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《Geological Journal of China Universities》 2005-03
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Spatial and Temporal Distribution and Characteristics of Granitoids in the Gangdese,Tibet and Implication for Crustal Growth and Evolution

MO Xuan-xue~1,2 , DONG Guo-chen~2, ZHAO Zhi-dan~1,2 , ZHOU Su~1,2WANG Liang-liang~2, QIU Rui-zhao~3, ZHANG Feng-qin~2(1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083,China; 2. School of Earth Science and Resources, China University of Geosciences, Beijing 100083,China; 3. Developing and Research Center, Chinese Geological Survey, Beijing 100037,China)  
Granites are important components in the continents, and also closely related to mineral resources. Granites take c.12% of the total area of Tibetan territory and about 80% (in area) of them are distributed in the Gangdese magmatic belt. Spatially, the Gangdese granitoid belt consists of three zones, i.e., north, middle and south zones, as a result of the evolution of Neo-Tethyan Bangong Co-Nujiang ocean and Yarlung Zangbo Ocean. Temporally, the tectono-magmatic events in the Tibetan Plateau and the Gangdese can be divided into three stages: Pre-collisional (65 Ma), syn-collisional (65~45 Ma) and post-collisional ( 45Ma). Nd and Sr isotopes of granitoids in the Gangdese provide a hint for understanding the crust growth and evolution. Most of granites in southern Gangdese have positive values of ε_Nd(t) (+1.64~+5.21) and young Nd model ages t_DM(500 Ma), showing characteristics of the juvenile crust. It implies that the mantle material played a significant role in granite petrogenesis. Granites in middle and northern Gangdese, however, are characterized by negative ε_Nd(t) (-5.3~-17.3)and relatively older t_DM, 1.2 Ga and 2.0~2.5 Ga, implying a Neo- and Paleo-Proterozoic basement. Crustal material played a major role in granite petrogenesis for the latter case.
【Fund】: 国家重点基础研究计划(2002CB412600)项目;; 国家自然科学基金项目(40172025;40103003;49802005;49772107);; 国土资源部西藏专项计划(2003009)项目的资助。
【CateGory Index】: P588.121
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