华南幕阜山北缘含稀有金属伟晶岩成矿时代及成矿过程

李乐广; 王连训; 朱煜翔; 马昌前; 佘振兵; 曹亮; 冷双梁; 闫育荞

doi:10.3799/dqkx.2022.141

Volume 48 Issue 9

Sep. 2023

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Article Navigation > Earth Science > 2023 > 48(9): 3221-3244

Li Leguang, Wang Lianxun, Zhu Yuxiang, Ma Changqian, She Zhenbing, Cao Liang, Leng Shuangliang, Yan Yuqiao, 2023. Metallogenic Age and Process of Rare Metal-Bearing Pegmatites from the Northern Margin of Mufushan Complex, South China. Earth Science, 48(9): 3221-3244. doi: 10.3799/dqkx.2022.141

Citation:

Li Leguang, Wang Lianxun, Zhu Yuxiang, Ma Changqian, She Zhenbing, Cao Liang, Leng Shuangliang, Yan Yuqiao, 2023. Metallogenic Age and Process of Rare Metal-Bearing Pegmatites from the Northern Margin of Mufushan Complex, South China. Earth Science, 48(9): 3221-3244. doi: 10.3799/dqkx.2022.141

Citation:

Li Leguang, Wang Lianxun, Zhu Yuxiang, Ma Changqian, She Zhenbing, Cao Liang, Leng Shuangliang, Yan Yuqiao, 2023. Metallogenic Age and Process of Rare Metal-Bearing Pegmatites from the Northern Margin of Mufushan Complex, South China. Earth Science, 48(9): 3221-3244. doi: 10.3799/dqkx.2022.141

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Metallogenic Age and Process of Rare Metal-Bearing Pegmatites from the Northern Margin of Mufushan Complex, South China

doi: 10.3799/dqkx.2022.141

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
3.
Wuhan Center of Geological Survey, China Geological Survey, Wuhan 430205, China
4.
Hubei Geological Survey, Wuhan 430034, China

Received Date: 2021-09-25
Available Online: 2023-10-07
Publish Date: 2023-09-25

Abstract

Abstract

The Late Mesozoic Mufushan complex in South China is one of the most important rare metal mineralization areas in China, and giant rare metal deposits such as Renli-Chuanziyuan have been ascertained in its southern margin. In contrast, the metallogenic age and metallogenesis of rare metal-bearing pegmatites widely exposed in the northern are far from being understood. In this work, four major pegmatite concentrated areas in the northern margin of Mufushan including Duanfengshan, Beigang, Maishi and Huangnidong are studied. Based on detailed field investigation, petrography, mineral chemistry and columbite U-Pb dating, we discuss the metallogenic age, identify the occurrence of rare-metal (Li-Be-Nb-Ta), and decipher the mechanism of rare-metal (Li-Be-Nb-Ta) mineralization. Columbite U-Pb dating results show that the rare-metal mineralization of the northern Mufushan pegmatites occurred at 136-138 Ma, slightly postdating the Mufushan granitoids and together constituting a sequential granite emplacement, which represents products of extreme magmatic fractionation. Petrographic observations and mineral chemistry suggest that the major host minerals for Li are lepidolite, petalite and elbaite, for Be are beryl, for Nb are columbite and manganocolumbite, and for Ta are microlite and manganocolumbite. Chemical compositions of rare metal minerals record the evolution process of melt, indicating that fractional crystallization played a predominant role in controlling the successive enrichment of rare-metals. There are some differences in the Li-bearing minerals between the southern and northern margins of Mufushan, which may be due to the different P-T conditions. The large-scale rare metal mineralization of pegmatites indicates that the Mufushan area was in an extensional setting in the Early Cretaceous.
- metallogenic age,
- metallogenesis,
- mineral chemistry,
- rare metal-bearing pegmatites,
- Mufushan,
- petrology,
- mineralogy

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References(76)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Metallogenic Age and Process of Rare Metal-Bearing Pegmatites from the Northern Margin of Mufushan Complex, South China

doi: 10.3799/dqkx.2022.141

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