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Metallogenic Province Derived from Mantle Sources: Nd, Sr, S and Pb Isotope Evidence from the Central Asian Orogenic Belt |
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| Authors: | Hong Dawei Wang Shiguang Xie Xilin Zhang Jisheng Wang Tao |
| Institution: | aInstitute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037, China bDepartment of Geology, Peking University, Beijing 100871, China cInstitute of Mineral Deposits, Chinese Academy of Geological Sciences, Beijing 100037, China |
| Abstract: | The Central Asian Orogenic Belt (CAOB) is one of the most important regions for Cu, Au and polymetallic and rare metallic (Li, Be, Nb, Ta) mineralization over the world. Most of the ore deposits in the CAOB are closely associated with granitoids. Available Sr, Nd, S and Pb isotopic data indicate that the metallogenic epoch and sources of the mineral deposits in the CAOB are consistent with that of the regional granites. Available data suggest that mantle sources could have played an important role in the Paleozoic to Mesozoic mineralization in the CAOB. |
| Keywords: | Central Asian Orogenic Belt metallogenic province mantle source Sr Nd S and Pb isotopes |
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