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- W2371304351 abstract "The source rocks in Qimugen-Sangzhuhe area of southwestern Tarim depression include Ordovician, Carboniferous-Lower Permian, Jurassic and Upper Cretaceous-Paleogene ones. The seismic data show that the Cambrian-Ordovician source rocks have a great thickness of 2 000 m at the footwall of the fault No. 20. The Carboniferous-Lower Permian source rocks are high to very high in maturity, with a wide distribution, great thickness, high content of organic material and better variety. They are at mature to highly mature stage in Kekeya and Pusha-Keliyang areas, as practical hydrocarbon source rocks. The Upper Cretaceous-Paleogene source rocks are at mature stage as good hydrocarbon source rocks, but with low potential of generating oil. Kashi depression is inferred as a place with great potential of oil generation." @default.
- W2371304351 created "2016-06-24" @default.
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- W2371304351 date "2002-01-01" @default.
- W2371304351 modified "2023-09-23" @default.
- W2371304351 title "CHARACTERISTICS OF HYDROCARBON SOURCE ROCKS IN QIMUGEN-SANGZHUHE AREA" @default.
- W2371304351 hasPublicationYear "2002" @default.
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