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dc.contributor.advisorBordy, Emese
dc.contributor.advisorMilkov, Alexei
dc.contributor.advisorBarkwith, Duncan
dc.contributor.authorMakhubele, Marvel M.H.
dc.date.accessioned2014-07-23T09:56:45Z
dc.date.available2014-07-23T09:56:45Z
dc.date.issued2014
dc.identifier.urihttp://hdl.handle.net/11394/3497
dc.descriptionMagister Scientiae - MScen_US
dc.description.abstractFollowing successful discovery and production of hydrocarbons, Gabon is one of the key hydrocarbon target countries in Africa. Located in the Lower Congo Basin, the study area is based in Etame Marin Permit (EMP), which is licensed to VAALCO Energy Inc., and has been producing hydrocarbons since 2002. The currently explored and producing reservoirs are in the pre-salt sandstones of the Aptian Gamba Formation, charged with hydrocarbons sourced from the syn-rift lacustrine shale of the pre-Aptian Melania Formation. With the aim of finding potential petroleum plays in the post-salt successions and by using 3D prestack depth migration (PSDM) seismic sections and wireline logs, a detailed study of the post-Aptian stratigraphy and salt tectonics of the EMP was undertaken. Eight distinct reflectors were identified based on gamma ray signatures, stratal terminations and isopach trends. Sediment distribution patterns and the relative sea level history of the succession were determined by applying principles of sequence stratigraphy and salt tectonics. Furthermore, two potential plays have been outlined in the post-salt carbonates of the Albian Madiela Formation as well as in sandstones of the Turonian Azile Formation. These reservoirs might have been charged with hydrocarbons from the pre-salt shale of the Melania Formation and/or potentially also enriched from the Albian and Cenomanian shales. For these post-salt hydrocarbon reservoirs to be charged by the pre-salt source rocks, windows within the extensive evaporitic sealing of the Aptian Ezanga Formation were required. 3D PSDM seismic sections attest that diapirism of the Aptian salt unit generated ample hydrocarbon migration pathways from the pre-salt source rocks to post-salt reservoirs. Five well-developed potential salt windows have been identified, two of which have good probability to have facilitated the upward migration of hydrocarbons, because these salt windows are located up dip of oil producing wells. However, even if hydrocarbons are found in the post-salt reservoirs, similarly to the Yombo Field (located offshore Congo, south of the EMP), these shallow reservoirs in the EMP are likely to produce heavy oils due to biodegradation.en_US
dc.language.isoenen_US
dc.publisherUniversity of Western Capeen_US
dc.subjectHydrocarbonen_US
dc.subjectSalt Tectonicsen_US
dc.subjectProduction of hydrocarbonsen_US
dc.subjectPotential petroleum plays in the post-salten_US
dc.titleThe role of salt tectonics in the hydrocarbon potential of the post-salt deposits (Albian to Recent), offshore Gabonen_US
dc.typeThesisen_US
dc.rights.holderUniversity of Western Capeen_US


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