川西甲基卡308号伟晶岩脉年代学和地球化学特征及其地质意义

代鸿章; 王登红; 刘丽君; 于扬; 代晶晶; 付小方

doi:10.3799/dqkx.2018.528

Volume 43 Issue 10

Oct. 2018

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Article Navigation > Earth Science > 2018 > 43(10): 3664-3681

Dai Hongzhang, Wang Denghong, Liu Lijun, Yu Yang, Dai Jingjing, Fu Xiaofang, 2018. Geochronology, Geochemistry and Their Geological Significances of No.308 Pegmatite Vein in the Jiajika Deposit, Western Sichuan, China. Earth Science, 43(10): 3664-3681. doi: 10.3799/dqkx.2018.528

Citation:

Dai Hongzhang, Wang Denghong, Liu Lijun, Yu Yang, Dai Jingjing, Fu Xiaofang, 2018. Geochronology, Geochemistry and Their Geological Significances of No.308 Pegmatite Vein in the Jiajika Deposit, Western Sichuan, China. Earth Science, 43(10): 3664-3681. doi: 10.3799/dqkx.2018.528

Citation:

Dai Hongzhang, Wang Denghong, Liu Lijun, Yu Yang, Dai Jingjing, Fu Xiaofang, 2018. Geochronology, Geochemistry and Their Geological Significances of No.308 Pegmatite Vein in the Jiajika Deposit, Western Sichuan, China. Earth Science, 43(10): 3664-3681. doi: 10.3799/dqkx.2018.528

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Geochronology, Geochemistry and Their Geological Significances of No.308 Pegmatite Vein in the Jiajika Deposit, Western Sichuan, China

doi: 10.3799/dqkx.2018.528

1.
Key Laboratory of Metallogeny and Mineral Resource Assessment of Ministry of Land and Resources, Institute of Mineral Resources of Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth Science and Resources, China University of Geoscience, Beijing 100083, China
3.
Geological Survey Institute of Sichuan Province, Chendu 610081, China

Received Date: 2017-06-27
Publish Date: 2018-10-20

Abstract

Abstract

No. 308 pegmatite vein has the maximal exposed area in the Jiajika rare metal deposit, which is the largest pegmatite type deposit in China. Because of the low degree of exploration and research, its metallogenic epoch and metallogenic mechanism remain unclear. Detailed geochronology and lithogeochemistry of the granitoids and pegmatites were carried out to explore the petrogenesis and tectonic setting cassiterite LA-MC-ICP-MS dating yields concordant ages with (210.9±4.6) Ma of spodumene-bearing pegmatite in the middle zone, which reflects that No.308 pegmatite vein in the Jiajika pegmatite deposit formed at the late stage of Indosinian and was the result of the relative stable period after the strong Indosinian Orogeny. Geochemical data show that REEs and other trace elements patterns of the barren aplite in marginal zone of No. 308 pegmatite vein are similar to the two-mica granite in the Jiajika deposit, and both of them are characterized by the peraluminous S-type granite and homology. Dfferentiation of the magmatic water gradually increased from granitic aplites to pegmatites. The granitic magma ascended and intruded under a medium-shallow deep and partial reducing environment. During the evolution of magma, there is a strong alkali metasomatism between the melt phase and the fluid phase rich in volatile, and resulting in that a large-scale rare metal mineralization occurred in the certain structural zoning of No.308 pegmatite vein in the Jiajika deposit.
- cassiterite U-Pb dating,
- geochemistry,
- petrogenesis,
- lithium polymetallic pegmatite,
- Jiajika

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References(77)

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Geochronology, Geochemistry and Their Geological Significances of No.308 Pegmatite Vein in the Jiajika Deposit, Western Sichuan, China

doi: 10.3799/dqkx.2018.528

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