2020
DOI: 10.1016/j.oregeorev.2020.103863
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The large Bakyrchik orogenic gold deposit, eastern Kazakhstan: Geology, mineralization, fluid inclusion, and stable isotope characteristics

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Cited by 9 publications
(1 citation statement)
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“…Helium isotopes were also considered to be indicative of mantle input (Graupner et al 2010). A magmatic contribution at Bakyrchik is assumed based upon near-zero δ 34 S isotope values and broadly coeval mafic dikes (Soloviev et al 2020). Damdinov et al (2021) argued that the presence of As-, Bi-, Sb-, and Te-bearing mineral phases; the presence of Agand Sb-rich sulfosalts; calculated δ 18 O values for auriferous quartz of about 6-7‰ and measured δ 34 S sulfide values of about − 4 to + 5‰; and restriction of ores to granitoid hosts 2020), a magmatic and/ or mantle thermal event superimposed a contact metamorphic overprint on previously regionally metamorphosed sediments.…”
Section: Yilgarn Craton the Fimiston Deposit Mined By The Goldenmentioning
confidence: 99%
“…Helium isotopes were also considered to be indicative of mantle input (Graupner et al 2010). A magmatic contribution at Bakyrchik is assumed based upon near-zero δ 34 S isotope values and broadly coeval mafic dikes (Soloviev et al 2020). Damdinov et al (2021) argued that the presence of As-, Bi-, Sb-, and Te-bearing mineral phases; the presence of Agand Sb-rich sulfosalts; calculated δ 18 O values for auriferous quartz of about 6-7‰ and measured δ 34 S sulfide values of about − 4 to + 5‰; and restriction of ores to granitoid hosts 2020), a magmatic and/ or mantle thermal event superimposed a contact metamorphic overprint on previously regionally metamorphosed sediments.…”
Section: Yilgarn Craton the Fimiston Deposit Mined By The Goldenmentioning
confidence: 99%