georefid:2002-034977SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2002-0349772001-01-01publicationgeorefid:2002-034977Cole, Gary A.BHP Petroleum, Houston, TX, United StatesauthorFarrer, BruceTDI-Brooks International, United StatesauthorYu, AlanauthorBrooks, JimauthorBernard, BernieauthorAmerican Association of Petroleum Geologists and Society of Economic Paleontologists and Mineralogists (AAPG), Tulsa, OK, United StatespublisherdocumentHardcopyIn: Anonymous, American Association of Petroleum Geologists 2001 annual meeting200139Large volumes of petroleum have been discovered in the deepwater offshore Lower Congo basin of Angola, but the deepwater Kwanza basin to the south remains unexplored. Since no wells have been drilled, the exploration risks remain relatively high for source presence, maturity, and charging (migration of hydrocarbons) of potential structures and traps. This paper will address how those risks were evaluated using seepage, surface heat flow probes, and 2D fluid flow modeling. Evidence for an actively working petroleum system are several macroseeps above shallow salt piercement structures that have been typed to a marine marl source origin. From wells on the shelf and from DSDP364 the most likely source interval is the basal Albian marls, but there may be potential marine source rocks within the pre-salt sag sequence. DSDP364 data suggests a source interval of 100+ meters thickness with excellent oil-prone source quality. Data from the sag sequence suggests a thinner source thickness (40-75 m), but with excellent oil-prone character. The Albian marls are expulsion mature in the deep sediment troughs, though volumes expelled are a critical risk. Constraining the heat flows, hence maturity, is a critical factor in the deepwater Kwanza. Heat flow probes suggest similar to slightly higher heat flows than shelf wells. The sag sequence can contribute hydrocarbon volumes through the salt withdrawal windows, thereby lowering charge risks. 2D fluid flow models showed that the main structures could be charged using the heat flow probe data from the deepwater region.completedEconomic geology, geology of energy sourcesAfricaAlbianAngolaAtlantic OceanCentral Africaclastic rocksCongo BasinCretaceousCuanza BasinDeep Sea Drilling Projectdeep-water environmentdrillingDSDP Site 364East Atlanticheat flowLeg 40Lower CretaceousmarlmaturityMesozoicmigrationoffshoreoil seepsoil wellspetroleumpetroleum explorationsalt tectonicssedimentary rockssource rocksstructural trapstectonicstrapstwo-dimensional modelsurn:org.iodp:exp:40urnlargerWorkCitationcampaignurn:org.iodp:exp:40:site:364urnlargerWorkCitationstudyurn:org.iodp:exp:40urnlargerWorkCitationcampaignEnglishgeoscientificInformation-80.000023.0000-60.000075.0000AngolaAtlantic Ocean