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- W2378201719 abstract "The coal-bearing rocks during Carboniferous deposited in marine and land transitional environment in Qilian area. The deposits are carbonate and clastics during early Carbonferous, which are subabyssal and abyssal gravity current deposits during late Carboniferous in Liuyuan area. The deposits are terrigenous clastics, marine clastics, carbonate and pyroclastics in the north of Xinjiang area. The clastics during Carboniferous period are medium arkose, lithic arkose, litharenite and feldsparthic litharenite in the north of Xinjiang area; which are quartzarenite, subfeldsparthic litharenite, litharenite and arkose in the Qilian area. The stage of diagenesis is telodiagensis A-B, C, and locally it is at metamorphic stage. There are intergranular pores, intragranular pores, intercrystalline micropores of kaolinite and fractures. The reservoirs are of lower porosity-lower permeability. There are fewer primary pores because of its strong compaction in the north of Xinjiang area. There are better reservoirs where is near the zone of weathering in Qilian area. The better reservoirs of Upper Carboniferous are distributed in Wucaiwan area of northeastern Junggar basin, Shuangjingzi area of Qitai region and Chepaizi and Baikouquan areas in western Junggar basin and Xiaheyan block of Zhongwei area, Hongshuipu block of Jingtai area, and so on of Qilian region. The better reservoirs of the Lower Carboniferous are distributed in the Shuangjingzi area of northern Xinjiang and Hongshuipu area in Qilian region." @default.
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- W2378201719 title "The study on the clastics reservoir of the Carboniferous in the northwest of China" @default.
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