2021
DOI: 10.17580/em.2021.01.02
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Geology and gold content of carbonaceous shale in Baikal mineralization site, Southern Ural

Abstract: tav S. et. al. GPS constraints on continental deformation in the Africa-Arabia-Eurasia continental collision zone and implica-tions for the dynamics of plate interactions.

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Cited by 6 publications
(5 citation statements)
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“…Black shales of the Kumak ore field are rich in gold, which is fine-grained, associated with sulfides (pyrite, arsenopyrite), and high-carat (919-1000). The maximum registered gold grade is 17.7 g/t [10]. Commercial gold and tungsten contents have been found in the shales of the Amur deposit [2].…”
Section: Black Shales Of the Magnitogorsk Trough And Adjacent Areasmentioning
confidence: 94%
“…Black shales of the Kumak ore field are rich in gold, which is fine-grained, associated with sulfides (pyrite, arsenopyrite), and high-carat (919-1000). The maximum registered gold grade is 17.7 g/t [10]. Commercial gold and tungsten contents have been found in the shales of the Amur deposit [2].…”
Section: Black Shales Of the Magnitogorsk Trough And Adjacent Areasmentioning
confidence: 94%
“…1). The volcanic sedimentary rocks are cut with numerous intrusive rocks from the Dzhabygasai diorite-plagiogranite-gabbro (pȖ-Ȗį-ȞD 3 d) and Kumak diorite-plagiogranite (įС 1 k) systems [13,17,18].…”
Section: Geological Structurementioning
confidence: 99%
“…The Kumak ore is dominated by fine high-karat gold (Аu 90-96%) associated with gold-bismuth-telluride and native gold-tourmaline assemblages [18]. The oxidation zone contains a little of supergene gold at an average amount of 2% of total gold.…”
Section: Geological Structurementioning
confidence: 99%
“…Единичные находки редкоземельных (РЗЭ) минералов на западном склоне Южного Урала известны давно [Орлова, 1960; Беккер, 1960]. Более или менее систематическое изучение этого типа минерализации начато А. А. Алексеевым и продолжено нами [Алексеев, Тимофеева 2007;Ковалев и др., 2017а, 2017б;Ковалев и др., 2023;Snachev et al, 2023]. Отложения шатакского комплекса в этом отношении представляют значительный интерес ввиду разнообразия слагающих его магматических (базальты, риодациты) и осадочных (конгломераты, песчаники, сланцы) пород.…”
Section: Introductionunclassified