Geochemical, fluid inclusion and O–H–S isotope constraints on the origin of the Rangraz copper deposit, Central Iran
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DOI: 10.1016/j.oregeorev.2020.103877
Abstract: Abstract The Rangraz copper deposit (5 Mt @ 0.83% Cu) is located 20 km north of Saveh city, Markazi Province, Iran, in the central Uromieh-Dokhtar volcano-plutonic belt. Host rocks are mainly composed of Eocene volcanic… read more here.
Keywords: copper deposit; fluid; copper; fluid inclusion ... See more keywords