How is the petrography affected by shear zones in the Kohistan complex? Gerold Zeilinger, Laurent...
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Transcript of How is the petrography affected by shear zones in the Kohistan complex? Gerold Zeilinger, Laurent...
How is the petrography affected by shear zones in the Kohistan complex?
Gerold Zeilinger, Laurent Arbaret,
Jean-Pierre Burg, Nawaz Chaudhry,
Hamid Dawood & Shahid Hussain
Preliminary report
• Petrological analysis of shear zones to document the
dynamics of intra arc deformation in the bottom parts
of the Kohistan Complex
– Granulitic gabbro (upper level of Jijal-Complex)
– Sarangar gabbro (lower level of Kamila shear zone)
Overview
Samples
• Granulitic gabbro (13/01/01)– Plagioclase, clinopyroxene, garnet, amphibole, quartz and
rutile. • mylonitic zone:
– Decrease in amount of pyroxene and increase of amphibole and quartz. Garnet is porphyroclastic in the very fine grained matrix (~0.3mm), partly rotated and fractured with new grown amphibole inside these fractures.
• undeformed part:– Granoblastic texture. Pyroxene is hypidioblastic with lobate to symplectitic
contacts with plagioclase. Garnets are poikiloblastic, intergrown with plagioclase, quartz and amphibole.
Samples
• Sarangar gabbro (16/01/01)– Amphibole, clino- and orthopyroxene, plagioclase, garnet,
epidote, ilmenite and quartz. • mylonitic zone:
– Amphiboles underline the fabric in the shear zone and are cut by small quartz veins. Poikiloblastic garnet occurs infrequently. Porphyroclasts (~2 mm) are plagioclase and quartz.
• undeformed part:– Orthopyroxene is idioblastic close to the mylonitic zone whereas farther
away it rims the clinopyroxene. This rim shows symplectitic intergrowth with a second rim comprised of greenish hornblende.
Method
• Electron Microprobe analysis– Cameca SX50 (University of Bern)
• Geobarometry with Al (tot) in hornblende– Hollister et al. 1987– Hammarstrom and Zen 1986– Schmidt 1992
• Geothermometry – hornblende - plagioclase
– Holland and Blundy 1994
– garnet - clinopyroxene– P: Eckert et al. 1991, Perkins et al. 1981– T: Krogh 1988, Ellis and Green 1979, Pattison and Newton 1989
100
90
80
70
60
50
40
30
20
10
100
90
80
70
60
50
40
30
20
10
100 90 80 70 60 50 40 30 20 10
Orthoclase
Plagioclase
Albite AnorthiteOligoclase Andesine Labradorite Bytownite
CaAl2Si2O8NaAlSi3O8
KAlSi3O8
LegendGranulitic gabbro undeformedGranulitic gabbro mylonitic zoneSarangar gabbro undeformedSarangar gabbro mylonitic zone
60
50
40
30
20
10
100
90
80
70
60
50
40
100 90 80 70 60 50 40 30 20 10
Clinoenstatite Clinoferrosilite
Diopside Hedenbergite
Pigeonite
Augite
Fe2Si2O6(Fs)Mg2Si2O6(En)
Ca2Si2O6(Wo)Clinopyroxene
Enstatite Ferrosilite
20
10
100
90
80
100 90 80 70 60 50 40 30 20 10
Ca2Si2O6(Wo)
Fe2Si2O6(Fs)Mg2Si2O6(En)
Ortho-pyroxene
LegendGranulitic gabbro undeformedGranulitic gabbro mylonitic zone
Sarangar gabbro undeformedSarangar gabbro mylonitic zone
Amphibole
5.56.06.57.07.58.0
0.0
0.5
1.0
Edenite Paragasite
Tremolite Hornblende Tschermakite
Ed Pa
Si
Hb Ts
Si Si Si Si Si
