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- W2387259641 abstract "The western Taiwan Basin is one of the NE-trending faulted/downwarped basins caused by the Cenozoic continental margin extension in offshore southeastern China. Three source rock sequences have been recognized from shallow to deep in this basin, including the Oligocene-Miocene marine mudstone and coal-bearing formations of transitional facies, the Paleocene-Eocene sand shale of shallow marine-bathyal facies, and the Cretaceous marine mudstone and coal-bearing formations of transitional facies. Source rock analysis shows that they are gas source rocks of high quality and have entered into gas window. These source rock intervals together with the overlying reservoirs and seals form favorable source-reservoir-cap rock combinations, providing good conditions for gas reservoiring. The Nanri and Penghu depressions in the western waters are studied in detail. The Cretaceous and Paleocene-Eocene source rocks are the major source rocks of these two depressions and peak gas generation begins at the burial depth near 2800 m. Study of the gas generation and petroleum systems indicates that these two depressions have good gas reservoiring conditions and are very important prospects for gas exploration in the western Taiwan Basin. The deep structural location of Nanri deression may have favorable conditions for accumulation of source-contacting gas." @default.
- W2387259641 created "2016-06-24" @default.
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- W2387259641 date "2007-01-01" @default.
- W2387259641 modified "2023-10-02" @default.
- W2387259641 title "SOURCE ROCK CHARACTERISTICS AND GAS RESERVOIRING CONDITIONS IN WEST TAIWAN BASIN" @default.
- W2387259641 hasPublicationYear "2007" @default.
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