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《Chinese Journal of Geophysics》 1980-03
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CHARACTERISTICS OF THE GEOPHYSICAL FIELDS AND PLATE TECTONICS OF THE QINGHAI-XIZANG PLATEAU AND ITS NEIGHBOURING REGIONS

Teng Ji-wen Wang Shao-zhou Yao Zhen-xingXú Zhen-wǔ Zhu Zhi-wen Yang Bing-ping Zhou Wen-hu (Institute of Geophysics, A oademia Sinica)  
In this paper, we have collected all the avtilable data that are pertinent to the study of this region, such as the crust and upper mantle structures in the Qinghai-Xizang region, the distributions of the geomagnetic field elements, the results of aero-magnetic surveys, the palaeomagnetic pole wandering paths, gravity anomalies, geo-thermal activities, earthquake activities, fault plane solutions and other results of geophysical interests, and tries to discover the relationships between these features of the geophyaical field and plate tectonics.The preliminary results indicate that the northern boundary of the zone where Indian plate and Eurasian plate are in contact is Yarlung Zangbo River and the south-ern boundary is in the northern edge of Ganga plain. The Himalayan zone is a transitional belt whose width is about 300 km or so. Most of the large and small earthquakes occurring in this zone are of shallow foci. Only in the arcuate mountain system and at the vertices of the east and west area as well as at the turning points of the range that earthquakes of medium depths occurred. In this transitional zone, hot water activity is very strong and the gravity field is not in isostatic equilibrium.From the north of Yarlung Zangbo River to Damxung region, the crust is 70-73 km thick, but in the Himalayan region, the crustal thickness decreases to about 68-45 km and is upwarping towards the south. The crust is multilayered and there exists a low velocity layer in the lower crust. The fault plane solution shows that the fault is thrusting towards the south, the principal compressional stress axis being in general directing either N-S or NE and relating to the focal depth. It seems that the recent tectonic and earthquake activities gradually move towards the south reaching the great fault of the main boundary.In the north of Yarlung Zangbo, the focal depths of small earthquakes increase to-wards the south, but in the north of the Ganga plain it increases to the north. More-over, in the two places mentioned above some earthquakes of medium depths occur.Therefore, there are thrusting faults both on the southern and on the northern sides of Himalayan zone. In the Hindukush region, the plane of the foci of the medium deep earthquakes dip towards to north in the Pamir zone; they dip towards the south. So the plane of the foci forma "V" shaped region.The stress and energy of the tectonic motion in the plateau and its adjacent regions have not been exhausted at all, and had direct influence on the earthquake activities and structures of the provinces of Sichuan, Shaanxi, Gansu and Ningxia.
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