Marine and Petroleum Geology 04 "0887# 274Ð390 Depositional environments and oil potential of Jurassic:Cretaceous source rocks within the Seychelles microcontinent Phillip S[ Plummer\ Patrick R[ Joseph\ Patrick J[ Samson Seychelles National pany\ PO Box 129\ Victoria\ Mahe\ Seychelles Received 3 December 0886^ 09 March 0887^ 29 March 0887 Abstract The Seychelles microcontinent became isolated between the Somali\ Mascarene and Arabian basins of the Indian Ocean as a result of the Mesozoic fragmentation of Gondwana[ Major rifting events occurred during the Triassic!Middle Jurassic and Late Cretaceous "Cenomanian!Santonian and Maastrichtian# during which shaly source rock facies accumulated in principally marginal marine:deltaic environments[ Between these times\ post!rift passive margin deposition within restricted to open marine environments produced shaly source rocks during late Middle Jurassic!Early Cretaceous\ Campanian!Maastrichtian and Paleocene times[ Recent geochemical analysis of cuttings from the Seagull Shoals!l well has identi_ed an oil!prone liptinitic "Type II# coaly shale within early Middle Jurassic abandoned deltaic deposits[ This coaly source rock is regionally developed\ having also been identi_ed in the Majunga and Morondava basins of Madagascar[ Oil!prone Type anic matter has also been identi_ed in the Owen Bank A!0 well within restricted marine shales of late Middle Jurassic age[ These shales are part of a thick post!rift source rock sequence that extends into the Early Cretaeous and is in part correlative with the proven Late Jurassic Uarandab Shale of Somalia[ Analysis of Campanian marine shales from Reith Bank!0 well identi_ed signi_cant dilution of anic carbon content posite\ compared to picked\ well cuttings samples[ This _nding supports a published inference that these post!rift shales have source rock potential[ The very limited drilling of the various Jurassic:Cretaceous source rock sequences in Seychelles "onl