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作 者:刘红瑾 Liu Hongjin(The Forth Geological Team of Henan Coal Geology Bureau,Zhengzhou,Henan,450000)
出 处:《中国井矿盐》2020年第4期27-29,共3页China Well and Rock Salt
摘 要:井田内地质构造主要表现为正、逆断层发育,褶皱较少,断层多而且互相切割交叉,构造程度较为复杂,受其影响,煤层厚度、瓦斯赋存及矿井涌水量等均发生了一定的变化,因此,对井田内构造进行详细分析和研究,对矿井的安全生产具有重大意义。Mine geological structure within the main show is positive and reverse fault development, less fold, fault and cutting cross each other, more degree of structure is relatively complex, affected by the thickness of coal seam gas occurrence and mine water inflow, etc must be changed, therefore, a detailed analysis and research within the field construction, is of great significance for mine safety production.
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