Physicochemical Parameters of the Origin of Hydrothermal Mineral Deposits: Evidence from Fluid Inclusions. V. Antimony, Arsenic, and Mercury Deposits
Author:
Publisher
Pleiades Publishing Ltd
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1134/S0016702918090082.pdf
Reference82 articles.
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5. A. Audetat, D. Gunther, and C. A. Heinrich, “Magmatic–hydrothermal evolution in a fractionating granite: a microchemical study of the Sn–W–F mineralized Mole Granite (Australia),” Geochim. Cosmochim. Acta 64 (19), 3373–3393 (2000).
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1. Changes in antimony isotopic composition as a tracer of hydrothermal fluid evolution at the Sb deposits in Pezinok (Slovakia);Mineralium Deposita;2023-10-20
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3. Conditions of the Formation of Unique Mineralization with Yushkinite V1 – xS · n[(Mg,Al)(OH)2] in Quartz–Calcite Veins, Pai-Khoi Ridge: Evidence from Study of Fluid Inclusions;Doklady Earth Sciences;2020-06
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