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- W2361974914 abstract "The vitrinite reflectance (R_o) and apatite fission track (AFT) data are used to regress for the geothermal gradient of Gaoyou Sag in Subei Basin. The result shows that average geothermal gradient of this area is 40.8~41.3℃/km, which is higher than that of nowadays. The forward simulation of geothermal history is made by apatite fission track dynamic model. Study shows that average geothermal gradient is about 41.0℃/km during K_2t (83Ma)-E_2s_2 (42Ma), then it decreases gradually with the tectonic subsidence halt, and approximate to 29.0℃/km during Ny (24.6Ma) of nowadays (0 Ma). The simulation result provides a foundation for studying the hydrocarbon accumulation, expulsion and accumulation history." @default.
- W2361974914 created "2016-06-24" @default.
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- W2361974914 date "2005-01-01" @default.
- W2361974914 modified "2023-09-23" @default.
- W2361974914 title "Study on Geothermal Evolution History of Gaoyou Sag in Subei Basin" @default.
- W2361974914 hasPublicationYear "2005" @default.
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