Geochronologic Constraints on the Magmatic Underplating of the Gangdisê Belt in the India-Eurasia Collision: Evidence of SHRIMP II Zircon U-Pb Dating

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Geochronologic Constraints on the Magmatic Underplating of the Gangdisê Belt in the India-Eurasia Collision: Evidence of SHRIMP II Zircon U-Pb Dating
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1 Introduction Mo et al. (2005) determined that magma mixing and mingling took place extensively in the Gangdisê magmatic belt around 50 Ma, and argued that magma mixing was genetically related to underplating of mantle-derived magmas beneath that belt. Underplating, as one of the major mechanisms for crustal growth, can occur in the environments of convergent plate boundaries, subduction and collision zones, and in intra-plate settings such as continental flood basalt provinces (Wilson, 19…

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DONG Guochen, MO Xuanxue, ZHAO Zhidan, GUO Tieying, WANG Liangliang, CHEN Tao State Key Laboratory of Geological Processes, Mineral Resources, China University of Geosciences, Beijing School of Earth Science, Resources, China University of Geosciences, Beijing, E-mail: moxx@cugb. edu. cn Hebei Bureau of Geology, Mineral Exploration, Development, Shijiazhuang, Hebei .2005. Geochronologic Constraints on the Magmatic Underplating of the Gangdisê Belt in the India-Eurasia Collision: Evidence of SHRIMP II Zircon U-Pb Dating[J]. Acta Geologica Sinica(),79(6):

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