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• W2133349623 abstract "Recent oolites from the Bahama Banks are shown to contain 1.23–4.13 wt% organic carbon of algal origin, chiefly in the form of proto-kerogen. Characterization of the ogranic matter by routine optical and chemical means revealed that, although it is immature, it has a very high potential for generating petroleum hydrocarbons. It is suggested that with rise in temperature due to burial, and perhaps to catalytic influence of the host sediments, this proto-kerogen of algal-amorphous facies would, through time, generate significant amounts of hydrocarbons. In those oolite deposits with adequate porosity, the hydrocarbons could accumulate as petroleum." @default.
• W2133349623 created "2016-06-24" @default.
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• W2133349623 date "1982-01-01" @default.
• W2133349623 modified "2023-09-23" @default.
• W2133349623 title "SOME ASPECTS OF THE OCCURRENCE OF PROTO-KEROGEN IN RECENT OOIDS" @default.
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• W2133349623 doi "https://doi.org/10.1111/j.1747-5457.1982.tb00539.x" @default.
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