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- W117803764 abstract "The sedimentary sequence capping the vast Seychelles bank reaches 6--8 km in thickness and contains a variety of play styles suitable for the entrapment of hydrocarbons. While this sequence extends well beyond the 200 m isobath of the bank, forming a microcontinent, amid this submarine plateau inliers of granitic basement emerge above the Indian Ocean to form the core islands of the Seychelles archipelago. The plateau's origin relates to the breakup of Gondwana. Its known history, extending back to the Middle Triassic, involves three phases of rift tectonics. It is also postulated that deposits of possible Permo-Carboniferous age lie in grabens that are as yet unpenetrated by the drill. The paper discusses the tectono-stratigraphic framework, the possibility of failed rift deposition, initial rift-drift sequence, further rifting and drifting, final rift-drift sequence, a brief exploration history, hydrocarbon play models (block faulted rift play, clastic pinchout play, wrench fault play, carbonate reef and onlap/drape plays), and source rock maturity." @default.
- W117803764 created "2016-06-24" @default.
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- W117803764 date "1993-12-27" @default.
- W117803764 modified "2023-09-26" @default.
- W117803764 title "Diversity of plays bodes well for promising search off Seychelles" @default.
- W117803764 hasPublicationYear "1993" @default.
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