司马煤矿瓦斯地质规律研究及突出危险区预测
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摘要
矿井瓦斯赋存分布规律研究涉及瓦斯风化带的确定和影响煤层瓦斯赋存的主控地质因素两个方面.结合司马煤矿煤层瓦斯情况,运用地质构造控制逐级制理论分析了矿井的瓦斯赋存特征,确定了3号煤层的瓦斯风化带、瓦斯的赋存形式及影响煤层瓦斯赋存的地质因素,揭示了3号煤层瓦斯聚集规律,分析了矿井瓦斯突出危险性指标,运用单项指标法对3号煤层煤与瓦斯突出危险区进行预测,为合理开发利用煤层瓦斯,防治煤与瓦斯突出和今后的安全生产提供了科学依据.
The determation of gas weathering zone and the main control factors of the gas occurrence are the two aspects of the discussion of the rule of gas occurrence in coal mine.This artical introduces the basic conditions of the Sima coal mine which including analyz the gas consequences in Sima coal mine and using the theroy of sequential control system of geological structure to analyze the features of the gas occurrence in coal.Thus it defines the gas waethering zone in No.3 coal mine and analyzes the occurrence of gas and the main effective geology factors of gas occurrence.In order to exploit the gas of coal reasonably,prevent and cure the coal and gas outburst,provide the foundation for the safe production in the future,this article aims to analyze the danger index of gas outburst and predict the danger zone of coal and gas outburst in No.3 coal mine by using the single index method.
The determation of gas weathering zone and the main control factors of the gas occurrence are the two aspects of the discussion of the rule of gas occurrence in coal mine.This artical introduces the basic conditions of the Sima coal mine which including analyz the gas consequences in Sima coal mine and using the theroy of sequential control system of geological structure to analyze the features of the gas occurrence in coal.Thus it defines the gas waethering zone in No.3 coal mine and analyzes the occurrence of gas and the main effective geology factors of gas occurrence.In order to exploit the gas of coal reasonably,prevent and cure the coal and gas outburst,provide the foundation for the safe production in the future,this article aims to analyze the danger index of gas outburst and predict the danger zone of coal and gas outburst in No.3 coal mine by using the single index method.
引文
[1]煤炭科学研究总院重庆分院.司马矿井煤层瓦斯含量测定及瓦斯涌出预测报告[R].2007.
[2]山西省114煤田地质队.山西省长治市潞安矿区司马井田勘探(精查)地质报告[R].2002.
[3]牛树银,陈路,许传诗,等.太行山区地壳演化及成矿规律[M].北京:地震出版社,1994.
[4]王永,冯富成.沁水盆地南端煤层气赋存的构造条件分析[J].西北地质,1998,19(3):28-31.
[5]张岳桥,杨农,马寅生.太行山隆起南段新构造变形过程研究[J].地质力学学报,2003,9(4):313-329.
[6]国土资源部.DZ/T0216-2002煤层气资源/储量规范[S].北京:地质出版社,2008.
[7]张子敏,张玉贵.瓦斯地质规律与瓦斯预测[M].北京:煤炭工业出版社,2005.
[8]张子敏,林又玲,吕绍林.中国煤层瓦斯分布特征[M].北京:煤炭工业出版社,1998.
[9]焦作矿业学院瓦斯地质研究室.瓦斯地质概率[M].北京:煤炭工业出版社,1990.
[10]周世宁,林柏泉.煤层瓦斯赋存与流动理论[M].北京:煤炭工业出版社,1999.
[11]郭德勇,韩德馨.地质构造控制煤和瓦斯突出作用类型研究[J].煤炭学报,1998,23(4):337-341.
[12]中华人民共和国煤炭工业部.防治煤与瓦斯突出细则[M].北京:煤炭工业出版社,1995.
[13]彭立世.煤与瓦斯突出区域预测的认识基础[J].煤矿安全,1996(2):35-37.
[2]山西省114煤田地质队.山西省长治市潞安矿区司马井田勘探(精查)地质报告[R].2002.
[3]牛树银,陈路,许传诗,等.太行山区地壳演化及成矿规律[M].北京:地震出版社,1994.
[4]王永,冯富成.沁水盆地南端煤层气赋存的构造条件分析[J].西北地质,1998,19(3):28-31.
[5]张岳桥,杨农,马寅生.太行山隆起南段新构造变形过程研究[J].地质力学学报,2003,9(4):313-329.
[6]国土资源部.DZ/T0216-2002煤层气资源/储量规范[S].北京:地质出版社,2008.
[7]张子敏,张玉贵.瓦斯地质规律与瓦斯预测[M].北京:煤炭工业出版社,2005.
[8]张子敏,林又玲,吕绍林.中国煤层瓦斯分布特征[M].北京:煤炭工业出版社,1998.
[9]焦作矿业学院瓦斯地质研究室.瓦斯地质概率[M].北京:煤炭工业出版社,1990.
[10]周世宁,林柏泉.煤层瓦斯赋存与流动理论[M].北京:煤炭工业出版社,1999.
[11]郭德勇,韩德馨.地质构造控制煤和瓦斯突出作用类型研究[J].煤炭学报,1998,23(4):337-341.
[12]中华人民共和国煤炭工业部.防治煤与瓦斯突出细则[M].北京:煤炭工业出版社,1995.
[13]彭立世.煤与瓦斯突出区域预测的认识基础[J].煤矿安全,1996(2):35-37.
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