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《长春地质学院学报》 1986-03
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CHARACTERISTICS OF THE RECENT TECTONIC STRESS FIELD OF PANXI RIFT VALLEY ZONE AND ITS VICINITY

Fu Weizhou Wu Yubao(Changchun College of Geology) (Geological Bureau of Sichuan Province)  
We have discussed the recent tectonic movement in Panxi area in the light of fault plane solution of 124 earthquakes(M≥ 4 )occurring in the area in almost the past thirty years, and measurements of earth stress and horizontal deformation. Results show that the stress stats in Panxi rift valley zone changed from the former ten-sional to the present compressional and shear.The rift is now withering.The direction of the main compressive stress in most partseast to Xianshuihe fault zone and Panxi rift valley is NWW,but in the West region,it is deflected clockwise southward and the massifs on both sides make relative sinistral shear movement.The recent tectonic stress field is nearly horizontal,
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