四川甲基卡锂矿床花岗岩体Li同位素组成及其对稀有金属成矿的制约

侯江龙; 李建康; 张玉洁; 李超

doi:10.3799/dqkx.2018.595

Volume 43 Issue 6

Jun. 2018

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Article Navigation > Earth Science > 2018 > 43(6): 2042-2054

Hou Jianglong, Li Jiankang, Zhang Yujie, Li Chao, 2018. Li Isotopic Composition and Its Constrains on Rare Metal Mineralization of Jiajika Two-Mica Granite, Sichuan Province. Earth Science, 43(6): 2042-2054. doi: 10.3799/dqkx.2018.595

Citation:

Hou Jianglong, Li Jiankang, Zhang Yujie, Li Chao, 2018. Li Isotopic Composition and Its Constrains on Rare Metal Mineralization of Jiajika Two-Mica Granite, Sichuan Province. Earth Science, 43(6): 2042-2054. doi: 10.3799/dqkx.2018.595

Citation:

Hou Jianglong, Li Jiankang, Zhang Yujie, Li Chao, 2018. Li Isotopic Composition and Its Constrains on Rare Metal Mineralization of Jiajika Two-Mica Granite, Sichuan Province. Earth Science, 43(6): 2042-2054. doi: 10.3799/dqkx.2018.595

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Li Isotopic Composition and Its Constrains on Rare Metal Mineralization of Jiajika Two-Mica Granite, Sichuan Province

doi: 10.3799/dqkx.2018.595

1.
MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
3.
National Research Center for Geoanalysis, Beijing 100037, China

Received Date: 2018-01-15
Publish Date: 2018-06-15

Abstract

Abstract

Jiajika superlarge hard rock type lithium deposit is one of the most abundant lithium mineral resouces in China. The two-mica granite outcropped in the southern Jiajika orefield is generally regarded as source rocks of the ore-bearing pegmatites. Li isotopic composition is a useful tool to explore the origin and evolution of rare metal. Based on the detailed field work, the lithium isotopic composition of granite was tested by MC-ICP-MS in this study. The results show that the lithium content of the granite is from 192×10^-6 to 470×10^-6, and the mean value is 309×10^-6; the value of δ⁷Li ranges from -1.56‰ to 0.90‰, and the mean value is -0.24‰, which is closed to the average value of upper crust. Jiajika two-mica granite apparently has higher content of lithium and lower value of δ⁷Li, and the δ⁷Li and Li, Rb, Ga, SiO₂ and ε_Nd(t) have no obvious correlation. Lithium isotopic composition of granite reflects its characteristics of source rock, and it has not been influenced by crystallization differentiation of magma and alteration. The geochemical and isotope geochemistry data indicate that the source of magma is mainly composed of partial melting of Triassic Xikang sand-mudstone, which may have been mixed with materials from deep source. In addition, variations of lithium content and Li isotopic composition show that the fluid of magma migrated from center to the north and south, and the metallogenic fluid of pegmatite is derived from Jiajika two-mica granite. The content of lithium and Li isotopic composition can not only be used to classify the types of lithium deposits, but also can facilitate the prospecting of rare metals.
- two-mica granite,
- pegmatite,
- lithium isotope,
- Jiajika,
- deposit,
- petrology

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References(76)

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