The large granitic pegmatite Li deposits formed at final collision of a three micro-continent amalgamation in the Central Altun Tagh, Northwest China-Reference-Cited by-同舟云学术

The large granitic pegmatite Li deposits formed at final collision of a three micro-continent amalgamation in the Central Altun Tagh, Northwest China

Published:2024-05 Issue: Volume:168 Page:106043
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Kang Kai,Hong Tao,Zhang Peng,Liu Shanke,Yao Fojun,Li Hang,Ma Yince,Wang Xuehai,Liao Zhaoxia,Niu Lei,Ma Jing,Jiao Pengli,Chen Jianzhong,Liu Xingzhong,Xu Xing-Wang

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference125 articles.

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3. Lithium enrichment in intracontinental rhyolite magmas leads to Li deposits in caldera basins;Benson;Nat. Commun.,2017

4. Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear Zone;Berthé;J. Struct. Geol.,1979

5. The spatial and temporal patterning of the deep crust and implications for the process of melt extraction;Brown;Philos. Trans. R. Soc. A Math. Phys. Eng. Sci.,2010

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1. Evolution of the rare-metal mineralization system associated with collision-related pegmatites in the western Altyn Tagh Orogen, Tugeman, NW China;Journal of Asian Earth Sciences;2024-08

2. Geochronology and Geochemistry of Granitic Pegmatites from Tashidaban Li Deposit in the Central Altun Tagh, Northwest China;Minerals;2024-05-24