Tourmaline chemical composition and boron isotopic composition at the Longmenshan pegmatite in Dahongliutan area, West Kunlun: Implication for rare-metal Li-Be mineralization

Author:

Yao Jun-Ming,Li Feng-Ling,Ma Guan-Zhong,Zhang Xue-Bing,Hou Ke-Jun,Yang Hong-Yun,Li Nuo

Publisher

Elsevier BV

Reference102 articles.

1. In-situ elemental and boron isotopic variations of tourmaline from the Koktokay pegmatitic rare-metal deposit, China: Insights into external contamination and the source of the granitic pegmatite;Bai;Ore Geol. Rev.,2023

2. Boron-isotope variations in tourmaline from granitic pegmatites of the Borborema Pegmatite Province, NE-Brazil;Beurlen;Asociación Geológica Argentina, Serie D, Publicación Especial,2011

3. Pegmatite magmatic evolution and rare metal mineralization of the dahongliutan pegmatite field, western kunlun orogen: Constraints from the B isotopic composition and mineral-chemistry;Cao;Int. Geol. Rev.,2023

4. Fertile granites of Precambrian rare-element pegmatite fields: is geochemistry controlled by tectonic setting or source lithologies?;Černý;Precambr. Res.,1991

5. Rare-element Granitic Pegmatites. Part I: Anatomy and Internal Evolution of Pegmatitic Deposits;Černý;Geosci. Can.,1991

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