镁铁-超镁铁质岩成岩成矿过程中的锂同位素地球化学：回顾与展望

肖燕; 潘旗旗; 唐冬梅; 毛亚晶; 田世洪; 陈晨; 苏本勋; 刘霞

doi:10.3799/dqkx.2021.111

Volume 46 Issue 12

Dec. 2021

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Article Navigation > Earth Science > 2021 > 46(12): 4334-4345

Xiao Yan, Pan Qiqi, Tang Dongmei, Mao Yajing, Tian Shihong, Chen Chen, Su Benxun, Liu Xia, 2021. Retrospects and Prospects on Li Isotope Geochemistry during Petrogenesis and Mineralization of Mafic-Ultramafic Rocks. Earth Science, 46(12): 4334-4345. doi: 10.3799/dqkx.2021.111

Citation:

Xiao Yan, Pan Qiqi, Tang Dongmei, Mao Yajing, Tian Shihong, Chen Chen, Su Benxun, Liu Xia, 2021. Retrospects and Prospects on Li Isotope Geochemistry during Petrogenesis and Mineralization of Mafic-Ultramafic Rocks. Earth Science, 46(12): 4334-4345. doi: 10.3799/dqkx.2021.111

Citation:

Xiao Yan, Pan Qiqi, Tang Dongmei, Mao Yajing, Tian Shihong, Chen Chen, Su Benxun, Liu Xia, 2021. Retrospects and Prospects on Li Isotope Geochemistry during Petrogenesis and Mineralization of Mafic-Ultramafic Rocks. Earth Science, 46(12): 4334-4345. doi: 10.3799/dqkx.2021.111

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Retrospects and Prospects on Li Isotope Geochemistry during Petrogenesis and Mineralization of Mafic-Ultramafic Rocks

doi: 10.3799/dqkx.2021.111

Xiao Yan^{1, 2
,
,},
Pan Qiqi^{1, 2, 3},
Tang Dongmei^{2, 4},
Mao Yajing^{2, 4},
Tian Shihong⁵,
Chen Chen⁶,
Su Benxun^{2, 3, 4},
Liu Xia^{2, 3, 4}

1.
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2.
Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing 100029, China
3.
University of Chinese Academy of Sciences, Beijing 100049, China
4.
Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
5.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
6.
Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510460, China

Received Date: 2021-04-30
Publish Date: 2021-12-15

Abstract

Abstract

In-situ Li isotope geochemistry has been better utilized to trace many complex processes including fractional crystallization, crust contamination and melt/fluid-mineral reaction during the petrogenesis and mineralization of mafic-ultramafic rocks. This study summarizes the major progresses in Li isotope geochemistry during petrogenesis and mineralization of mafic-ultramafic intrusions based on case studies. Firstly, the Li isotope study of Yellow Hill Alaskan-type intrusion reveal Li isotope fractionation during magma differentiation. Secondly, the studies on ophiolites from Turkey and Tibet indicate that Li isotope systematics have potential to constrain genesis of ophiolitic mantle section and evolution of chromitites. Thirdly, the Li isotope study of the ultramafic zone of the Stillwater complex demonstrates that hydrous fluids constrained mineral composition and acted as a critical medium of chemical exchange between minerals in the chromitites. Finally, Li isotope fractionation behavior in the formation of magmatic Ni-Cu sulfide deposits has been investigated.
- Li isotope,
- mafic-ultramafic intrusion,
- mineralization,
- fractional crystallization,
- melt/fluid-mineral reaction,
- geochemistry

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References(48)

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Retrospects and Prospects on Li Isotope Geochemistry during Petrogenesis and Mineralization of Mafic-Ultramafic Rocks

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