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- W2372037577 abstract "The activities of hot fluid flow exert a great influence on the tempo-pressure field in a basin and encourage the evolution of organic matter and generation of petroleum. Hot fluid flow , generally, falls into 4 types: mantle fluid, basin fluid, metamorphose fluid and magmatic fluid. The Pearl River Mouth Basin, which is an important oil-bearing basin in the South China Sea, has subjected to the collision of the Indian Plate with the Eurasian Plate and the subduction of the Pacific Plate into the Eurasian. Five important tectonisms and magmatisms cause the sophisticated evolutionary history and high geothermal gradient and heat value for the Pearl River Mouth Basin. Inclusion data shows that the migration of petroleum in the basin initiated from the Late Oligocene to the Early Miocene, up to the Quaternary. Two important migrations at least occurred in the hydrocarbon evolutionary history." @default.
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- W2372037577 date "2005-01-01" @default.
- W2372037577 modified "2023-09-25" @default.
- W2372037577 title "Tectono-magmatism and Hot Fluid Flow in the Pearl River Mouth Basin, South China Sea" @default.
- W2372037577 hasPublicationYear "2005" @default.
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