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《Chinese Journal of Geophysics》 1980-03
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THE DISTRIBUTION OF EARTHQUAKES FOCI AND PLATE MOTION IN THE QINGHAI-XIZANG PLATEAU

Huan Wen-lin Wang Su-yun Shi Zhen-liang Yan Jia-quan(Institute of Geophysics, State Seismological Bureau)  
In this paper, the data of focal depths of a alrge number of earthquakes which occurred recently in the Qinghai-Xizang plateau and its vicinity are analysed. We find that not only there are widely distributed shallow earthquakes in this region, but also there are regularly distributed intermediate shocks. These intermediate earth-quakes form three seismic zones in this region.The first zone stretches along the plate convergence zone. The planes of foci in the Hindukush and in the India-Burma mountain arc which are located in the two flanks of Indian subcontinent are north-dipping and east-dipping respectively toward Asian continent. But the planes of foci of intermediate earthquakes in the Indus and Yarlung Zangbo River convergence zone are all southward dipping. The second zone is located in the areas of the Pamir, the West Kunlun mountain and the northern margin of the Qaidam Basin. The planes of foci here are all south-dipping. The third zone is located in the southern margin of the Tianshan. The plane of foci is south-dipping too.If the above-mentioned inclined focal planes along which many intermediate earthquakes occurred, is taken as the subduction zone, then there are three south-dipping lithospheric subduction zones from the Himalayas to Tianshan. The existence of the three southward inclined lithospheric subduction zones implies that it was the Asian plate rather than the Indian plate which has been subducted.If we regard the depth of the subduction zone as the part disappeared in the mantle, then the Asian continental crust along the above three subduction zones has shortened at feast 300-700 kms since the India-Eurasia collision.The discontinuous distribution of the intermediate earthquake zones indicates recent activity of some strike slip faults. The large displacements of some strike slip faults show that the lateral movement between the blocks is closely related to the northward movement of the Indian plate.In the last part of this paper, we proposed a model on the origin of three south-dipping subduction zones in the Asian continent.
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