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- W2369944105 abstract "The Liupanshan Basin.which was mainly formed during the Cretaceous.is located in the southeastern tip of the Hexi Corridor and on the west of the Ordos Basin.Due to the basin's tectonism and evolution,two sedimentary filling cycles were developed in the Cretaceous section of the Liupanshan Basin,resulting in a fan deltaic-lacustrine sedimentary system and a braided stream deltaic-lacustrine sedimentary system,which consist of a number of source-reservoir-seal associations.Of them,the Lower Cretaceous Liwaxia Formation and Madongshan-Naijiahe Formation are two series of effective hydrocarbon source rock series of strata.Due to compression during the Himalayan,a large-scale overthrusting on the southwestern margin of the basin was developed,forming numerous NW-trending anticlinal traps favorable for hydrocarbon accumulation and for exploration aimed at the Cretaceous section in the basin." @default.
- W2369944105 created "2016-06-24" @default.
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- W2369944105 date "2007-01-01" @default.
- W2369944105 modified "2023-09-26" @default.
- W2369944105 title "Mesozoic Geological Characteristics and Hydrocarbon Exploration Direction in Liupanshan Basin" @default.
- W2369944105 hasPublicationYear "2007" @default.
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