| Ore Genesis and Tectonic Setting of Laojiagou Porphyry Mo Deposit, Inner Mongolia (Northern China): Evidence from Ore Geology, Fluid Inclusions, H-O Isotopes, Zircon U-Pb Age and Whole-rock Geochemistry |
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| 作者姓名： | TANG Wenhao LI Jian WANG Keyong LI Shund CAI Wenyan LIU Hanlun WANG Yicun |
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| 作者单位： | 1 College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China,1 College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China,1 College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China；2 Key laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources of China, Changchun 130061, Jilin, China,1 College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China,1 College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China,1 College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China and 1 College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China |
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Accreted Terranes in the Paleo‐Asian Ocean |
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| Authors: | TANG Wenhao LI Jian WANG Keyong LI Shund CAI Wenyan LIU Hanlun WANG Yicun |
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| Abstract: | Terrane accretion is considered to be one of the main contributors to the growth of continental crust (Stern and Scholl, 2010). Allochthonous terranes can be categorized into three general groups, including island arcs, seamounts (oceanic plateaus, submarine ridges), and continental fragments. The Central Asian Orogenic Belt (CAOB) is one of the largest and long‐lived accretionary collages on the globe, and is composed of numerous island arcs, and accretionary wedges, seamounts, and microcontinents associated with the growth and consumption of the Paleo‐Asian Ocean (Fig.1; ?engör et al., 1993; Windley et al., 2007; Xiao et al., 2015; Yang et al., 2015). |
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