THE PRELIMINARY RESULTS OF MEASURING THE CRUSTAL DEFORMATION
IN QINGHAI-TIBET AREA USING GPS TECHNIQUE
Zhu W.Y., Xiong Y.Q., Cheng Z.Y., Xu H.G.
Shanghai Observatory, Chinese Academy of Science, 80 Nandan Road,
Shanghai 200030, P.R.China
GPS repetition measurement data in Qinghai-Tibet area in 1992 and 1994 have
been processed using SHAnghai observatory Gps Analysis Program (SHAGAP).
Based on the preliminary results given in this paper, several conclusion
can be arrived:
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1.
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At present, the relative accuracy of measuring baseline is better than
10ppb, and near 1ppb using GPS technique, it is possible to obtain a
reliable information about large scale crustal horizontal motion from the
periodic repetition measurements for no long time.
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2.
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It is first time to get the reliable result of large scale crustal
movement in China. These results are also the first time to give the
direct observed evidence to support the opinion that the main force source
to effect the motion of chinese continental crust is from the northward
propulsion of India plate. From the results, it also gives the evidence
to maintain the conclusion that the effect of the propulsion to crustal
motion of Qinghai-Tibet area is reduced from south to north.
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3.
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The result shows that the diamond block surrounded by the fracture from
Jingsha river to Hong river and other fractures from south to north in
southwest area of China , has an obvious southward strike slip movement,
that coincides with the motion model which comes from the geological or
geophysical data.