太行山山前断裂带之邯郸断裂段北起永年临洺关，过邯郸市区西 侧，大致沿京广线延伸，到达磁县北，被北西西(NWW)向的磁县断裂分 隔，全长约 56 公里，走向北北东(NNE)向，倾向东(E)，为邯郸断陷 的西边界，与东界临漳断裂带一起控制了沉积厚度...
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冰达坂-夏热嘎断裂呈北西西向贯通研究区。
Bingdaban-Xiarega Fault runs through this area in northwest-west orientation.
北西西系是成盆期的构造和同沉积构造，对盆地聚煤起最主要的控制作用；
The NNW structural system is considered to be synbasinal and syndepositional structures, which appear exert the most important controlling effects on coal accumulation in the basin.
由此推测，主震的错动面为北西西走向，可能是高倾角的左旋平移断层的滑动结果。
From this, it has been inferred that the strike of the dislocating fault plane of the main shock is NWW. It seems to be a left lateral horizontal slip fault with high dipping Angle.
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