Phase equilibria in the KFeS2–Fe–S system at 300–600 °C and bartonite stability

Author:

Osadchii Valentin O.ORCID,Voronin Mikhail V.,Baranov Alexander V.

Funder

Russian Foundation for Basic Research

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference50 articles.

1. Amthauer G, Bente K (1983) Mixed-valent iron in synthetic rasvumite, KFe2S3. Naturwissenschaften 70:146–147. https://doi.org/10.1007/BF00401605

2. Azarova YV, Krinov DI, Sokolova MN (2006) A structural and genetic relationship of djerfisherite and bartonite, and the problem of isomorphous substitutions in the system djerfisherite–“Cu-djerfisherite”–bartonite (in Russian). New Data Miner 41:98–107

3. Balabonin NL, Voloshin AV, Pakhomovsky JA, Poljakov KI (1980) The composition of djerfisherite in alkali complexes of the Kola Peninsula (in Russian). Mineral J 2:90–99

4. Barkov AI, Laajoki KVO, Gehor SA et al (1997) Chlorine-poor analogues of Djerfisherite–Thalfenisite from Noril’sk, Siberia and Salmagorsky, Kola Peninsula, Russia. Can Mineral 35:1421–1430

5. Barkov AY, Martin RF, Cabri LJ (2015) Rare sulfides enriched in K, Tl and Pb from the Noril’sk and Salmagorsky complexes, Russia: new data and implications. Mineral Mag 79:799–808. https://doi.org/10.1180/minmag.2015.079.3.20

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