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《Seismology and Geology》 1988-04
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CRETACEOUS PALEOMAGNETIC RESULTS FROM HONGHE FAULT ZONE AND GEOLOGIC-TECTONIC EVOLUTION OF THE QINGHAI-TIBET PLATEAU

Cheng Gou-liang, Bai yun-hong, Li su-ling and Sun yu-hang(Institute of Geology, State Seismological Bureau)  
Paleomagnetic results from the both sides of Honghe fault zone have shown that the Yangzi block has been united with the Qiangtang terrane since Cretaceous. The Qinghai-Tibet Plateau was a tectonic composite consisting of four terranes named Kunlun, Qiangtang, Lhase and Himalayans from north to south. These terranes were the component parts of Laurasian, Cathaysia and Gondwana, respectively, in Late Paleozoic, having different history of development. The collision and matching of the Lhase terrane with the Qiangtang terrane have caused the formation of the tectonic framework of Eurasian plate. On the other hand, the collision and matching of himalayan terrane and Indian plate have given rise to the uplifting of Qinghai-Tibet Plateau, which caused sinistral strike-slip movement of the blocks of Eurasian plate along the pre-existing faults. This process continued till now.
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