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ABIDJAN MARGIN

Petroleum Systems

Reservoir: Reservoirs age ranges from Albian to Maastrichtian. Sands were deposited in a various of depositional environments from fluvial, alluvial fans, deltafan deposits to lacustrine, marginal marine and deltaic sandstones.

Source Rock: Proven source rock intervals have been identified both in the upper Albian and the Cenomanian.

Trap: Trapping mechanisms are both stratigraphic and structural. The structural traps are primarily fault-related. The structural trend is dominated by NE-SW or E-W normal faults. Structures were formed early before hydrocarbon migration.

Seal: Proven interbedded Lower Cretaceous claystones and shales act both as up-dip seal and lateral seal across fault closure.

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

CI-500

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161 125 114
  • Simba
  • Clastic reservoirs are present in sediments of Albian to Maastrichtian age in this block
  • The identified plays are primarily in Cretaceous and Early Tetriary sediments. Structural and stratigraphic prospects in the Albian and post Albian

CI-503

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325 300 242
  • Ivco-16
  • Both structural and stratigraphic traps. Thestructural traps are primarily fault related
  • The area is dominated by NE-SW or E-W trending normal faults

CI-504

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398 428 398
  • Zaizou1X
  • The idntified plays are upper Turonian mainly stratigraphic and faulted

CI-526

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2979 1409 2979 -
  • Sand-rich reservois intervals have been identified in Albian, Cenomanian and Turonian sections
  • Thick sandstone reservoirs with interbedded claystones are expected

CI-710

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1339 1298 1339
  • Ivoire-1X: oil sampled
  • The main reservoirs are Turonian and Lower Senonian turbiditic and basin floor fan sandstones
  • Ivoire-1X well has encountered oil in the Turonian and Cenomanian good reservoirs quality

CI-804

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980 151 792
  • Ivco-3
  • Ivco-17
  • The block has sgnificant oil and gas shows and successfully flow tested in Upper Creataceous reservoir sandstones predominantly in channelized facies

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