Tracing the ore-formation history of the shear-zone-controlled Huogeqi Cu–Pb–Zn deposit in Inner Mongolia, northern China, using H, O, S, and Fe isotopes

Pi, Qiaohui; Zhong, Richen; Hu, Ruizhong

doi:10.1016/j.oregeorev.2015.06.003

Cited by 10 publications

(1 citation statement)

References 29 publications

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“…Subsequent work on different continental magmatic-hydrothermal and metamorphic Fe-Cu-Au-Sn-W sulfide ore deposits confirmed notable Fe isotope variations in pyrite over a range of at least ~2‰, whereas other major Fe-bearing minerals such as chalcopyrite, pyrrhotite or magnetite usually exhibit smaller variations of  57 Fe values (Markl et al, 2006;Wang et al, 2011;Cheng et al, 2015;Pi et al, 2015;Wawryk and Foden, 2015;Li et al, 2018;Zhu et al, 2018). Likewise, direct data for dissolved iron isotope compositions in modern hydrothermal fluids from MOR show variations of  57 Fe values over at least 1.5‰ (e.g., Sharma et al, 2001;Beard et al, 2003;Rouxel et al, 2008;Bennett et al, 2009;Syverson et al, 2017).…”

Section: Introductionmentioning

confidence: 98%

Mechanisms and rates of pyrite formation from hydrothermal fluid revealed by iron isotopes

Pokrovski

Blanchard²,

Saunier³

et al. 2021

Geochimica et Cosmochimica Acta

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