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《Acta Geosicientia Sinica》 1990-02
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NEW PALEOMAGNETIC RESULTS FROM YADONG- GOLMUD GEOSCIENCE TRANSECT AND A PRELIMINARY STUDY ON THE MODEL OF TERRANES EVOLUTION IN QINGHAI-XIZANG PLATEAU

Dong Xuebin Wang ZhongminTan Chengze Yang HuixinCheng Liren Zhou Yaoxiu Changchun College of Geology. Chinese University of Gcllogy(Beijing). Center of Acrogeophysical Remote Sensing, Ministry of Geology and Mineral Resources.  
Based on 29 sets of new paleomagnetic data from Paleozoic and Mesoz-oic main terranes in Xizang plateau and data of other writers. Some geological problems related to Xizang plateau, such as paleogeographic distributions, boundary between the terranes, collision time of terranes, active tectonic and swell mechanism, etc., have been analyzed and discussed, and the terranes evolution pattern has also tentatively been established. The pattern is that Himalaya, Gandise, Qiangtag and Kunlun terranes had been located in sourthern latitude during Paleozoic era. Overall, Xizang plateau has shown a tendency to move from south to north since Paleozoic era and Qiangtag and Bayanhar terrane had been accreted to southern and northern Kunlun terr-ane from late Triassic epoch to early Jurassic epoch, Gandise terrane to Qiangtang terrane from late Jurassic epoch to early Cretaceous epoch, and Himalaya to Gangdise terrane from late Cretaceous epoch to early Paleog-ene period. Thus these terranes made a unified continent. It responds to the uninterrupted process of accretion of Eurasia. The important mechanism that Xizang Plateau swelled is an intensely intercontinent reduction produced by many terranes on northern Xizang after Cretaceous period.
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