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《Chinese Journal of Geophysics》 1994-02
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DISCOVERY AND EVIDENCE OF THE FIFTH SUTURE ZONE OF QINGHAI-XIZANG PLATEAU

PAN YU-SHENG (Lab. of Lithosphere Tectonic Evolution, Institute of Geology, Academia Sinica, Beijing 100029)  
Kunlun mountain was believed the typical illustration of Hercynian or Indo-Sinian orogens previous. Since 1987, supported by both the Chinese Academy of Sciences and National Natural Science Foundation of China, a multi-disciplinary scientific expedition was conducted in Karakorum and Kunlun mountain ranges by Integrated Scientific Expeditional Team to Qinghai-Xizang plateau, Chinese Academy of Sciences, which obtained much new information. This paper is carried out on the basis of the results of this expedition. There was an ocean called the Proto-Tethys in western Kunlun, which was blocked and opened on southern Laurasia continental basements and developed mainly from Sinian to Ordovician(about 800-450Ma). The Proto-Tethys was closed by the Caledonian orogeny and formed now a remnant of Kudi-Shubashi suture zone which called fifth suture zone of Qinghai-Xizang plateau. Therefore geological history and tectonic evolution of Qinghai-Xizang plateau are clear.
【Fund】: “七五”期间国家基金
【CateGory Index】: P548.2
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