Timing of Magma Mixing in the Gangdise Magmatic Belt during the India-Asia Collision: Zircon SHRIMP U-Pb Dating
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P542.3;P597.3

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    Abstract:

    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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MO Xuanxue, DONG Guochen, ZHAO Zhidan, GUO Tieying, WANG Liangliang, CHEN Tao State Key Laboratory of Geo-Processes, Mineral Resources, China University of Geosciences, Beijing School of Earth Science, Resources, China University of Geosciences, Beijing Heibei Bureau of Geology, Mineral Exploration, Development, Shijiazhuang, Hebei .2005. Timing of Magma Mixing in the Gangdise Magmatic Belt during the India-Asia Collision: Zircon SHRIMP U-Pb Dating[J]. Acta Geologica Sinica(),79(1):

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