Internationa Bidding Round Offshore License Contracts
Transcript of Internationa Bidding Round Offshore License Contracts
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INTERNATIONALBIDDING ROUND
TO GRANT
OFFSHORELICENSE CONTRACTS
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IIXV
IX
XXVIII
174
76
39
130
108
12364
126
117
135
131
Z-46
Z-35
Z-45103
Z-36
95
57
Z-52
Z-51
144116
Z-48
114
Z-6
Z-49
58
163
145
161
156
160
129
Z-33
137
105
138
XXVI
133
Z-38
109
1-AB
XXII
XXI
Z-34
Z-1
XIII
107
115
88
XIX
121
8
121
8
X
31-E
8
XXIV
III
8
8
Z-2B
102
67
56
XXIII
67
XXVII
IV
31-B
117
I
XIII
105
XXV
VI
VII
Z-6
V
31-C
100
31-D
XX
XX
Ica
LIMA
Puno
Piura
Tacna
Cusco
Tumbes
Huaráz
Iquitos
Huánuco
Abancay
Moquegua
Huancayo
Chiclayo
Pucallpa
Trujillo
Arequipa
Ayacucho
Moyobamba
Cajamarca
Chachapoyas
Huancavelica
Cerro de Pasco
Pto. Maldonado
Callao
Z-59
Z-60
Z-50
Z-53
Z-54
Z-58
Z-56
Z-55
Z-57
70°
70°
75°
75°
80°
80°
5° 5°
10° 10°
15° 15°
³ ECUADOR COLOMBIA
BRASIL
B OL I V I A
CHILE
T I T I C A C A L A
K E
A T L A N T I C
O C E A N
P A C I F I C O C E A N
PERU
P A C I F I C
O C E A N
0 40 80 120 16020KM
FECHA :OCTUBRE, 2011
Escala 1: 2'000,000
GERENCIA DE EXPLORACION
BANCO DE DATOS
LOTES DE CONTRATOS
Y
POZOS EXPLORATORIOS
PP-001CARTOGRAFIA DIGITAL : PLANO Nº :
MAPA DEL PERU
50,000 m 100500 150 Km
PROYECCION : TRANSVERSAL DE MERCATOR
LA AGENCIA NACIONAL DE LOS HIDROCARBUROS
GRAPHIC SCALE
1:2,000,000
Mayo, 2013
Fuente: Información Cartográfica Instituto Geográfico Nacional del Perú 2009
INTERNATIONAL BIDDING
ROUND TO GRANT OFFSHORE
LICENSE CONTRACTS
LEGEND
PromotionBlocks 2013
Blocksunder contrac
The basins located in the centralpart of the continental shelf and in
the south of the country, are one
of the least explored areas, despite
having geological and geophysical
information of regional nature.
For this reason, has beenprioritized the promotion and
contracting of these areas for
hydrocarbon exploration. For this,has been defined nine blocks in five
offshore basins, to be integrated in
the International Bidding Round.
Geologically blocks are locatedparallel to the shoreline, following
the main trend of offshore basins,
thereby increasing the probability to
define “complete” structures, in the
same direction and with enough area
to conduct the development of a
discovery.
The offshore sedimentary basins, due to their location, are one of the least exploredgeological areas in Peru, although for more than a century were discovered hydrocarbons inthe north coast. Currently, this area has the highest daily and cumulative oil production in Peru.
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LIMA
LIMAPISCO
SALAVERRYTRUJILLO
MOLLENDO
L I S
T
BASINS
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LimaBasinOn the North part of Lima basin, has been set up oneblock for the International Bidding Round to grant Offshore License
Contracts.
Block Z-50 borders to the East with Blocks with current contractsZ-48 and Z-49, to the South borders with Block Z-51, and West with
the Lima basin boundary. This block has a fair amount of 2D seismicdata, but has not identified any exploration prospects yet.
Maturity Model in the Cretaceous:
93-75 Seismic Line located between
the northern part of Pisco basin and
southern of Lima Basin, showing
Cretaceous kitchen.
Unexplored basin, with many geologicalpossibilities. Lack to confirm the Petroleum
System in the basin. It needs more geological and
geophysical studies.
There is recent technical information in Trujillo and Pisco basins, surrounding the area.
It is estimated that Lima basin has the same
Petroleum System than Trujillo basin.
