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2021 Vol. 54, No. 3
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WANG Wei, WANG Jiaxin, MA Huadong, ZHU Bingyu, LIU Xianjun. 2021. Mineralization Age of the Karakorum Luobugaizi Large Lead-zinc Deposit: The Implication on Exploration of Tianshuihai-Karakorum Super-large Lead-zinc Deposits. Northwestern Geology, 54(3): 155-162. doi: 10.19751/j.cnki.61-1149/p.2021.03.012
Citation: WANG Wei, WANG Jiaxin, MA Huadong, ZHU Bingyu, LIU Xianjun. 2021. Mineralization Age of the Karakorum Luobugaizi Large Lead-zinc Deposit: The Implication on Exploration of Tianshuihai-Karakorum Super-large Lead-zinc Deposits. Northwestern Geology, 54(3): 155-162. doi: 10.19751/j.cnki.61-1149/p.2021.03.012
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Mineralization Age of the Karakorum Luobugaizi Large Lead-zinc Deposit: The Implication on Exploration of Tianshuihai-Karakorum Super-large Lead-zinc Deposits

  • 1. The Research Centerof Resource and Environment of Xinjiang, Urumuqi 830000, Xinjiang, China;

  • 2. The National 305 Project Office of Xinjiang, Urumuqi 830000, Xinjiang, China;

  • 3. Sichuan Xinli Geological Exploration Co., Ltd., Chengdu 610072, Sichuan, China

Received Date:  14 December 2020
Revised Date:  18 March 2021
    Abstract
  • The Western Kunlun-Karakorum is in the northern margin of the Qinghai-Tibet Plateau, belonging to the Tethyan tectonic domain. In recent years, the nonferrous metals exploration in this region has achieved significant breakthrough. Several large and super-large lead-zinc deposits have been discovered.Among them, the Luobugaizi large lead-zinc deposit, which is in the western section of the Tianshuihai-Karakorum nonferrous metals belt, has more than 1000,000 ton reserve.On the basis of the geological features the authors concluded that the deposit is a typical hydrothermal deposit related to the Cretaceous intrusive event, with the U-Pb age of (99.25±0.78) Ma, hence the Luobugaizi lead-zinc deposit was hydrothermal type. Through the comprehensive analysis, this paper concluded that the lead-zinc deposits were controlled by the Jurassic-Cretaceous sedimentary magmatic rocks. This metallogenic belt has great potential for the future mineral exploration.
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