首页> 外文期刊>Journal of natural gas science and engineering >Occurrence features and gas content analysis of marine and continental shales: A comparative study of Longmaxi Formation and Yanchang Formation
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Occurrence features and gas content analysis of marine and continental shales: A comparative study of Longmaxi Formation and Yanchang Formation

机译:海洋和大陆的发生特征和天然气内容分析:龙曼地区与延阳地层的比较研究

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摘要

To study the occurrence state and content of shale gas in different depositional environments, 15 marine shale samples from Longmaxi Formation in the Sichuan Basin and 15 continental shale samples from Yanchang Formation in the Ordos Basin were sampled. Then a series of experiments, including X-ray diffraction analysis, TOC content analysis, R-o measurement, NMR measurements, FE-ESEM observation, low-pressure N-2 adsorption, and CH4 isothermal adsorption were conducted. In general, shale gas in Yanchang formation has the characteristics of primary adsorbed gas, moderate free gas, and non-ignorable dissolved gas, whereas shale gas in Longmaxi formation has the characteristics of joint dominated free gas and adsorbed gas, as well as negligible dissolved gas. Both macroscopic accumulation pattern and microscopic occurrence model show four stages in the whole thermal evolution, that is, adsorption, pore filling, fracture filling and accumulation. By analyzing the affecting factors of shale gas adsorption, conclusions can be drawn that geological characteristics, mineral compositions, pore structure features and formation conditions have influence on adsorbed gas content to various degrees. Cause analyses reveal that differences in occurrence state and gas content between marine and continental shales are immediately affected by the differences of organic matter type, thermal maturity, brittle minerals content, carbonate content, SSA, PD, porosity, gas saturation, residual oil quantity, as well as T&P, indirectly controlled by sedimentary environment and tectonic movement.
机译:为了研究不同沉积环境中页岩气的出现状态和含量,在鄂尔多斯盆地中,四川盆地中龙曼河谷形成的15个海洋页岩样本和来自鄂尔多斯盆地的延长地层的15个欧式页岩样品。然后进行一系列实验,包括X射线衍射分析,TOC含量分析,R-O测量,NMR测量,Fe-ESEM观察,低压N-2吸附和CH 4等温吸附。一般来说,延长地层的页岩气具有初级吸附气体,适度的自由气体和不可忽略的溶解气体的特点,而龙马模块中的页岩气具有关节主导的自由气和吸附气体的特点,以及可忽略的溶解气体。宏观累积模式和微观发生模型均显示出全热演化中的四个阶段,即吸附,孔隙,骨折填充和积累。通过分析页岩气吸附的影响因素,可以绘制结论,地质特征,矿物组合物,孔结构特征和地层条件对各种度的吸附气体含量影响。原因分析表明,海洋和大陆股骨头之间发生状态和天然气含量的差异立即受到有机物质类型,热成熟度,脆性矿物质含量,碳酸盐含量,SSA,Pd,孔隙率,气体饱和度,残留油量的差异影响,以及T&P,由沉积环境和构造运动间接控制。

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