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Pore characteristics of lacustrine shale within the oil window in the Upper Triassic Yanchang Formation, southeastern Ordos Basin, China

机译:鄂尔多斯盆地东南鄂尔斯盆地地区油窗口湖窗口中的孔隙特征

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摘要

Organic matter (OM)-rich shale in the Yanchang Formation is recognized as a promising hybrid shale oil/shale gas system in lacustrine strata in China. Being mainly in the oil window, both the type and distribution of the pores in the shale have been affected by several factors, including petroleum expulsion and retention, mineral and organic composition, and compaction. To obtain a better understanding of the factors controlling OM pore development, 10 core samples were selected with various OM content from the Chang 7 and Chang 9 members of the Yanchang Formation for pore characterization. The investigation combined microscopic observation, both of thin sections and ion milled surfaces of samples with low-pressure carbon dioxide and nitrogen adsorption and bulk porosity measurements, with the main emphasis being on OM-associated pores.
机译:延长地层中的有机物(OM)-RICH页岩被认为是中国湖泊地层中有前景的混合物流油/页岩气体系统。 主要在油窗口中,页岩中毛孔的类型和分布都受到了几种因素的影响,包括石油驱逐和保留,矿物质和有机组合物,并压实。 为了更好地理解控制OM孔隙发育的因素,选择了10个核心样本,其中来自延长形成的延长形成的常高7和延长9成员进行孔表征。 调查组合显微镜观察,薄截面和离子研磨表面的样品,具有低压二氧化碳和氮吸附和散装孔隙率测量,主要重点是在OM-相关孔隙上。

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