Geologicial Feature and Chronology Study of Kangxiwar Beryl-Bearing Muscovite Pegmatite in Weste Kunlun Orogen, Xinjiang

ZHANG Ze; LIANG Ting; FENG Yonggang; YANG Xiuqing; LI Kan; DING Kun; WANG Yiqian

doi:10.19751/j.cnki.61-1149/p.2019.01.007

Northwestern Geology > 2019 > 52(1): 75-88. > DOI: 10.19751/j.cnki.61-1149/p.2019.01.007

ZHANG Ze, LIANG Ting, FENG Yonggang, et al. Geologicial Feature and Chronology Study of Kangxiwar Beryl-Bearing Muscovite Pegmatite in Weste Kunlun Orogen, Xinjiang[J]. Northwestern Geology, 2019, 52(1): 75-88. DOI: 10.19751/j.cnki.61-1149/p.2019.01.007

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Geologicial Feature and Chronology Study of Kangxiwar Beryl-Bearing Muscovite Pegmatite in Weste Kunlun Orogen, Xinjiang

1. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China;
2. Laboratory of Mineralization and dynamics, Chang'an University, Xi'an 710054, Shaanxi, China;
3. Xi'an Geological Survey Center, China Geological Survey, Xi'an 710054, Shaanxi, China

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Received Date: April 12, 2018
Revised Date: September 11, 2018
Available Online: July 28, 2022
Published Date: March 04, 2019

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Abstract

Abstract

The Kangxiwar-Dahongliutan pegmatite field is an important area with abundant LCT family rare-metal pegmatites in the West Kunlun Orogen. The Kangxiwar beryl-bearing muscovite pegmatite and Dahongliutan spodumene pegmatites are the representative beryllium deposit and lithium deposit, respectively in this pegmatite field. Previous studies were focused on the Dahongliutan granitic pluton and lithium deposits that were formed at 220~210Ma in the Dahongliutan area. Nevertheless, there are few studies on the Kangxiwar pegmatite. Based on the field observation, this study summarizes geological features of the Kangxiwar beryl-bearing muscovite pegmatite and presents the latest zircon U-Pb dating results. According to our dating results, the crystallization age of the Kangxiwar beryl-bearing muscovite pegmatite is (209±4.4)Ma, which is consistent with the ages of the Dahongliutan spodumene pegmatite and Dahongliutan granitic pluton, indicating that theberyl-bearing muscovite pegmatite, spodumene pegmatites and granite were likely the products of the same magmatic event. In addition, the zircon from the Kangxiwar pegmatite also has recorded a hydrothermal event around 200Ma and a metamorphic event at~160Ma. Based on muscovite ⁴⁰Ar-³⁹Ar dating, previous studies suggested that the age of the Kangxiwar pegmatite is 185~156 Ma. The reported ⁴⁰Ar-³⁹Ar age is significantly younger than the crystallization ages of the beryl-bearing muscovite pegmatite, granitic pluton and spodumene pegmatites that had been obtained using U-Pb dating of zircon, cassiterite and columbite, but it is comparable to the age of the metamorphic zircon in this study, which suggested that the muscovite ⁴⁰Ar-³⁹Ar isotope system of the Kangxiwar pegmatite underwent thermal disturbance due to the metamorphic event in the Kangxiwar-Dahongliutan pegmatite field.
- west Kunlun orogen,
- Kangxiwar-Dahongliutan pegmatite field,
- beryl-bearing pegmatite,
- zircon U-Pb dating

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References (51)

References

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Geologicial Feature and Chronology Study of Kangxiwar Beryl-Bearing Muscovite Pegmatite in Weste Kunlun Orogen, Xinjiang

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