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A Study on Triassic Shale Gas Reservoir Characteristics from Ordos Basin

机译:鄂尔多斯盆地三叠纪页岩气藏特征研究

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The Triassic continental shale from Ordos basin was selected as the research object, through the analysis of X-ray diffraction (XRD), field emission scanning electron microscopy (SEM) and nitrogen adsorption experiment, the mineral composition and pore structure characteristics of Triassic continental shale from Ordos basin have been investigated in detail. X-ray diffraction analysis result shows that the mineral composition is mostly composed of clay minerals and silica minerals, with minor contributions made by carbonate minerals. The clay mineral content ranges from 40.5% to 66.0% with an average of 55.8%, and the silicoide mineral content accounts for 22.4% to 58.3%. Compared with marine shale gas reservoir, Triassic continental shales from Ordos basin are characterised by high clay mineral content. The shale samples show high specific surface areas of 1.1~22.9 m~2·g~(-1).
机译:来自鄂尔多斯盆地的三叠纪大陆页岩作为研究对象,通过分析X射线衍射(XRD),场发射扫描电子显微镜(SEM)和氮吸附实验,矿物成分和孔隙结构特征Triassic Continental Shale从鄂尔多斯盆地进行了详细研究。 X射线衍射分析结果表明,矿物组合物主要由粘土矿物和二氧化硅矿物组成,碳酸盐矿物质的少量贡献。粘土矿物质含量为40.5%至66.0%,平均为55.8%,硅化物矿物质含量占22.4%至58.3%。与海洋页岩煤气藏相比,鄂尔多斯盆地的三叠纪大陆Shales的特点是高粘土矿物质含量。页岩样品显示出1.1〜22.9 m〜2·g〜(-1)的高比表面积。

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