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断块构造区域内煤层及其周围岩层在构造应力作用下的形变具有很好的协调性和密切的相关性。利用煤层构造破碎度,能预测底板隔水层的构造破坏程度。经过几年的现场试验研究,证明该方法简便,结果直观。
The deformation of the coal seam and its surrounding strata under the tectonic stress within the fault block structure has good coordination and close correlation. By using the coal seam to construct the degree of fragmentation, it is possible to predict the structural failure of the aqueduct. After several years of field experiments, the method proved to be simple and the result was intuitive.