Precious-Metal Mineralization and Formation Conditions of the Biche-Kadyr-Oos Epithermal Au-Ag Ore Occurrence (Eastern Sayan, Russia)
Author:
Kuzhuget Renat V.1, Ankusheva Natalia N.123ORCID, Hertek Ailai K.1, Kalinin Yuri A.4, Damdinov Bulat B.5ORCID, Pirajno Franco6, Butanaev Yuri V.1, Suge-Maadyr Nadezhda V.1, Soldup Sholban N.1
Affiliation:
1. Tuvinian Institute for Exploration of Natural Resources of Siberian Branch of RAS (TuvIENR SB RAS), 667007 Kyzyl, Russia 2. South Urals Federal Research Center of Mineralogy and Geoecology UB RAS, Institute of Mineralogy, 456317 Miass, Russia 3. Geological Faculty, South Urals State University, 456314 Miass, Russia 4. Sobolev Institute of Geology and Mineralogy SB RAS, 630090 Novosibirsk, Russia 5. Dobretsov Geological Institute SB RAS, 670047 Ulan-Ude, Russia 6. Centre for Exploration Targeting, University of Western Australia, Perth, WA 6009, Australia
Abstract
The Biche-Kadyr-Oos epithermal Au-Ag ore occurrence is a prospective object in the Ak-Sug porphyry copper ore cluster (Eastern Sayan) in the northern part of the Central Asian orogenic belt (CAOB). The mineralization consists of gold-sulfide-quartz and gold-polysulfide-carbonate-quartz veins with argillic zones in the Lower Cambrian volcanic-sedimentary rocks. The origin of the Au-Ag ore occurrence is still debatable. To determine the origin, we examined the mineralogical and geochemical features, conditions of formation, and fluid sources of the Biche-Kadyr-Oos ore. A mineralogical and geochemical investigation outlines three stages of mineral formation: early argillic stage; gold-sulfide-quartz stage with pyrite, marcasite, pyrrhotite, arsenopyrite, chalcopyrite, less frequently sphalerite, hessite, gold, and electrum; and late gold-polysulfide-carbonate-quartz stage with gold, electrum, Hg-electrum, Se-acanthite, Se-galena, bornite, tennantite, tetrahedrite, hessite, tellurobismuthite, bismuthinite, matildite, jamesonite, ourayite, native Bi, and barite. Fluid inclusion study (thermometry, Raman spectroscopy) in quartz and mineral thermometry (electrum and sphalerite paragenesis) determined that ore veins were formed at P~0.5 kbar from CO2-water Na-K-chloride fluid (4.9–9.6 wt % NaCl eqv) and temperatures from 300 to 200 °C (early gold-sulfide-quartz veins at 300–230 °C, and late gold-polysulfide-carbonate-quartz veins at 290–200 °C) and variations in fO2, fS2, fSe2 and fTe2. The S isotopic composition in sulfides and δ34SH2S values of the fluid are +1.3‰ and +4.7‰, respectively, (T = 300–275 °C) indicating magmatic S in ore formation. The oxygen isotope data indicate that during the formation of veins, the magmatic fluid mixed with meteoric water (δ18Ofluid is from +3.4 to +6.4‰). The isotopic data that were obtained combined with mineralogical and geochemical features and conditions of ore formation indicate the similarity of Biche-Kadyr-Oos ore occurrence with epithermal Au-Ag deposits of intermediate sulfidation (IS) type. The presence of epithermal Au-Ag mineralization of the Biche-Kadyr-Oos IS type in ore cluster of the Ak-Sug Cu-Au-Mo porphyry deposit indicates the existence of a single porphyry-epithermal ore-magmatic system.
Funder
Russian Science Foundation
Subject
Geology,Geotechnical Engineering and Engineering Geology
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