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《Earthquake Research In China》 1991-02
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Discussion on the Model of the Seismogenic Structure for Datong-Yanggao Earthquake Swarm

Xu Xiwei Che Yongtai Yang Zhuen You Huichuan Wang Yanglong Zhu Yuxin(Institute of Geology,SSB)  
The regional environment of seismogenic structures, the pattern of the active faults, the destructive features of the buildings and properties or geometrical combination of the structural ground fissures caused by the strong ground motions during the earthquake swarm are discussed in detail in this paper. It is proposed that the Datong-Yanggao earthquake swarm was produced by the abrupt normal faulting on the northern piedmont fault of Mt. Liulingshan which induced the sinistral slipping of the NW-trending faults and the small block bounded by these faults clockwise rotated under the conditions of the crustal strenching in the northern extensional domain of the north part of the Shanxi rift system. Its occurrence may indicate that seismicity in the Shanxi rift system has entered a new active period.
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