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Investigation of pore structure and fractal characteristics of marine-continental transitional shales from Longtan Formation using MICP, gas adsorption, and NMR (Guizhou, China)

机译:麦克风,天然气吸附和NMR(贵州)龙堤地层隆至龙潭地层孔隙结构和分形特征研究

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摘要

Organic-rich shale samples from marine-continental transitional facies of the Late Permian Longtan Formation in southwestern Guizhou were investigated using organic petrography analysis, X-ray diffraction analysis, mercury intrusion capillary pressure experiments, gas adsorption experiments, nuclear magnetic resonance, scanning electron microscopy image analysis, and multi-fractal theory to quantitatively and qualitatively investigate the full-size pore structure and fractal characteristics of the shale. The correlations among the total organic carbon (TOC) content, mineral composition, and pore structure were discussed. The fractal dimension was used to evaluate the production potential of a shale reservoir.
机译:来自贵州西南部二叠纪龙潭地层的有机富有的页岩样品,采用有机探测器分析,X射线衍射分析,汞入侵毛细管压力实验,气体吸附实验,核磁共振,扫描电子显微镜检查 图像分析,多分形理论定量,定性地研究了页岩全尺寸孔隙结构和分形特征。 讨论了总有机碳(TOC)含量,矿物组合物和孔结构之间的相关性。 分形尺寸用于评估页岩储层的生产潜力。

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