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《Chinese Journal of Geophysics》 1980-03
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THE AVERAGE STRESS FIELDS OF ZHAMO AND DAMXUNG REGIONS IN THE XIZANG PLATEAU

Zhang Li-min Shu Pei-yi Yang Bing-ping Zhang Zhi-he(Institute of Geophysics, Academia Sinica)  
The average stress fields of Zhamo and Damxung regions in Xizang Plateau are obtained by smoothing the first motion patterns from the regional seismological ob-servation data. The results are as follows:1. The compressional axes in Damxung region and part A of Zhamo region are roughly in the north-south direction. The angles of elevation of these axes are small, being 23 degrees and 14 degrees respectively. This indicates that the interaction be-tween two plates is dominantly compression.2. In part B of Zhamo region, the compressional axis is in the east-west direc-tion with an angle of elevation about 51 degrees. This seems to correspond to the underthrusting condition.Such a result is basically in accord with the model of collision between the Indian plate and the Eurasian plate and agrees with the fault plane solutions of the major earthquakes which occurred in that region. This implies that all earthquakes whether large or small are all controlled by the- plate movement.
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