五阳矿井瓦斯地质规律与瓦斯预测
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摘要
通过运用瓦斯赋存构造逐级控制理论,研究了潞安矿区五阳矿井地质构造对瓦斯赋存的控制;结合五阳矿井大量瓦斯地质资料和实测数据,编制矿井瓦斯地质图;研究矿井瓦斯赋存规律,并对矿井进行瓦斯含量和瓦斯涌出量预测,评价煤层气(瓦斯)资源量,对煤与瓦斯突出区域进行预测。
潞安矿区主体构造是NNE向、NE向展布的向、背斜褶皱及与EW方向构造的复合;矿井内天仓向斜的轴部地带瓦斯含量较高,小型断层和陷落柱比较发育,陷落柱密集分布于天仓向斜轴附近约800m的范围内。论文具体内容:编制五阳矿井瓦斯地质图;把煤层上覆基岩厚度、顶底板岩性、距断层的距离、煤层厚度、煤的挥发分5个相关因素进行多元分析,得出了多元分析瓦斯赋存情况与单因素煤层埋深情况相近,采用单因素煤层埋深进行瓦斯含量预测;依据五阳矿井的实际情况,把五阳矿井划分为15个块段进行资源量计算;依据实测参数和矿井主要地质构造特点,将井田内3#煤层埋深490m以深划为煤与瓦斯突出危险区。
Through the use of gas deposit step by step structure control theory ,to study the Luan Mining, Wuyang mine geological structure of the gas distribution control; Combination of a lot of gas geological data and field data in Wuyang mine, making gas geological map; to study Mine Gas deposit law, and mine gas emission and gas content prediction, evaluation coal methane (gas) resource, coal and gas outburst forecast.
Main structure of Luan mining area is NNE, NE anticline and compound structure of the EW direction; the gas content is high at axis of Tianchang syncline, relatively small-scale faults and collapse column development, collapse column is distributed axis of the Tianchang synclinal about 800m range. Paper details: Making Wuyang mine gas geological map; The depth of coal seam, roof and floor rock, the distance from the fault, coal seam thickness, volatile of coal, five related factors multielement analysis shows that the multivariate analysis of gas occurrence situation is similar to the case of single factor, coal seam depth of the single factor forecast gas content; Based on the actual situation in Wuyang mine, the mine was divided into 15 block, to calculate resources; based on the measured parameters and mine geological features to predict elevation +482 seam below, near axis of Tianchang syncline, coal and gas outburst is the most dangerous..
潞安矿区主体构造是NNE向、NE向展布的向、背斜褶皱及与EW方向构造的复合;矿井内天仓向斜的轴部地带瓦斯含量较高,小型断层和陷落柱比较发育,陷落柱密集分布于天仓向斜轴附近约800m的范围内。论文具体内容:编制五阳矿井瓦斯地质图;把煤层上覆基岩厚度、顶底板岩性、距断层的距离、煤层厚度、煤的挥发分5个相关因素进行多元分析,得出了多元分析瓦斯赋存情况与单因素煤层埋深情况相近,采用单因素煤层埋深进行瓦斯含量预测;依据五阳矿井的实际情况,把五阳矿井划分为15个块段进行资源量计算;依据实测参数和矿井主要地质构造特点,将井田内3#煤层埋深490m以深划为煤与瓦斯突出危险区。
Through the use of gas deposit step by step structure control theory ,to study the Luan Mining, Wuyang mine geological structure of the gas distribution control; Combination of a lot of gas geological data and field data in Wuyang mine, making gas geological map; to study Mine Gas deposit law, and mine gas emission and gas content prediction, evaluation coal methane (gas) resource, coal and gas outburst forecast.
Main structure of Luan mining area is NNE, NE anticline and compound structure of the EW direction; the gas content is high at axis of Tianchang syncline, relatively small-scale faults and collapse column development, collapse column is distributed axis of the Tianchang synclinal about 800m range. Paper details: Making Wuyang mine gas geological map; The depth of coal seam, roof and floor rock, the distance from the fault, coal seam thickness, volatile of coal, five related factors multielement analysis shows that the multivariate analysis of gas occurrence situation is similar to the case of single factor, coal seam depth of the single factor forecast gas content; Based on the actual situation in Wuyang mine, the mine was divided into 15 block, to calculate resources; based on the measured parameters and mine geological features to predict elevation +482 seam below, near axis of Tianchang syncline, coal and gas outburst is the most dangerous..
引文
[1]张子敏,高建良,张瑞林等.关于中国煤层瓦斯区域分布的几点认识[J].地质科技情报, 1999(04): 67-70.
[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(02): 174-179.
[3]张子敏,张玉贵.瓦斯地质学[M].徐州:中国矿业大学出版社,2009:5.
