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- W2382457012 abstract "Dongpu depression lies in the southwest of Bohaiwang Basin,and is a tensional pull fault basin developed in Paleogene.While Baimiao structure is located in the southern part of the sag,and it has an absolute response of the overpressure.In the Baimiao area the overpressure mechanism was studied by every aspect of possibility,such as the compaction disequilibrium and hydrocarbon generation.The result indicates that the Paleogene formation of Baimiao area shows a compaction disequilibrium situation where mudstone acoustictime curve present a two parts linear evolvement,with the inflexion depth about 3 100 m. Meanwhile,the measured top depth of overpressure is 2 800-3 050 m.This verifies that the compaction disequilibrium causes the overpressure in the area.On the other hand,there is a good coherence between the top depth of the overpressure and the hydrocarbon generation fastigium,and the Ro is 1.0% at the depth of 3 050 m,which verifies the contribution of the hydrocarbon generation to the overpressure development.Therefore,it can be concluded that hydrocarbon generation and the compaction disequilibrium are the main mechanism of the overpressure development." @default.
- W2382457012 created "2016-06-24" @default.
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- W2382457012 date "2007-01-01" @default.
- W2382457012 modified "2023-09-22" @default.
- W2382457012 title "Eogene Overpressure Mechanism in Baimiao Area of Dongpu Depression" @default.
- W2382457012 hasPublicationYear "2007" @default.
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