Zircon U–Pb Dating and Geochemistry of the Linong Granitoid and Its Relationship to Cu Mineralization in the Yangla Copper Deposit,Yunnan, China |
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Authors: | Xi‐An Yang Jia‐Jun Liu Da‐Peng Li De‐Gao Zhai Long‐Bo Yang Si‐Yu Han Huan Wang |
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Affiliation: | 1. State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences, , Beijing, China;2. Chinese Academy of Geological Sciences, , Beijing, China |
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Abstract: | The Yangla copper deposit (Cu reserves: 1.2 Mt) in the Jinshajiang–Lancangjiang–Nujiang region in China is spatially associated with the Linong granitoid. Zircon U–Pb dating shows the granitoid formed at 234.1 ± 1.2 to 235.6 ± 1.2 Ma, and the KT2 ore body of the deposit yields a molybdenite Re–Os model age of 230.9 ± 3.2 Ma. The ages of mineralization and crystallization of the granitoid are identical within the measurement uncertainties, suggesting the Yangla deposit is genitically related to the Indosinian Linong granitoid. |
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Keywords: | Cu mineralization geochemistry granitoid Yangla copper deposit zircon U– Pb dating |
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