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鄂尔多斯盆地南北部侏罗系煤层含气性差异分析

Analysis of gas bearing property difference of Jurassic coal between Southern and Northern Ordos Basin

  • 摘要: 为了弄清造成鄂尔多斯盆地南北部侏罗系煤层含气性差异的主要原因,以盆地内煤层含气量与含气饱和度为基础,从煤层的生气能力、构造运动、水文地质条件与煤层顶底板岩性特征等4个方面进行了分析研究。结果表明,侏罗系煤层在盆地北部保存完整但含气性较差、南部保存不完整但含气性较好。南部煤层热演化程度较北部高,生气强度大,盆地南部地层水矿化度较盆地北部高,地下水动力条件较弱,有利于煤层气的富集和保存,而盆地南北部主要煤层顶底板岩性主要以泥岩为主,顶底板岩性对煤层气的富集影响大致相同。综合分析认为,影响鄂尔多斯盆地南北部侏罗系煤层含气性差异的主要因素是水文地质条件、构造运动和生气能力。

     

    Abstract: In order to find out the main reasons for the difference of gas bearing property of Jurassic coal seam in the northern and southern Ordos Basin,based on the gas content and gas saturation of coal seam in the basin,from the four aspects of the coal seam's gas generating capacity,tectonic movement,hydrogeological conditions and lithologic characteristics of roof and floor of coal seam,the analysis and research are carried out.The results show that Jurassic coal seam is intact in the northern part of the basin,but has poor gas content,the southern part is incomplete but has good gas content.The degree of thermal evolution of the coal seam in the south is higher than that in the north,and the gas intensity is strong,the mineralization degree of formation water in the southern part of the basin is higher than that in the northern part of the basin,and the dynamic condition of groundwater is weak,which is favorable for the enrichment and preservation of coalbed methane.The roof and floor of the main coal seam in the north and south of the basin is mainly mudstone,and the influence of them on coalbed methane is almost the same.The comprehensive analysis shows that the main factors affecting the gas-bearing difference of the Jurassic coal seam in the northern and southern Ordos Basin are hydrogeological conditions,tectonic movement and vitality.

     

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