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《EARTH SCIENCE》 1996-01
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EXPOSE THE UPLIFT OF QINGHAI-TIBET PLATEAU: YADONG-GOLMUD GEOSCIENCE TRANSECT IN QINGHAI-TIBET PLATEAU,CHINA

Wu Gongjian Xiao Xuchang Li Tingdong (Chinese Academy of Geological Sciences,Beijing 100037)  
Geological,geophysical and geochemical data have been combined to give a general picture of the evolution of the lithosphere along the Yadong-Golmud geoscience transect.The Qinghai-Tibet Plateau,composed of six distinct terranes,is heterogeneous both laterally and vertically and its tectonic fabrics vary between the terranes.The shortening,thickening and uplift of the crust have been caused by a variety of factors,including compression due to northward movement of the Indian plate,resistance to such movement by the material in the Qaidam Basin region,and isostatic effects on both the crust and mantle.Thermal activity in the mantle is less important than that in the crust.The Himalayan orogenic belt has some important features that distinguish it from the Andean and Alpine orogenic belts.
【CateGory Index】: P542.2
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