Origin and evolution of hydrothermal fluids in the Marshoun epithermal Pb–Zn–Cu (Ag) deposit, Tarom-Hashtjin metallogenic belt, NW Iran

• Published in: Ore geology reviews Vol. 113; p. 103087
• Main Authors: Kouhestani, Hossein, Mokhtari, Mir Ali Asghar, Qin, Kezhang, Zhao, Junxing
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.10.2019
• Subjects: Fluid inclusion; Intermediate-sulfidation; Iran; Marshoun; Oxygen and sulfur isotopes; Tarom–Hashtjin; Marshoun; Tarom–Hashtjin; Oxygen and sulfur isotopes; Iran; Intermediate-sulfidation; Fluid inclusion

[Display omitted] •The Marshoun deposit is an intermediate-sulfidation style of epithermal mineralization.•Microthermometric data indicates trapping of moderate- to high-temperature and moderate-salinity fluids.•Fluid boiling and mixing facilitated hydrothermal alteration and mineralization.•Stable...