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《Earthquake》 1984-05
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A STUDY ON FEATURES OF RECENT ACTIVITY ALONG MAJOR FRACTURE ZONES IN WEST SICHUAN-YUNNAN REGION USING DATA OF FAULT DISPLACEMENT

Ye Chengzhi Hou Zhihua (Seismo-geological Brigade, State Seismological Bureau)  
Based on the data of fault displacement measured in the past decade or more from 14 sites along the Xianshuihe fracture zone, Xiaojiang fracture zone, Anninghe fracture zone and Honghe fracture zone, the directions of stresses acting upon the faults are inferred. The results show:1.According to the vectors of fault displacement, the directions of the compres-sive stresses mostly are NW-SE. Subjected to the principal compressive stresses in NW-SE direction, the nearly N-S striking faults are generally characterized by a counterclockwise compressive shearing, while the N-W striking faults by a counterclockwise tensile shearing.2.The tectonic activity in this region is quite intensive, with clear tendency, but behaves differently in places. Therefore, attentions should be given to those segments which are inactive or less active along these intensely active fracture zones in the future earthquake monitoring work.
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