Test of Deep Seismic Reflection Profiling across Central Uplift of Qiangtang Terrane in Tibetan Plateau  

作　　者：卢占武 高锐 李秋生 贺日政 匡朝阳 侯贺晟 熊小松 管烨 王海燕 Klemperer S L 

机构地区：[1]Lithosphere Research Centre,Institute of Geology,Key Laboratory of Earthprobe and Geodynamics,Chinese Acdemy of Geological Sciences [2]Department of Geophysics,Stanford University

出　　处：《Journal of China University of Geosciences》2009年第2期438-447,共10页中国地质大学学报（英文版）

基　　金：supported by the National Natural Science Foundation of China (Nos. 40830316, 40874045 and 40704016);the Ministry of Science and Technology of China (Nos. SinoProbe-02, 2006DFA21340);the Ministry of Land and Resources of China (Nos. 2004-06, 200811021);the Open Fund of Key Laboratory of Geo-detection of China Uni-versity of Geosciences (Beijing) (No. GDL0603)

摘　　要：A test of deep seismic reflection profiling across the central uplift or metamorphic belt of the Qiangtang （羌塘） terrane, Tibet plateau, provides a first image of the crustal structure. Complex reflection patterns in the upper crust are interpreted as a series of folds and thrusts, and bivergent reflections in the lower crust may represent a convergence between the Indian and the Eurasian plates.A test of deep seismic reflection profiling across the central uplift or metamorphic belt of the Qiangtang （羌塘） terrane, Tibet plateau, provides a first image of the crustal structure. Complex reflection patterns in the upper crust are interpreted as a series of folds and thrusts, and bivergent reflections in the lower crust may represent a convergence between the Indian and the Eurasian plates.

关 键 词：Qiangtang terrane central uplift zone crustal structure test of deep reflection profiling convergent process. 

分 类 号：P548[天文地球—构造地质学]