片麻岩穹窿与伟晶岩型锂矿的成矿规律探讨

许志琴; 付小方; 赵中宝; 李广伟; 郑艺龙; 马泽良

doi:10.3799/dqkx.2019.042

Volume 44 Issue 5

May 2019

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Xu Zhiqin, Fu Xiaofang, Zhao Zhongbao, Li Guangwei, Zheng Yilong, Ma Zeliang, 2019. Discussion on Relationships of Gneiss Dome and Metallogenic Regularity of Pegmatite-Type Lithium Deposits. Earth Science, 44(5): 1452-1463. doi: 10.3799/dqkx.2019.042

Citation:

Xu Zhiqin, Fu Xiaofang, Zhao Zhongbao, Li Guangwei, Zheng Yilong, Ma Zeliang, 2019. Discussion on Relationships of Gneiss Dome and Metallogenic Regularity of Pegmatite-Type Lithium Deposits. Earth Science, 44(5): 1452-1463. doi: 10.3799/dqkx.2019.042

Citation:

Xu Zhiqin, Fu Xiaofang, Zhao Zhongbao, Li Guangwei, Zheng Yilong, Ma Zeliang, 2019. Discussion on Relationships of Gneiss Dome and Metallogenic Regularity of Pegmatite-Type Lithium Deposits. Earth Science, 44(5): 1452-1463. doi: 10.3799/dqkx.2019.042

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Discussion on Relationships of Gneiss Dome and Metallogenic Regularity of Pegmatite-Type Lithium Deposits

doi: 10.3799/dqkx.2019.042

1.
School of Earth Sciences and Engineering, State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210023, China
2.
Sichuan Geological Survey, Chengdu 610081, China
3.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2019-03-08
Publish Date: 2019-05-15

Abstract

Abstract

Gneiss domes develop in exhuming orogens, where they constitute an efficient mechanism for material and heat advection of continental crust during orogenesis, which is always related to magmatism (or migmatization). Dome formation may be accompanied by heterogeneous thinning of the upper crust that may occur as the ductile lower crust flows into a gneiss dome by convergent flow and lead to contraction strain in the core. During gneiss dome formation process, lithium-rich (with other rare earth elements) pegmatite is beneficial to form and hence, lead to lithium enrichment. Previous researches indicate that the Songpan-Ganzi-Tianshuihai Indosinian orogenic belt, located in the northern part of the Qinghai-Tibetan Plateau, is the "pegmatite-type" lithium mine resources base in China. The ultra-large pegmatite-type lithium belt in the southwestern of the Songpan-Ganzi occurs in the Triassic flysch which is the country rock of Barrow-type metamorphism with low/medium pressure-high temperature metamorphic traits. It has a genetic relationship with the Late Triassic granite and the lithium-bearing pegmatite intrusion. The authors suggest that future studies should focus on (1) exploring the formation process and tectonic mechanism of gneiss domes; (2) identifying the geochemical properties of granite-bearing pegmatites; (3) revealing the genetic relationship between the differentiation of granite and the evolution of ore-bearing pegmatite; (4) clarifying lithium migrating and enriching process in the melt; (5) delineating the distribution of the Barrow-type metamorphic facies belt in the Triassic strata; (6) proving the favorable metamorphic facies belts and P-T conditions where the lithium-rich pegmatite formed can reveal the space-time coupling of "deformation-metamorphism-magmatic deep-melting-metallogenesis". Moreover, the law of enrichment and preservation of lithium ore, used to establish the metallogenic kinetics model, is an important scientific aspect to reveal the relationships of gneiss dome and metallogenic regularity of pegmatite-type lithium deposits.
- gneiss dome,
- granite,
- lithium-bearing pegmatite,
- four integrated factors of "metamorphism-deformation-magmatism-mineralization",
- lithium deposit,
- mineral deposit

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References(77)

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