(Na
+ K
) A
LegendGranulitic gabbro undeformedGranulitic gabbro mylonitic zone
Sarangar gabbro undeformedSarangar gabbro mylonitic zone
100
90
80
70
60
50
40
30
20
10
100
90
80
70
60
50
40
30
20
10
100 90 80 70 60 50 40 30 20 10
Almandine + Spessartine
Grossular + Andradite Pyrope
Garnet LegendGranulitic gabbro undeformedGranulitic gabbro mylonitic zone
Sarangar gabbro undeformedSarangar gabbro mylonitic zone
1
2
2
3
4
1 eclogites2 granulites3 amphibolites4 epidote amphiboles(after Dobretsov et al., 1972)
Results• Plagioclase
– Andesine in both mylonitic zones
– Labradorite in the Sarangar gabbro
– Oligoclase to Andesine in the Granulitic gabbro
• Pyroxene
– Diopside in the Granulitic gabbro
– Enstatite - Ferrosilite in the Sarangar gabbro
Results• Amphibole
– Granulitic gabbro: Hornblende (undef. zone) to Tschermakite/Paragasite (myl. zone)
– Sarangar gabbro: Hornblende to Tschermakite (undef. zone) and Tschermakite (myl. zone)
• Garnet
– Almandine-Pyrope in Granulitic gabbro
– Almandine rich garnet in mylonitic zone and Grossular in Sarangar gabbro
0.50 1.00 1.50 2.00 2.50 3.00 3.500.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
P in
kba
r
Schmidt. 1992 (± 0.6 kbar)
Hollister. 1987 (± 1.0 kbar)
Hammarston et Zen. 1986 (± 3.0 kbar)
P in
GP
amylonitic zone
0.50 1.00 1.50 2.00 2.50 3.00 3.50Al (tot) in hornblende
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
gt-cpx barometer
undeformed partGranulitic gabbro
Al (tot) in hornblende
0.50 1.00 1.50 2.00 2.50 3.00 3.50Al (tot) in hornblende
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
P in
kba
r
Schmidt. 1992 (± 0.6 kbar)
Hollister. 1987 (± 1.0 kbar)
Hammarston et Zen. 1986 (± 3.0 kbar)
P in
GP
amylonitic zone undeformed partSarangar gabbro
0.50 1.00 1.50 2.00 2.50 3.00 3.50Al (tot) in hornblende
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
Results
• Hornblende - plagioclase thermometer:
– Granulitic gabbro mylonitic zone 700 - 750 °C
– Sarangar gabbro mylonitic zone 740 - 770 °C
– Sarangar gabbro undeformed part 750 - 850 °C
• Garnet - clinopyroxene barothermometer:
– Granulitic gabbro undeformed part 1.2 - 1.55 GPa, 750-930 °C
Results
• Al (tot) - hornblende barometer:
– Granulitic gabbro mylonitic zone 0.9 - 1.2 GPa
– Granulitic gabbro undeformed part ? 1.25 - 1.4 GPa (~0.6 , ~0.3)
– Sarangar gabbro mylonitic zone 1.05 - 1.25 GPa
– Sarangar gabbro undeformed part 1.2 -1.6 GPa (~0.9 , ~0.2)
Interpretation
• Shearing under lower amphibolite facies in both,
the Granulitic and Sarangar gabbro.
Temperature in °C
LegendGranulitic gabbroundeformedmylonitic
Granulitic gabbroundeformedmylonitic
Granulit
e
BS
GS
EAA
PP
Eclogite
And
Gar
net i
n
Alb
ite
Jade
ite Q
uart
z
Sil
Ky
Sil
300 400 500 600 700 800 900 1000 1100 12000.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
1.8
2.0
solid
us
P in
GP
a
Acknowledgements:
• Supported by the Swiss National Science Foundation (grant 20-49372.96)
• Special thanks to Dr. Edwin Gnos (University of Bern) for his support during microprobe analysis and Prof. Jacques Martignole for helpful comments