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鄂尔多斯盆地西南缘煤矿瓦斯地质条件
引用本文:范立民,申涛.鄂尔多斯盆地西南缘煤矿瓦斯地质条件[J].中国煤炭地质,2011(3):18-23.
作者姓名:范立民  申涛
作者单位:陕西省地质调查院,陕西西安710065
基金项目:国家能源局全国瓦斯地质编图项目(国能煤炭[2009]117号); 陕西省人民政府“高瓦斯和煤与瓦斯突出矿井通风及瓦斯治理”项目(陕政办发〔2005〕120号)
摘    要:鄂尔多斯盆地西南缘的彬长矿区开采侏罗系4号煤层,大地构造位置处于华北板块鄂尔多斯盆地渭北隆起带西部的彬长坳褶带内,矿区内瓦斯含量总体偏低,但褶皱地带及断层附近存在高瓦斯区域。研究结果显示,该区瓦斯含量主要受断层和褶曲构造的控制,瓦斯涌出量基本与煤层底板标高为负相关,与煤层厚度为正相关,与煤层埋藏深度和上覆基岩厚度呈正相关,总体上彬长矿区瓦斯涌出量从矿区周边向中部有明显增大的趋势,瓦斯绝对涌出量将随着煤矿生产能力的增大而增大。矿区瓦斯资源总量约44.91亿m3,可开发量约12.94亿m3,具有较好的开发前景,应尽早开展总体规划,统筹考虑,科学开发利用。

关 键 词:瓦斯(煤层气)  赋存规律  延安组  构造控气  鄂尔多斯盆地

Gas Geological Condition of Coalmines on Southwestern Margin of Ordos Basin
Fan Limin,Shen Tao.Gas Geological Condition of Coalmines on Southwestern Margin of Ordos Basin[J].Coal Geology of China,2011(3):18-23.
Authors:Fan Limin  Shen Tao
Affiliation:(Shaanxi Provincial Geological Exploration Institute,Xian,Shaanxi 710065)
Abstract:The Binchang mining area on the southwestern margin of the Ordos Basin is now mining Jurassic No.4 coal seam.Tectonic location of the mining area is within the Binchang depression/fold belt,Weibei uplift zone in the Ordos Basin,North China plate.As a whole,the gas content is on the low side,but high gas content regions are existed near the folded area and faults.The studied result has demonstrated that gas content in the area is mainly controlled by faults and folds.Gas emission basically presents negative correlation with coal seam floor elevation,positive correlation with coal thickness,buried depth and overburden thickness.In the mass,gas emission has an increasing tendency from mining area periphery toward the center,absolute emission increasing along with coalmine capacity.Total resource of gas in the mining area is about 4.491 billion cubic meters,exploitable about 1.294 billion cubic meters,thus has preferable exploitation prospect.Overall planning at the earliest opportunity,plan as a whole and scientifically exploitation and utilization have been suggested.
Keywords:gas(CBM)  hosting pattern  Yanan Formation  structural gas control  southwestern margin of Ordos Basin
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