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- W2097523643 abstract "Abstract Carbonate cements in Tertiary reservoir sandstones from the northern North Sea have distinctive carbon isotopic compositions (δ 13 C). Oil migration up faults from deeper structures and biodegradation of oil pools are factors of particular importance in influencing the δ 13 C of carbonate cements in these sandstones. As a result, δ 13 C can be used as an exploration guide to locating the positions of vertical leakoff points from the Jurassic source rocks. The histogram distribution of δ 13 C in these carbonate cements is trimodal, with peaks at around −26, −3 and +12‰ (ranges −22 to −30, +2 to −10 and +8 to +18‰, respectively). Bacterial processes played major roles in determining this distribution, with oxidative biodegradation of oil resulting in carbonate cements with very negative compositions and bacterial fermentation resulting in the positive δ 13 C cements. δ 13 C distribution patterns may be used to differentiate Tertiary reservoir sandstones from Jurassic in the northern North Sea, and these regional carbonate cement δ 13 C datasets allow geologically useful inferences to be drawn from δ 13 C data from new sample locations." @default.
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- W2097523643 date "2000-03-01" @default.
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- W2097523643 title "Oil migration makes the difference: regional distribution of carbonate cement δ<sup>13</sup>C in northern North Sea Tertiary sandstones" @default.
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- W2097523643 doi "https://doi.org/10.1180/000985500546738" @default.
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