云母和电气石矿物化学特征对西昆仑大红柳滩地区伟晶岩型锂矿化的指示

夏永旗; 庹明洁; 李诺; 祁冬梅; 加纳提古丽·吾斯曼; 王慧慧; 王文波; 李婷; 邰宗尧

doi:10.3799/dqkx.2023.213

Volume 49 Issue 3

Mar. 2024

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Article Navigation > Earth Science > 2024 > 49(3): 922-938

Xia Yongqi, Tuo Mingjie, Li Nuo, Qi Dongmei, Jianatiguli Wusiman, Wang Huihui, Wang Wenbo, Li Ting, Tai Zongyao, 2024. Mineral Characteristics of Mica and Tourmaline and Geological Implication for the Pegmatite-Type Lithium Mineralization, Dahongliutan Area, West Kunlun. Earth Science, 49(3): 922-938. doi: 10.3799/dqkx.2023.213

Citation:

Xia Yongqi, Tuo Mingjie, Li Nuo, Qi Dongmei, Jianatiguli Wusiman, Wang Huihui, Wang Wenbo, Li Ting, Tai Zongyao, 2024. Mineral Characteristics of Mica and Tourmaline and Geological Implication for the Pegmatite-Type Lithium Mineralization, Dahongliutan Area, West Kunlun. Earth Science, 49(3): 922-938. doi: 10.3799/dqkx.2023.213

Citation:

Xia Yongqi, Tuo Mingjie, Li Nuo, Qi Dongmei, Jianatiguli Wusiman, Wang Huihui, Wang Wenbo, Li Ting, Tai Zongyao, 2024. Mineral Characteristics of Mica and Tourmaline and Geological Implication for the Pegmatite-Type Lithium Mineralization, Dahongliutan Area, West Kunlun. Earth Science, 49(3): 922-938. doi: 10.3799/dqkx.2023.213

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Mineral Characteristics of Mica and Tourmaline and Geological Implication for the Pegmatite-Type Lithium Mineralization, Dahongliutan Area, West Kunlun

doi: 10.3799/dqkx.2023.213

Xia Yongqi^{1, 2
,
,},
Tuo Mingjie²,
Li Nuo^{2, 3, 4
,
,
,},
Qi Dongmei¹,
Jianatiguli Wusiman²,
Wang Huihui¹,
Wang Wenbo¹,
Li Ting⁵,
Tai Zongyao⁵

1.
Laboratory of Continental Dynamics and Metallogenic Prediction of Central Asian Orogenic Belt, Xinjiang University, Urumqi 830049, China
2.
Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
3.
Key Laboratory of Ecological Security and Sustainable Development of Arid Areas, State Key Laboratory of Desert and Oasis Ecology, Chinese Academy of Sciences, Urumqi 830011, China
4.
Xinjiang Laboratory of Mineral Resources and Digital Geology, Urumqi 830011, China
5.
Beijing Research Institute of Uranium Geology, Beijing 100029, China

Received Date: 2023-07-24
Available Online: 2024-04-12
Publish Date: 2024-03-25

Abstract

Abstract

The Dahongliutan two-mica granite is considered as parental rock to the adjacent pegmatite-type lithium deposits such as Bailongshan. To constrain the magmatic-hydrothermal evolution of granite and associated pegmatites, we selected the penetrative minerals, mica and tourmaline, from two-mica granite and pegmatite with different degrees of mineralization, for backscattering observation (BSE) and electron probe microanalysis (EPMA). In the two-mica granite (Ms₁) and muscovite-microcline pegmatite (Ms₂), the muscovite is homogeneous, with limited chemical variations. In muscovite-albite-spodumene pegmatite, the muscovite (Ms₃) incorporates much higher Li (Li₂O up to 4.68%) and F (up to 6.47%) in comparison to Ms₁ and Ms₂. There are additional Li-bearing phengite, zinnwaldite and lepidolite that have replaced muscovite. Tourmalines from two-mica granite (Tur₁) and muscovite-microcline pegmatite (Tur₂) belong to alkaline schorl, while those from spodumene pegmatite (Tur₃) are alkaline elbaite. Compared to alkaline schorl, alkaline elbaite is enriched in SiO₂, Al₂O₃, Li₂O, but depleted in TiO₂, MgO and CaO. The textural and compositional features of mica and tourmaline reveal that the two-mica granite and muscovite-microcline pegmatite were formed by magmatic process, without lithium mineralization. By contrast, muscovite-albite-spodumene pegmatite was formed during the magmatic-hydrothermal transition, where lithium was significantly enriched, and numerous lithium-rich minerals such as spodumene, lithium-rich polysilicon muscovite, Li-bearing phengite, zinnwaldite, lepidolite and elbaite, were precipitated. Accordingly, we propose that the magmatic-hydrothermal transition is of great significance for lithium mineralization. In pegmatite-type deposits, the presence of elbaite and lepidolite indicates high degree of magmatic evolution.
- rare-metal pegmatite,
- mica,
- tourmaline,
- magmatic-hydrothermal evolution,
- mineral composition characteristics,
- mineralogy,
- petrology

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References(103)

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