There have been conducted geologicaland geophysical studies by various companies
in the coastal areas of Lima, Pisco and Paracas,
having collected 49 samples for geochemical
analysis. From these analyzes it was concluded
that the Ambo Group of Carboniferous is the
main Source Rock of Pisco and Lima Basins,
being the same source rock of hydrocarbons inCamisea.
Block
Z-50 876,753741 km
2D seismicNone
Area (ha) AvailableinformationIdentified
Prospects/Leads
2D seismic in Block Z-50, Lima basin.
1000 m: Bathymetry
Main factors for block configuration:
1. Basin configuration.
2. Petroleum System “hypothetical” Paleozoic (same OS of the
proposed well in Pisco offshore basin next to drill).
B L O C K
Cretaceous
kitchen
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Lima-PiscoBasinsOn the North part of Pisco basin and south of Lima basin,have been set up 3 new Blocks for the International Bidding Round
to grant Offshore License Contracts.
Main factors for Blocks configuration:
1. Prospects and leads with exploration probabilities.
2. Existence of an Petroleum System “hypothetical” Paleozoic,next to be confirmed with drilling.
Schematic Transversal Section.
West to East Pisco Basin (Hunt Oil, 2002).
B L O C K
Block
Z-53 823,6172,493 km
2D seismic7
Area (ha) AvailableinformationIdentified
Prospects/Leads
Z-54 717,518856 km
2D seismic6
Z-55 651,145515 km
2D seismic
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Block Z-53 is located between the basins Pisco to the South andLima to the North, separated by a structural high intermediate, and
borders to the East by Block Z-33.
Blocks Z-54 and Z-55 in Pisco basin, border to the East withline of 7 miles of artisanal fishing protection and Islands Systems,
Islets and “Puntas Guaneras“. Block Z-54 also partially borders to the
East with the Paracas National Reserve. To the West, the boundary of
the 3 Blocks is approximately Pisco basin boundary.
All of these Blocks have good amount of recently 2D seismicinformation, but no exploratory Wells have been drilled in the
offshore area. The Prospects and leads showed have been defined
from the 2D seismic.
2D seismic, prospects and leads in Block Z-53, Lima-Pisco basins.
1000 m: Bathymetry
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B L O C K B L O C K
Inside Pisco Basin has been identified an activePetroleum System with a Carboniferous Source Rock,
capable to generate hydrocarbons, mainly light oil and
gas-condensate.
In outcrops were observed Excellent ReservoirRocks in Choros Formation of the Tertiary, with
porosity and permeability of 34% and 533 milidarcies,
respectively.
Sandstones with a strong oil smell in ChorosFormation, suggest that hydrocarbon generationcomes from Ambo Group of the Carboniferous.
Dark limestone from Pariatambo Formation of theCretaceous with strong oil smell, could be principal or
secondary Reservoir Rock.
The field geology and seismic interpretation, as
well as drillings made through Oceanographic DrillingProgram (ODP) have identified possible Seal Rocks
present in the basin, which belong to Pisco Formation
of the Upper Miocene, recovering the reservoirs of
Choros Formation.
Tectonic trenches and sub-basins types of “pull-apart” from post-Eocene age, associated with strike-
slip faults and gravitational and rotational movements
were caused by a major extensional event, being this
predominant structural style for hydrocarbon traps
forming. This structural style was recently confirmed
by field geology and a new seismic interpretation at
regional level.
2D seismic, prospects and leads in Block Z-54, Pisco basin.
000 m: Bathymetry
2D seismic, prospects and leads in Block Z-55, Pisco basin.
1000 m: Bathymetry
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The delivery of information does not grant rights
to applicants for the same on the areas related to
such information, for which purpose they must first
participate in the International Bidding Round to grant
Offshore License Contracts, within the time periods and
conditions contained in the terms.
The companies or their duly authorized representatives
must register and confirm their interest.
Oil companies interested in available Areas for
new hydrocarbons exploration and exploitation
contracts in Peruvian basins will find the most
relevant information in digital format and free of
cost.
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TECHNICAL INFORMATION IN OUR
Website
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Salaverry-TrujilloBasinsIn Salaverry-Trujillo basins, have been set up 2 new Blocksfor the International Bidding Round to grant Offshore License
Contracts.
Lobos and Morsa North exploratorywells found significant samples of oil during thedrilling. Also, has been detected and obtained
hydrocarbon samples in natural outcrops on the sea
surface, which have demonstrated the existence of an
active Petroleum System in this basin.
