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Research on coupling mechanism of mine structure and gas occurrence

机译:矿井构造与瓦斯涌出耦合机理研究

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Taking south and east Suzhou mining areas as an example, the coupling mechanism of mine structure and gas occurrence is further discussed. The results show that the regional tectonics have a distinctly control over the distribution of gas content. East Suzhou mining area, located in the overlying system of Xu-Su thrust nappe structure, has good sealing conditions to preserve gas, which leads to a well developed high-gas coal reservoir. Relatively, south Suzhou mining area lies in the underlying system, showing a low gas content. Meanwhile, mine structures also control the heterogeneity of gas distribution. For example, relatively large scale mine fractures are always the demarcation of adjacent gas division and the shear fractures is the main basis for division of relatively closed tectonic units. Moreover, shear sliding faults often change the thickness of coal seam rapidly, resulting in dangerous zones of high gas content and outburst.
机译:以苏州南部和东部矿区为例,进一步探讨了矿井构造与瓦斯涌出的耦合机理。结果表明,区域构造对瓦斯含量的分布具有明显的控制作用。苏州东部矿区位于徐苏逆冲推覆构造的上覆系统中,具有良好的封闭条件,可以保护瓦斯,从而形成了发达的高瓦斯煤藏。相对而言,苏州南部矿区位于下伏系统中,天然气含量较低。同时,矿井结构也控制了瓦斯分布的非均质性。例如,相对较大的矿井裂缝始终是相邻瓦斯划分的分界,而剪切裂缝是划分相对封闭的构造单元的主要依据。而且,剪切滑动断层经常迅速改变煤层的厚度,从而导致高瓦斯含量和突出的危险区域。

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