Magmatic–hydrothermal evolution of the Koktokay No. 3 pegmatite, Altai, northwestern China: Constraints from in situ boron isotope and chemical compositions of tourmaline-Reference-Cited by-同舟云学术

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Magmatic–hydrothermal evolution of the Koktokay No. 3 pegmatite, Altai, northwestern China: Constraints from in situ boron isotope and chemical compositions of tourmaline

Published:2023-12 Issue: Volume:462-463 Page:107398
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Yin Rong,Huang Xiao-Long,Wang Ru-Cheng,Wei Gang-Jian,Xu Yi-Gang,Wang Yu,Sun Xiao-Ming,Zhang Le,Xia Xiao-Ping

Funder

National Key Research and Development Program of China

National Natural Science Foundation of China

Guangzhou Institute of Geochemistry, Chinese Academy of Sciences

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference86 articles.

1. Experimental investigation of the stability of a chloroborate complex and thermodynamic description of aqueous species in the B-Na-Cl-O-H system up to 350 °C;Akinfiev;Geochem. Int.,2006

2. Mineral/leucosome trace-element partitioning in a peraluminous migmatite (a laser ablation-ICP-MS study);Bea;Chem. Geol.,1994

3. Boron-isotope variations in tourmaline from granitic pegmatites of the Borborema pegmatite province, NE Brazil, (Asociación Geólogica Argentina: Serie D-13, Publicaciones especiales);Beurlen,2011

4. Geological framework and Paleozoic tectonic history of the Chinese Altai, NW China: a review;Cai;Russ. Geol. Geophys.,2011

5. The classification of granitic pegmatites revised;Černý;Can. Mineral.,2005

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