[4]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,2006:4,55
[5]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
[6] A.9.彼特罗祥著(宋世钊译).煤矿沼气涌出[M].北京:煤炭工业出版社,1980.
[7] DAVID P. CREEDY. Geological controls on the Formation and distribution of Gas in.3ritish coalM easure strata,UK[J]. International of coal geology. 1988,(10).
[8] Frodsham K ,GayerR A.Thei mpacto ftectonicd eformationu poncoalsea ms' in the South Wales coalfield, UK[J]. Int J.Coal Geol.1999 (38):297-332.
[9] Shepherd J. Outbursts and geological structures in coal mines,Australia[J].Int J Rock Mech M in Sci&Geomech. 1981,18(4):267.
[10]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,1998,70-84.
[11]张子敏,高建良,张瑞林,等.关于中国煤层瓦斯区域分布的几点认识[J].地质科技情报,
[12]曹运兴,张玉贵,李凯奇,等.构造煤的动力变质作用及其演化规律[J].煤田地质与勘探,1996,24(4):15-17
[13] Zhang, Y. G.,Cao, Y. X.,Xie, H. B.,et al. Orphological and structural features of tectonic coal[A]. Li,B.Q. and Liu,Z.Y.Prospects for Coal Science in the 21st Century[C].Taiyuan, China,Shanxi Science Press,1999,57-60
[14] Zhang Yugui,Li Fan,Lu Huiqin, Xie Kechang,Tang Xuyi . The effects of macerals and their structure on the proneness of coal spontaneous combustion. In Symposium of the 2000 Safety Science and Technology International Beijing Conference. 2000,5. (ISTP收录)
[15]周世宁.瓦斯在煤层中的流动机理[J].煤炭学报,1990,15(1):61-67
[16]张亮,山西煤层气资源评价及开发利用[M].太原:山西出版集团\山西经济出版社,2007
[17]单秀琴.沁水盆地煤层储集性能[J].石油与天然气地质, 1998(04)
[18]冀涛,杨德义.沁水盆地煤层气地质条件评价[J].煤炭工程, 2007(10)
[19]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(01)
[20]池卫国.沁水盆地煤层气的水文地质控制作用[J].石油勘探与开发, 1998(03)
[21]曹代勇,钱光谟,关英斌等.晋获断裂带发育对煤矿区构造的控制[J].中国矿业大学学报,
[22]张子敏主编,瓦斯地质学[M].徐州:中国矿业大学出版社,2009
[23]林柏泉周世宁,煤层瓦斯赋存与流动理论[M].北京:煤炭工业出版社,1999
[24]刘洪林,李贵中,王广俊等编著,沁水盆地煤层气地质特征与开发前景[M]:石油工业出版社,2009: 152.
[25]张玉贵,张子敏,曹运兴.构造煤结构与瓦斯突出[J].煤炭学报, 2007(03): 281-284.
[26]田旭飞,张文平.五阳煤矿3#煤层瓦斯含量多元回归分析[J].问题探讨,2009(09):53—54.
[27]张小兵,张子敏,张玉贵.力化学作用与构造煤结构[J].中国煤炭地质, 2009(02): 10-14.
[28] ZHANG Zixu,YUAN Chongfu.Study on mathematical model of coalbed gas geology used top rediction of mine gas emission[J].Journal of China Coal Society ,1994 (4):368-372.
[29] ZHANG Zixu,TANG Youyi.The Research Report of the Rules of Gas Geology In Xinwen Mine[D].Jiaozuo:Jiaozuo Institute of Technology,2000:8 -11.
[30] Zhang Yugui,Cao Yunxin,Xie Hongbao,et al Morphological And Structural Features of Tectonic Coal[J].In The 10th In ternational Coal Conference,1999,9: 34-38.
[31] CaoY X,Hou Q L,ZhangY G,et al .Some basic problems on ductile shear zones along coal seams within shallow and superficial tectonic layers[A] Geology Society of China.Progress in Geology of China(1993-1996)-papers to 30th IGC[C] .Beijing:Ocean Press , 1996 ,(8):355-358.
[32]丘元禧.论构造复合[J].地质力学学报,1998,4(1):1-12.
[33]严家平,王定武.利用煤田钻孔测井信息判识祁东煤矿构造煤的理论与实践[J].矿业安全与环保,2003,30(6):36-38.
[34]张玉贵,樊孝敏,王世国.测井曲线在研究构造煤中的应用[J].焦作矿业学院学报,1995,14(1):76-78.
[35]杨为民.利用测井曲线分析和判别构造煤[J].煤炭科技资料,1991,(4):1-5.
[36]龙王寅,朱文伟,徐静等.利用测井曲线判识煤体结构探讨[J].中国煤田地质,1999,11(2):64-69.
[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(02): 174-179.
[3]张子敏,张玉贵.瓦斯地质学[M].徐州:中国矿业大学出版社,2009:5.
