Copper isotope fractionation during magmatic evolution in a convergent tectonic setting: Constraints from sulfide Cu-S isotopes and whole-rock PGE of the Xiarihamu Ni-Cu sulfide deposit-Reference-Cited by-同舟云学术

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Copper isotope fractionation during magmatic evolution in a convergent tectonic setting: Constraints from sulfide Cu-S isotopes and whole-rock PGE of the Xiarihamu Ni-Cu sulfide deposit

Published:2024-11 Issue: Volume:668 Page:122348
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Tang Qingyan,Bao Jian,Zhang Yan,Li Zhuoming,Zhao Chi,Liu Wei,Li Lu

Publisher

Elsevier BV

Reference85 articles.

1. The stable isotope geochemistry of copper and zinc;Albarede;Rev. Mineral. Geochem.,2004

2. Enrichment of cobalt in the Xiarihamu Ni-Co sulfide deposit in the East Kunlun orogenic belt, Western China: Constraints from distribution of cobalt in sulfides and Fe and S isotopes of sulfides;Bao;J. Asian Earth Sci.,2024

3. The formation of magmatic nickel copper–PGE sulfide deposits;Barnes;Econ. Geol.,2005

4. Sulfide–olivine Fe–Ni exchange and the origin of anomalously Ni-rich magmatic sulfides;Barnes;Econ. Geol.,2013

5. Platinum group elements in mantle melts and mantle samples;Barnes;Lithos,2015

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