| 贵州习水矿区构造特征分析 |
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| 引用本文： | 唐显贵,黄文.贵州习水矿区构造特征分析[J].中国煤田地质,2007,19(4):21-24. |
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| 作者姓名： | 唐显贵 黄文 |
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| 作者单位： | [1]贵州煤矿地质工程咨询与地质环境监测中心,贵州贵阳550009 [2]贵州省煤田地质局地质勘察处,贵州贵阳550009 |
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| 摘 要： | 根据已有煤田地质资料,对习水矿区的地质构造进行了分析研究,认为矿区断裂以正断层为主,断层力学性质多属压扭性,东西向构造早于北东向构造;构造复合部位较复杂,其余区段较简单;矿区南部以褶断带为主,北部以断裂为主的单斜构造带。构造线方向性明显,与区域构造线方向一致。建议在矿区开发时,应尽可能避开构造复合部位（区段）,选择构造对煤层影响较小的矿区北部地段。
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| 关 键 词： | 构造特征 组合关系 习水矿区 |
| 文章编号： | 1004-9177（2007）04-0021-04 |
| 收稿时间： | 2007-05-28 |
| 修稿时间： | 2007-05-28 |
Discussion on Structural Characteristics in Xishui Mining Area |
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| Tang Xiangui, Huang Wen.Discussion on Structural Characteristics in Xishui Mining Area[J].Coal Geology of China,2007,19(4):21-24. |
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| Authors: | Tang Xiangui Huang Wen |
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| Institution: | 1. Guizhou Coalmine Geological Engineering Consultation and Geological Environmental Supervision and Testing Center, Guiyang, Guizhou 550009; 2.Geological Exploration Department, Guizhou Bureau of Coal Geology, Guiyang, Guizhou 550009 |
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| Abstract: | Based on geological data of look for coal,the paper analyzed geological structure in the Xishui mining area,considered that the faulted structure in the mining area is mainly compresso-sheafing normal faults. EW structure is earlier than NE structure, structural compounding part is rather complex, while other parts are simple. Southern mining area is mainly a fault-fold zone; northern part is mainly faulted monocline zone, Directivity of structural line is clear; it is in accord with tectonic lineament. It is advised that during the mining area exploitation, the structural compounding part should keep away from; while the northern part of the mining area less structural impact sector will be better. |
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| Keywords: | structural characteristic combination Xishui mining area |
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