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KANG Lei, LIU Liang, CAO Yu-ting, WANG Chao, YANG Wen-qiang, ZHU Xiao-hui. 2011: Geochemistry, zircon LA-ICP-MS U-Pb ages and Hf isotopes of Hongliugou moyite from north Altyn Tagh tectonic belt. Geological Bulletin of China, 30(7): 1066-1076. DOI: 10.12097/gbc.20110709
Citation: KANG Lei, LIU Liang, CAO Yu-ting, WANG Chao, YANG Wen-qiang, ZHU Xiao-hui. 2011: Geochemistry, zircon LA-ICP-MS U-Pb ages and Hf isotopes of Hongliugou moyite from north Altyn Tagh tectonic belt. Geological Bulletin of China, 30(7): 1066-1076. DOI: 10.12097/gbc.20110709
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Geochemistry, zircon LA-ICP-MS U-Pb ages and Hf isotopes of Hongliugou moyite from north Altyn Tagh tectonic belt

  • State Key Laboratory of Continental Dynamics/Department of Geology, Northwest University, Xi'an 710069, Shaanxi, China; 2. Xi′an Institute of Geology and Mineral Resources,China Geological Survey, Xi′an 710054, Shaanxi, China

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  • Hongliugou moyite outcropped in western Hongliugou-Lapeiquan complex belt belongs to high K cal-alkaline granites, characterized by SiO2>69.0%, Al2O3>13.0%, (K2O+Na2O)>7.0%, K2O/Na2O>1, 10.4, and hence this age can be regarded as the formation age of the moyite. Combined with regional geological characteristics, the authors consider that the formation of the rock was related to the subduction of the oceanic crust, with the tectonic setting being continental margin arc.
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