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SAN PEDRO MARGIN

Petroleum Systems

Reservoir: Reservoirs are found in Cretaceous, consisting of turbidites and basin floor fans sandstones encountered with several types of geometries.

Source Rock: Mature source rocks are Albian and Cenomanian ages coming from deep offshore. They reached the oil window in the Early Tertiary.

Trap: Trapping mechanisms are both stratigraphic and structural. They are respectively characterized by channelized submarine fan systems and structural closures. Hydrocarbons migrate through fault systems vertically and/or laterally.

Seal: Cretaceous to Tertiary shales provide good top and lateral sealing capacity over the area.

AREA BLOCKS SIZE SEISMIC DATA GEOLOGY DATA
2D (km) 3D (Sq.km) WELLS LEADS/PLAYS
SAN PEDRO MARGIN

CI-513

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1443 894 1443
  • Ayame-1X
  • Albian structural closures
  • Cenomanian - Lower Senonian fan-shaped prospective sand bodies

CI-700

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3134 980 1123 -
  • Albian structural closures
  • Cenomanian to Lower Senonian stratographic trapping updip slopes

CI-701

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3049 1620 2015 -
  • Albian structural closures
  • Cenomanian to Lower Senonian stratographic trapping updip slopes
  • Stacked basinal channel-levee system

CI-702

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3344 2069 1983
  • San Pedro-1X
  • Aigle-1X
  • Albian structural closures
  • Good sandstone reservoirs in teh Turonian and Albian

CI-703

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2323 1445 505 -
  • Albian structural closures
  • Cenomanian - Santonian fairways

CI-704

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1962 1297 950
  • Saumon-1X
  • Albian structural closures
  • Reservoirs from Albian to Campanian

CI-705

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2289 2214 1686
  • K1-1X
  • K1-2X
  • Barracuda-1X
  • Albian structural closures

CI-706

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911 1089 910
  • South Grand Lahou-1X
  • East Grand Lahou-1X
  • Kosrou-1X
  • Albian structural closures
  • Cenomanian turbidites, slopes fans and basin floor fans

CI-707

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980 151 792
  • Rubis-1X
  • Morue-1X
  • Saphir-1X: oil-sampled (Turonian & Cenomanian)
  • Good source rocks quality in Albian and Cenomian intervals

CI-708

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1446 644 1446 -
  • Best source rocks in Albian to Cenomanian sediments
  • Organic matter is dominated by Type II kerogen oil-prone and petroleum potential is fair to good

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COTE D’IVOIRE Sedimentary Basin
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