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SHANG Haijun, CHEN Weimin, ZHANG Yaoxuan, et al. Zircon U-Pb Dating of Diorite from the Keyinbulake Cu-Zn Deposit in Altay, Xinjiang and Its Geological Implications[J]. Northwestern Geology, 2017, 50(4): 59-69.
Citation: SHANG Haijun, CHEN Weimin, ZHANG Yaoxuan, et al. Zircon U-Pb Dating of Diorite from the Keyinbulake Cu-Zn Deposit in Altay, Xinjiang and Its Geological Implications[J]. Northwestern Geology, 2017, 50(4): 59-69.
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Zircon U-Pb Dating of Diorite from the Keyinbulake Cu-Zn Deposit in Altay, Xinjiang and Its Geological Implications

  • 1. Geological Prospecting Fund Project Management Center of Xinjiang Uygur Autonomous Region, Urumqi 830002, Xinjiang, China;

  • 2. Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography of Chinese Academy of Sciences, Urumqi 830011, Xinjiang, China;

  • 3. Xinjiang Laboratory of Mineral Resources and Digital Geology, Urumqi 830011, Xinjiang, China

More Information
  • Received Date: March 31, 2016
  • Revised Date: July 09, 2017
  • Available Online: July 28, 2022
  • Published Date: December 04, 2017
    Graphical Abstract
    • Abstract
  • The Keyinbulake copper-zinc deposit is located at Chonghuer volcanic-sedimentary basin in Southern Altay. Granite pluton was exposed widely in this deposit,where the ore body occurred in the exocontact zones between granite and Upper Silurian-Lower Devonian Kangbutiebao Formation. In the underground mining process, there are geological phenomena of the diorite vein interspersed with copper and zinc ore bodies and granite. Zircon LA-MC-ICP-MS U-Pb dating of diorite has yielded a weighted average age of 262.0±2.1 Ma (MSDW=4.6), showing that the magmatic activitytook place in Middle-Late Permian. Combine with geological characteristic and the age of monzonitic granite, it's confined taht the Keyinbulake copper-zinc deposit was formed in the Early-Middle Permian, with an age of appreciably 278~262 Ma.
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    • References (87)
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    TENG Jia-xin, WANG Qing-ming. 2006: Major Ore Deposits in Altay Metallogenic Zone and Propecting Areas. Northwestern Geology, 39(2): 17-33.

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