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《Chinese Journal of Geophysics》 1981-02
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EXPLOSION SEISMIC STUDY FOR VELOCITY DISTRIBUTION AND STRUCTURE OF THE CRUST AND UPPER MANTLE FROM DAMXUNG TO YADONG OF XIZANG PLATEAU

Institute of Geophysics, Academia Sinica  
In order to study the layered structures and characteristics of the velocity distributions in the crust and upper mantle of the Xizang plateau region we have carried out explosions in the Lakes of Yarzhoyum, Pomu and Nam. Nine seismic records were obtained along a profile 430 km long in a nearly N-S direction.Six groups of phases of seismic waves through the crust and upper mantle in the area are observed which show different kinematic and dynamic properties.The result shows that the crust and upper mantle of Xizang plateau are stratified. Here the thickness of the sedimentary layer is from 4 to 5 km. The crustal structures along the two sides of Yarlung Zangbo river are different. The crustal thickness from the north of the river to Damxung region is from 70 to 73 km and the interfaces in the crust are essentially plane. Compared with that of the northern part, the crust of the southern part of the river is thinner. From the river to Yadong belt the crustal thickness is from 68 to 45 km. The crust of Xizang plateau consists also of high and low velocities layers. There is a low velocity layer in the lower crust and its thickness is 10 km, and its velocity 5.67 km/sec. A composite cross section and a model of the crust is given.The northern boundary of the collision zone of the two plates is quite clear cut and every layer in the crust is upwarping towards south. It shows that the formation of a thick crust and the uplift of the plateau are due to the results of a long period of compression, deformation, and crustal shortening by folding in a large scale.
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