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ZHENG Zhen, CHEN Yan-jing, DENG Xiao-hua, YUE Su-wei, CHEN Hong-jin. Muscovite 40Ar/39Ar dating of the BaiganhuW-Sn orefield, Qimantag, East Kunlun Mountains, and its geological implications[J]. GEOLOGY IN CHINA, 2016, 43(4): 1341-1352. DOI: 10.12029/gc20160419
Citation: ZHENG Zhen, CHEN Yan-jing, DENG Xiao-hua, YUE Su-wei, CHEN Hong-jin. Muscovite 40Ar/39Ar dating of the BaiganhuW-Sn orefield, Qimantag, East Kunlun Mountains, and its geological implications[J]. GEOLOGY IN CHINA, 2016, 43(4): 1341-1352. DOI: 10.12029/gc20160419

Muscovite 40Ar/39Ar dating of the BaiganhuW-Sn orefield, Qimantag, East Kunlun Mountains, and its geological implications

Funds: 

China Geological Survey Project 1212011140056

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  • Author Bio:

    ZHENG Zhen, female, born in 1987, doctor, mainly engages in the study of mineral deposits, petrology and mineralogy; E-mail:tianchilian@163.com

  • Corresponding author:

    CHEN Yan-jing, male, born in 1962, professor, engages in the study of mineral deposits, oreforming regularity of orogenic belt; E-mail:yjchen@pku.edu.cn

  • Received Date: March 13, 2016
  • Revised Date: June 19, 2016
  • Available Online: September 25, 2023
  • The newly discovered Baiganhu W-Sn ore district in Qimantag of East Kunlun orogenic belt provides a key window to insight into the W-Sn mineralization in Northwest China. In this paper, the authors present results from the 40Ar/39Ar dating of two muscovite samples collected from the ore-bearing quartz veins in the Baiganhu W-Sn ore district, which yielded two 40Ar/39Ar plateau ages of 422.7 ±4.5 Ma and 421.8 ±2.7 Ma, respectively. These two samples also yielded consistent (within errors) isochronal and inverse isochronal ages of 424 ±15 Ma and 418 ±24 Ma, respectively, suggesting that the analytical results are reliable. The new plateau ages show that the mineralization occurred in the Late Silurian, associated with the tectonic-thermal events induced by the closure of Proto-Tethys. The post-subduction continental collision caused the formation of granitic magmas sourced from remelting of the metalliferous metamorphosed Proterozoic sediments. The W-Sn mineralization resulted by the hydrothermal fluids exsolved from the granitic magmas during their upward emplacement.

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