晋获断裂带位于沁水煤田东侧，是在基底软弱带基础上发育起来的一条区域性断裂带，由于变形强度、后期隆升、剥蚀和改造的差异，呈现明显的构造分段特征．晋获断裂带的发育和演化，对沁水煤田东部煤系赋存状况和煤矿区构造展布具有重要的影响 The Jinzheng fault zone is located on the east side of the Qinshui coalfield and is a regional fault zone developed on the basis of the weak zone of the basement. Due to the differences in deformation intensity, uplift, erosion and alteration during the later stages, the tectonic segment features are obvious. The development and evolution of Jinzheng fault zone have an important influence on the occurrence of coal measures and tectonic distribution in the east of Qinshui coalfield