潞安常村井田陷落柱分布规律与成因初探
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摘要
陷落柱发育、导水和集聚瓦斯都对煤矿安全生产产生威胁.依据常村井田现勘探揭露陷落柱发育的位置和特征,从岩溶发育条件、地下水径流条件以及构造发育条件等3个方面对常村井田陷落柱成因进行了分析,指出上述3个条件是常村井田陷落柱发育的主要因素,且三者相互联系,进而得出了陷落柱发育的规律:陷落柱多发育在奥灰水富水异常区、张扭性断层应力集中部位和向斜轴部褶曲部位及其转折端.
The cultivation,conducting water and gathering gas of the karstic collapse columns are threatening in the coal mines.According to the location and features of the karstic collapse columns in Changcun coal mine field,the causes of the karstic collapse columns were analyzed in the aspects of the karst development condition,the ground water flow condition and the tectonic setting,which were considered to major factors,and these factors interacted with each other and they did not function separably.The basic rule of karstic collapse columns' spatial distribution in Changcun coal mine field is concluded finally as follows:Ordovician limestone rich water anomalies,tenso-shear faults stress concentrations and the syncline axises and their turning ends are the positions in which the karstic collapse columns are likely to develop.
The cultivation,conducting water and gathering gas of the karstic collapse columns are threatening in the coal mines.According to the location and features of the karstic collapse columns in Changcun coal mine field,the causes of the karstic collapse columns were analyzed in the aspects of the karst development condition,the ground water flow condition and the tectonic setting,which were considered to major factors,and these factors interacted with each other and they did not function separably.The basic rule of karstic collapse columns' spatial distribution in Changcun coal mine field is concluded finally as follows:Ordovician limestone rich water anomalies,tenso-shear faults stress concentrations and the syncline axises and their turning ends are the positions in which the karstic collapse columns are likely to develop.
引文
[1]钟亚平.开滦煤矿防治水综合技术研究[M].北京:煤炭工业出版社,2001.
[2]曹代勇,张杰林,关英斌,等.潞安矿区构造格局及构造演化[J].煤炭学报,1995,20(2):174-178.
[3]马永明.潞安-长治矿区地质构造形成机制探讨[J].中国煤田地质,2005,17(1):1-3.
[4]曹代勇,关英斌.晋-获断裂带分段模式研究[J].大地构造与成矿学,1997,21(4):323-329.
[5]白海波,缪协兴.潞安矿区奥陶系岩溶演化主控因素分析[J].采矿与安全工程学报,2008,25(1):17-21.
[6]李祥根.中国新构造运动概论[M].北京:地震出版社,2003:19.
[7]钱学溥.石膏喀斯特陷落柱的形成及其水文地质意义[J].中国岩溶,1988,7(4):344-34.
[8]尹尚先.煤矿区突(涌)水系统分析模拟及应用[D].北京:中国矿业大学(北京),2002.5.
[9]王锐.论华北地区岩溶陷落柱的形成[J].水文地质工程地质,1982(1):37-44.
[10]徐卫国,赵桂荣.试论岩溶矿区地面塌陷的真空吸蚀作用[J].地质论评,1981,27(2):175-180.
[11]张茂林,伊尚先.华北型煤田陷落柱形成过程研究[J].煤田地质与勘探,2007,35(6):26-29.
[12]史红霞.潞安矿区岩溶陷落柱相关因素分析[J].煤,2004,13(4):52-53.
[13]刘芳珍.潞安矿区奥陶系岩溶发育规律及成因探讨[J].地下水,1997,20(2):70-73.
[14]河南省煤炭地质勘察研究院.常村煤矿生产矿井地质报告[R].2004.
[15]白海波,缪协兴.王庄-常村断裂带新生性及其控水作用[J].辽宁工程技术大学学报,2006,25(增刊):25-27.
[16]白海波,缪协兴,冯梅梅.潞安矿区新构造及其控水作用的研究[J].采矿与安全工程学报,2006,23(4):382-388.
[17]陈敬轶,姚军朋,张子敏,等.晋城成庄煤矿陷落柱成因与差异升降运动[J].河南理工大学学报:自然科学版,2006,25(6):465-468.
[2]曹代勇,张杰林,关英斌,等.潞安矿区构造格局及构造演化[J].煤炭学报,1995,20(2):174-178.
[3]马永明.潞安-长治矿区地质构造形成机制探讨[J].中国煤田地质,2005,17(1):1-3.
[4]曹代勇,关英斌.晋-获断裂带分段模式研究[J].大地构造与成矿学,1997,21(4):323-329.
[5]白海波,缪协兴.潞安矿区奥陶系岩溶演化主控因素分析[J].采矿与安全工程学报,2008,25(1):17-21.
[6]李祥根.中国新构造运动概论[M].北京:地震出版社,2003:19.
[7]钱学溥.石膏喀斯特陷落柱的形成及其水文地质意义[J].中国岩溶,1988,7(4):344-34.
[8]尹尚先.煤矿区突(涌)水系统分析模拟及应用[D].北京:中国矿业大学(北京),2002.5.
[9]王锐.论华北地区岩溶陷落柱的形成[J].水文地质工程地质,1982(1):37-44.
[10]徐卫国,赵桂荣.试论岩溶矿区地面塌陷的真空吸蚀作用[J].地质论评,1981,27(2):175-180.
[11]张茂林,伊尚先.华北型煤田陷落柱形成过程研究[J].煤田地质与勘探,2007,35(6):26-29.
[12]史红霞.潞安矿区岩溶陷落柱相关因素分析[J].煤,2004,13(4):52-53.
[13]刘芳珍.潞安矿区奥陶系岩溶发育规律及成因探讨[J].地下水,1997,20(2):70-73.
[14]河南省煤炭地质勘察研究院.常村煤矿生产矿井地质报告[R].2004.
[15]白海波,缪协兴.王庄-常村断裂带新生性及其控水作用[J].辽宁工程技术大学学报,2006,25(增刊):25-27.
[16]白海波,缪协兴,冯梅梅.潞安矿区新构造及其控水作用的研究[J].采矿与安全工程学报,2006,23(4):382-388.
[17]陈敬轶,姚军朋,张子敏,等.晋城成庄煤矿陷落柱成因与差异升降运动[J].河南理工大学学报:自然科学版,2006,25(6):465-468.
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