To the north of Trujillo, in Talara basin, the
most important Source Rock is Muerto Formation(Lower Cretaceous). In Trujillo Basin, Lobos 1X
well found a shale powerful section of the Upper
Main factors for Blocks configuration:
1. The West boundary of Trujillo basin.
2. The presence of a “hypothetical” Petroleum System in Trujillobasin.
B L O C K B L O C K
Lote
Z-56 716,2943,305 km
2D seismic6
Area (ha) AvailableinformationIdentified
Prospects/Leads
Z-57 578,8592,051 km
2D seismic4
Blocks Z-56 and Z-57 border to the East mainly with the Blockof the current Z-35 contract; the south part of the Block Z-57 borders
to the East with Block Z-48. Block Z-56 borders to the North with
Blocks Z-46 and Z-35. Both Blocks in the bidding, border to the West
with the border of Trujillo basin, constituted by the edge of the upper
slope of the continental shelf. Blocks Z-56 and Z-57 have a large
database of 2D seismic, and have identified 6 and 4 leads respectively.
2D seismic, prospects and leads in Blocks Z-56 and Z-57, Trujillo basin.
1000 m: Bathymetry
Delfin (OXY) 1
Ballena (OXY) 1
Morsa Norte 1X
2 0 0
2 0 0
5 0 0
5
0 0
1 0 0 0
1 0 0 0
1 5 0 0
1 5 0 0
2 0 0 0
2 0 0 0
2 5 0 0
2 5 0
0
3 5 0 0
4 0 0 0
3 0 0 0
3 0 0 0
1 0 0
DHI 96-57
DHI 96-12
DHI 96-81
Seismic DHI’s?Seismic DHI´s
96-81 seismic lineshowing amplitude anomalies.
96-57 seismic lineshowing amplitude anomalies.
DIRECT HYDROCARBONS INDICATOR DHI: Location map of seismic DHI significant (red spots).
Cretaceous that possibly
reached the level
of maturity in some
depocenters.
RESERVOIRS:Good quality
platform sands and
turbidites from the Middle
and Early Eocene.
SEALS: Shales and siltstones
from the Late Oligocene.
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Main factors for Blocks configuration:
1. Border with protection areas of artisanal and small-scalefishing.
2. Prospective geological trends of the basin.
MollendoBasinIn Mollendo basin has been set up 3 new Blocks for theInternational Bidding Round to grant Offshore License Contracts.
B L O C K
Block
Z-58 699,161430 km
2D seismic3
Area (ha) AvailableinformationIdentified
Prospects/Leads
Z-59 1’040,005454 km
2D seismic2
Z-60 901,863399 km
2D seismic2
These 3 Blocks border to the East with line of 7 miles ofprotection of artisanal fishing, small-scale fishing, and with the
System of Islands, Islets and “Puntas Guaneras”. To the West the
Blocks’ boundary consists of the basin boundary. Also these Blocks
have a fair amount of 2D seismic data, but no exploratory wells have
been drilled yet. From the existing 2D seismic in blocks Z-58, Z-59
and Z-60 have been defined 3, 2 and 2 leads respectively.
Generalized Stratigraphic Column, Adán Pino, 2004.
Geological map
and seismic data
for Block Z-60
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L O T E L O T E
Mollendo basin is a structural depressionbetween the Coast Cordillera and the Peruvian
Trench. Along the shoreline outcrops the
Precambrian Metamorphic Complex, which is
covered by clastic and carbonate sediments of
the Paleozoic, Triassic, Jurassic and Cretaceous,
extending westward into Mollendo basin. Tertiary sequences dominated by deltaic-
fluvial clastic sediments and marine cover the
oldest rocks on a discordance.
Have been found some asphalt layersin Lower and Middle Jurassic formations,
indicating the presence of potential Source
Rocks in this basin completely unexplored,
with many probabilities for hydrocarbon
exploration.
STRUCTURAL STYLE: Extensional tectonics with pillars and Tectonic Trench creation. Half of
the trenches in the depressions are truncated by an erosional surface.
2D seismic, Prospects and Leads in Block Z-58 from Mollendo basin. 2D se ismic, Prospects an d Leads in Block Z-59 from Mollen do basin.
2D seismic, Prospects and Leads in Block Z-60 from Mollendo basin.
1000 m: Bathymetry 1000 m: Bathymetry
1000 m: Bathymetry
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PERUPETRO S.A.Luis Aldana 320, San Borja
Lima 41 - Perú T. (051-1) 206-1800