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- W1990969319 abstract "Geochemical modelling in rapidly subsiding basins presents some puzzling questions. In trying to clarify them, two African basins related to different domains were studied. The high Tertiary and Quaternary sedimentation rate is a common feature of the two basins. In each of them present heat flow values were computed in different wells on the basis of temperature, stratigraphic and petrophysical data using a one dimensional finite element mathematical model. The resulting distributions show in some cases irregular patterns, which are examined in detail to outline their possible causes. Extrapolation of the present thermal regime to the past generally gives computed maturity values considerably higher than those obtained experimentally. The experimental data include vitrinite reflectance values, Rock-Eval pyrolysis results, sterane and hopane isomerization and sterane aromatization. Hypotheses about thermal history are made in order to explain the areal maturity distribution. They are checked comparing computed maturity values and experimental ones. By combining experimental data and results of the modelling exercise we conclude that the high sedimentation rate, independent of the tectonic domain in which it occurs, can induce noticeable and peculiar thermal anomalies." @default.
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- W1990969319 date "1988-01-01" @default.
- W1990969319 modified "2023-10-18" @default.
- W1990969319 title "Geochemical modelling in rapidly subsiding basins" @default.
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- W1990969319 doi "https://doi.org/10.1016/0146-6380(88)90038-1" @default.
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