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临汾盆地处于祁、吕、贺山字形构造的东翼,汾河地堑中段。这里断层构造复杂,新构造活动比较强烈,历史上曾发生过两次八级强震。一九六六年邢台地震后,盆地地震活动增强。一九七一年国家地震局组织地球物理所,地震地质大队等六个单位二百多人来我区开展地震会战工作达两年之久。为了加强领导,地委成立了地震会战领导组,配备了一名专职干部,印刷了一部分地震宣传材料,建立了八个群测群报土仪器点,十四个水位和动物观测点,做了一些工作。但由于当时对党的地震工作方针理解不深,对大搞群测群防运动认识不足,致使地震工作冷冷清清,没有形成群众运动。
Linfen basin is located in Qi, Lu, He Shan shaped structure of the eastern wing, Fenhe grabens the middle. Here the fault structure is complex, the new tectonic activity is relatively strong, there have been eight strong earthquakes in history. After the Xingtai earthquake in 1966, the seismic activity of the basin increased. In 1981, the Seismological Bureau organized more than 200 people from six units including the Institute of Geophysics and the Seismic Geological Brigade to conduct Earthquake Fighting Work in our district for two years. In order to strengthen leadership, the prefectural committee set up a leadership group for the earthquake warfare, equipped with a full-time cadre, printed some of the earthquake propaganda materials, established eight group survey earth equipment points, fourteen water levels and animal observation points and did Some work However, due to the lack of understanding of the party’s earthquake work guidelines at the time, the lack of understanding of mass vigilantes and prevention campaigns led to the cold and clear earthquakes and the absence of a mass movement.