作者单位: | MO Xuanxue1,2,DONG Guochen1,2,3,ZHAO Zhidan1,2,GUO Tieying1,WANG Liangliang1 and CHEN Tao1 1 State Key Laboratory of Geo-Processes and Mineral Resources,China University of Geosciences,Beijing 100083; 2 School of Earth Science and Resources,China University of Geosciences,Beijing 100083 3 Heibei Bureau of Geology and Mineral Exploration and Development,Shijiazhuang,Hebei 050081 |
摘 要: | 1 IntroductionIt is widely accepted that the collision of India withEurasia proceeded from "soft" to "hard" phases between c.65-70 Ma and c. 45 Ma (Yin and Harrison, 2000; Flower etal., 2001; Dong, 2002; Mo et al., 2003; Zhou et al., 2004,and references therein). Obviously, it is important tounderstand what kind of process took place at the depth ofthe Tibetan Plateau and its timing and geodynamicenvironment responding to the India-Eurasia continentalcollision. The giant Gangdise granito…
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