.1343












Width (km): 17.1 AR

Area (km²): 1156.51 AR








0.153 0.006-0.3 EJ Share-Database (2011)


Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 320

Página 593 de 632








Unknown




Source Comment



References

Variability



Página 594 de 632



ID: PO033 Fault Name: Azambuja (1/2)

Segment Name: Azambuja NE-Segment

Location X: -8.7846













Width (km): 18.6 AR

Area (km²): 123.64 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 321

Página 595 de 632








Unknown




Source Comment



References

Variability



Página 596 de 632



ID: PO034 Fault Name: Azambuja (2/2)

Segment Name: Azambuja SW-Segment


Location Y: 39.1439












Width (km): 18.6 AR

Area (km²): 400.36 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 322

Página 597 de 632








Unknown




Source Comment



References

Variability



Página 598 de 632



ID: PO035 Fault Name: Lower Tagus Valley (1/2)

Segment Name: Lower Tagus Valley SW segment

Location X: -9.1097

Location Y: 38.7141












Width (km): 18.8 AR

Area (km²): 1149.22 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 323

Página 599 de 632








Unknown




Source Comment



References

Variability



Página 600 de 632



ID: PO036 Fault Name: Lower Tagus Valley (2/2)

Segment Name: Lower Tagus Valley NE segment

Location X: -8.706

Location Y: 39.2173












Width (km): 18.8 AR

Area (km²): 757.05 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 324

Página 601 de 632








Unknown




Source Comment



References

Variability



Página 602 de 632



ID: PO037 Fault Name: Vila Franca da Xira (NE Segment)

Segment Name: NE Segment

Location X: -9.008

Location Y: 38.937

Name of Compiler(s): Cabral J., Carvalho J., Nemser E.S. and Martín Banda, R.

Filiation: Lisbon University; LNEG; ICIST (Portugal); IGME










Width (km): 18.1 AR

Area (km²): 262.28 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 325

Página 603 de 632








Unknown




Source Comment



References

Variability



Página 604 de 632



ID: PO038 Fault Name: Lower Tagus Valley Fault Zone (1/2)

Segment Name: Lower Tagus Valley Fault














Width (km): 18.1 AR

Area (km²): 341.98 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 326

Página 605 de 632








Unknown




Source Comment



References

Variability



Página 606 de 632



ID: PO039 Fault Name: Lower Tagus Valley Fault Zone (2/2)

Segment Name: Entroncamento-Santarem









Rake (º): 90 EJ SHARE-Database (2011)





Width (km): 18.1 AR

Area (km²): 291.51 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 327

Página 607 de 632








Unknown




Source Comment



References

Variability



Página 608 de 632



ID: PO040 Fault Name: Aljezur-S. Teotónio Fault Sistem (1/2)

Segment Name: Aljezur-S. Teotónio Fault Sistem-Sinceira segment

Location X: -8.8995













Width (km): 19.9 AR

Area (km²): 243.79 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 328

Página 609 de 632








Unknown




Source Comment



References

Variability



Página 610 de 632



ID: PO041 Fault Name: Aljezur-S. Teotónio Fault Sistem (2/2)

Segment Name: Aljezur-S. Teotónio Fault Sistem-Baiona segment

Location X: -8.8518






Average Strike(º): 021 +1/-9 OD Martín Banda based on SHARE-Database (2011)







Width (km): 19.9 AR

Area (km²): 739.05 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 329

Página 611 de 632








Unknown




Source Comment



References

Variability



Página 612 de 632



ID: PO042 Fault Name: Barao de S. Joao (1/2)

Segment Name: Barao de S. Joao (NE segment)


Location Y: 37.1537












Width (km): 19.9 AR











Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 330

Página 613 de 632








Unknown




Source Comment



References

Variability



Página 614 de 632



ID: PO043 Fault Name: Barao de S. Joao (2/2)

Segment Name: Barao de S. Joao (SW segment)

Location X: -8.7961

Location Y: 37.1185












Width (km): 19.9 AR

Area (km²): 177.45 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 331

Página 615 de 632








Unknown




Source Comment



References

Variability



Página 616 de 632



ID: PO044 Fault Name: Espiche-Odiáxere (1/2)

Segment Name: Espiche-Odiáxere (SW segment)

Location X: -8.8402

Location Y: 37.0603












Width (km): 19.9 AR

Area (km²): 303.14 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 332

Página 617 de 632








Unknown




Source Comment



References

Variability



Página 618 de 632



ID: PO045 Fault Name: Espiche-Odiáxere (2/2)

Segment Name: Espiche-Odiáxere (NE segment)

Location X: -8.69

Location Y: 37.125












Width (km): 19.9 AR

Area (km²): 200.77 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 333

Página 619 de 632








Unknown




Source Comment



References

Variability



Página 620 de 632



ID: PO046 Fault Name: S. Marcos-Quarteira (1/2)

Segment Name: S. Marcos-Quarteira (NW segment)

Location X: -8.4875

Location Y: 37.4625












Width (km): 20.4 AR

Area (km²): 899.71 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 334

Página 621 de 632








Unknown




Source Comment



References

Variability



Página 622 de 632



ID: PO047 Fault Name: S. Marcos-Quarteira (2/2)

Segment Name: S. Marcos-Quarteira (SE segment)

Location X: -8.2003













Width (km): 20.4 AR

Area (km²): 224.12 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 335

Página 623 de 632








Unknown




Source Comment



References

Variability



Página 624 de 632



ID: PO048 Fault Name: Carcavai (1/2)

Segment Name: Carcavai (SW segment)

Location X: -8.0865

Location Y: 37.0583












Width (km): 19.9 AR

Area (km²): 141.58 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 336

Página 625 de 632








Unknown




Source Comment



References

Variability



Página 626 de 632



ID: PO049 Fault Name: Carcavai (2/2)

Segment Name: Carcavai (NE segment)

Location X: -8.0409

Location Y: 37.1107












Width (km): 19.9 AR

Area (km²): 296.70 AR










Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 337

Página 627 de 632








Unknown




Source Comment



References

Variability



Página 628 de 632



ID: PO050 Fault Name: S. Estevao (1/2)

Segment Name: S. Estevao (SW segment)


Location Y: 37.0437












Width (km): 19.6 AR

Area (km²): 358.04 AR




0.025 0.02-0.03 EJ Assumed pure dip-slip faulting.






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 338

Página 629 de 632








Unknown




Source Comment



References

Variability



Página 630 de 632



ID: PO051 Fault Name: S. Estevao (2/2)

Segment Name: S. Estevao (NE segment)

Location X: -7.6753













Width (km): 19.6 AR

Area (km²): 438.12 AR




0.025 0.02-0.03 EJ Assumed pure dip-slip faulting.






Unknown


Unknown


Unknown

Identification


Quaternary Activity

Variability Source

Comment

Seismic Potential





Comment




Paleoearthquakes

Orden Visual: 339

Página 631 de 632








Unknown



Stirling, M., Rhoades, D. and Berryman K. (2002): Comparison of Earthquake Scaling Relations Derived from Data of the Instrumental and Preinstrumental Era. Bulletin of the Seismological Society of America, 92 (2): 812–830.SHARE-Database (2011). The European Database of Seismogenic Faults: http://diss.rm.ingv.it/share-edsf/index.html


Source Comment



References

Variability



Página 632 de 632

Geometry and Kinematics - IGME

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Transcript of Geometry and Kinematics - IGME