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LIN Xinwang, ZHANG Yafeng, WANG Xing, et al. Zircon U-Pb Dating of the Muzitawu Plutons from the Friendship Peak Region in Altay, Xinjiang and Its Geological Significance[J]. Northwestern Geology, 2017, 50(3): 83-91.
Citation: LIN Xinwang, ZHANG Yafeng, WANG Xing, et al. Zircon U-Pb Dating of the Muzitawu Plutons from the Friendship Peak Region in Altay, Xinjiang and Its Geological Significance[J]. Northwestern Geology, 2017, 50(3): 83-91.
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Zircon U-Pb Dating of the Muzitawu Plutons from the Friendship Peak Region in Altay, Xinjiang and Its Geological Significance

  • Shaanxi Center of Geological Survey, Xi'an 710068, Shaanxi, China

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  • Received Date: March 07, 2017
  • Revised Date: May 16, 2017
  • Available Online: July 28, 2022
  • Published Date: September 04, 2017
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    • Abstract
  • Large quantities of granites are developed in the southern margin of Altay orogenic belt. The previous studies have focused on the formation age and structural setting of the granites from the eastern section of Altay orogenic belt, but the research its western section is still limited.Muzitawu Plutons are located in Muzitawu area of Western Friendship Peak, Burqin County, Altay, Xinjiang, which are mainly consist of biotite granite, porphyritic biotitesyenogranite and muscovite syenogranite.In these plutons, the pegmatite veins are very developed, with rare metal mineralization. The LA-ICP-MS zircon U-Pb method was used to study the chronology of porphyritic biotitesyenogranite, and the zircon 206Pb/238U weighted average age of the plutons is (198.3±3.8)Ma (MSWD=2.0), indicating that these plutons were formed in early Jurassic. This age is basically in line with the metallogenic epoch of pegmatite vein-type rare metals in the eastern section of Altay orogenic belt, which provides a chronological restriction for the study on the mineralization epoch of rare metal-muscovite-gemstone relating to pegmatite in this area.
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