[4]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,2006:4,55
[5]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
[6] A.9.彼特罗祥著(宋世钊译).煤矿沼气涌出[M].北京:煤炭工业出版社,1980.
[7] DAVID P. CREEDY. Geological controls on the Formation and distribution of Gas in.3ritish coalM easure strata,UK[J]. International of coal geology. 1988,(10).
[8] Frodsham K ,GayerR A.Thei mpacto ftectonicd eformationu poncoalsea ms' in the South Wales coalfield, UK[J]. Int J.Coal Geol.1999 (38):297-332.
[9] Shepherd J. Outbursts and geological structures in coal mines,Australia[J].Int J Rock Mech M in Sci&Geomech. 1981,18(4):267.
[10]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,1998,70-84.
[11]张子敏,高建良,张瑞林,等.关于中国煤层瓦斯区域分布的几点认识[J].地质科技情报,
[12]曹运兴,张玉贵,李凯奇,等.构造煤的动力变质作用及其演化规律[J].煤田地质与勘探,1996,24(4):15-17
[13] Zhang, Y. G.,Cao, Y. X.,Xie, H. B.,et al. Orphological and structural features of tectonic coal[A]. Li,B.Q. and Liu,Z.Y.Prospects for Coal Science in the 21st Century[C].Taiyuan, China,Shanxi Science Press,1999,57-60
[14] Zhang Yugui,Li Fan,Lu Huiqin, Xie Kechang,Tang Xuyi . The effects of macerals and their structure on the proneness of coal spontaneous combustion. In Symposium of the 2000 Safety Science and Technology International Beijing Conference. 2000,5. (ISTP收录)
[15]周世宁.瓦斯在煤层中的流动机理[J].煤炭学报,1990,15(1):61-67
[16]张亮,山西煤层气资源评价及开发利用[M].太原:山西出版集团\山西经济出版社,2007
[17]单秀琴.沁水盆地煤层储集性能[J].石油与天然气地质, 1998(04)
[18]冀涛,杨德义.沁水盆地煤层气地质条件评价[J].煤炭工程, 2007(10)
[19]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(01)
[20]池卫国.沁水盆地煤层气的水文地质控制作用[J].石油勘探与开发, 1998(03)
[21]曹代勇,钱光谟,关英斌等.晋获断裂带发育对煤矿区构造的控制[J].中国矿业大学学报,
[22]张子敏主编,瓦斯地质学[M].徐州:中国矿业大学出版社,2009
[23]林柏泉周世宁,煤层瓦斯赋存与流动理论[M].北京:煤炭工业出版社,1999
[24]刘洪林,李贵中,王广俊等编著,沁水盆地煤层气地质特征与开发前景[M]:石油工业出版社,2009: 152.
[25]张玉贵,张子敏,曹运兴.构造煤结构与瓦斯突出[J].煤炭学报, 2007(03): 281-284.
[26]田旭飞,张文平.五阳煤矿3#煤层瓦斯含量多元回归分析[J].问题探讨,2009(09):53—54.
[27]张小兵,张子敏,张玉贵.力化学作用与构造煤结构[J].中国煤炭地质, 2009(02): 10-14.
[28] ZHANG Zixu,YUAN Chongfu.Study on mathematical model of coalbed gas geology used top rediction of mine gas emission[J].Journal of China Coal Society ,1994 (4):368-372.
[29] ZHANG Zixu,TANG Youyi.The Research Report of the Rules of Gas Geology In Xinwen Mine[D].Jiaozuo:Jiaozuo Institute of Technology,2000:8 -11.
[30] Zhang Yugui,Cao Yunxin,Xie Hongbao,et al Morphological And Structural Features of Tectonic Coal[J].In The 10th In ternational Coal Conference,1999,9: 34-38.
[31] CaoY X,Hou Q L,ZhangY G,et al .Some basic problems on ductile shear zones along coal seams within shallow and superficial tectonic layers[A] Geology Society of China.Progress in Geology of China(1993-1996)-papers to 30th IGC[C] .Beijing:Ocean Press , 1996 ,(8):355-358.
[32]丘元禧.论构造复合[J].地质力学学报,1998,4(1):1-12.
[33]严家平,王定武.利用煤田钻孔测井信息判识祁东煤矿构造煤的理论与实践[J].矿业安全与环保,2003,30(6):36-38.
[34]张玉贵,樊孝敏,王世国.测井曲线在研究构造煤中的应用[J].焦作矿业学院学报,1995,14(1):76-78.
[35]杨为民.利用测井曲线分析和判别构造煤[J].煤炭科技资料,1991,(4):1-5.
[36]龙王寅,朱文伟,徐静等.利用测井曲线判识煤体结构探讨[J].中国煤田地质,1999,11(2):64-69.