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《Earth Science-Journal of China University of Geosciences》 1983-01
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ON THE GEOTEC TONIC UNITS OF XIZANG (TIBET) REGION

Wang Hongzhen  
The geotectonic units of Xizang recognized in this paper are Ⅰ.Qiang-tang massif, whose basement is represented by the metamorphic recks near Mayigang, which is covered by non-metamcrphic Devonian sediments. The age of the rnetamorphic series is presumably Precambrian,but also possibly Early Palaeozoic.Ⅱ.Gangdise massif,basement represented by the Precambrian Nyainoentangllla Group, which is covered by platform type Ordovician and Silurian near Hainza . Ⅲ. Himalaya massif, representing the Middle and Upper Proterozoic belt on the northern border of the Indian craton. These massifs are separated from each other by crustal consumption zones or geo-sutures, and by fold zones of various ages. The northernmost geosuture, the Xiugou Maxin convergent crustal consurnpton zone, was closed in the early Indosinian, when the opposite continental margins of North China and Yangzze Platforms became coagulated. The Bangong Lake-Nujiang convergent zone separates the northern Qiangtang massif and the southern Gang-dise massif, and was coalesced in the Yanshaniaa. The southern geosuture, the Yarlung Zangbo , lies between the Gangdise and the Himalaya massifs and was closed in the Eoccne . This zcne , though important and magnificent, is however intracratonic in nature, as it lies within the scope of the complicated and dissociated continental margin tract cf the Gcndwana, and may therefore be called accretional crustal consumption zone. The subdivision of tectonic domains and development of the Tethys, especially the Gcndwana Eurasian boundary problem are also discussed. It is held that the actual boundary between the Gondwanan and the Eurasian continents should be considered in connection with the period when the configuration of Pangaca was most prominent and clear, i. e. from Late Carboniferous to Triussic, One of ihe characteristic features of the Eurasian continent in the Chinese part lies in its final consolidation and coagulation in the Indisinian, when the extensive triangular region of western Qinling and Bayan Har was uplifted and folded,and the Yangtze-Qiangtang tectonic domain, as it maybe called, became coalesced with the North China-Tarim continent.Thus,the Bayan Har represents the northern branch of the Tethys. The southern branch of the Tethys is the Yarlung Zangbo marine terrain,which came to existence through the openning between Gangdise and Himalaya in Permo Carboniferous, a nd was brought to a closure in Middle to Late Eocene.It constitutes the southern branch of the Tethys.The main part of the Tethys seems however to have been located bwtween the Gangdise and the Qiangtang,the scope of which may be delimited by the southern limit of distribution of the Permian Cathaysian flora, and the northern limit of distribution of the latest Carboniferous glacial deposits and cold water faunas. This marine terrain, which may well have began to exist since from Early Palaeozoic, has separated the Gondwana ani the Yangtze-Qiangtang tectonic domains, until Latr Jurassic to Early Cretaceous, when Gangdise and Qiangtang massifs were brought to collision of each other. A simplified outline map of Xizang and adjacent regions was prepared to show the tectonic setting of the different domains and units .
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