2020
DOI: 10.3103/s0145875220060113
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The Siratur Gold Deposit in Carbonaceous Rocks of an Ophiolite Association, South Urals

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Cited by 3 publications
(2 citation statements)
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“…For the carbonaceous shales of the Polyakovskaya Formation (О 1-2 pl), which is located in the juncture of the Bashkirian megaanticlinorium and the northern closure of the Magnitogorsk megazone (Siratur ore field, Chernoe Ozero gold occurrence) (Fig. 1), the maximum С org content is up to 4% (2% on average, based on the data for 4 samples) and the δ 13 С org (5 samples) is -27.28…-24.84‰ [20,21,22]. These values are characteristic of the bottom sediments in the marginal-marine zone.…”
Section: Black Shales As Oil Source Rocks and Analogues Of Shelf Carbonatesmentioning
confidence: 99%
“…For the carbonaceous shales of the Polyakovskaya Formation (О 1-2 pl), which is located in the juncture of the Bashkirian megaanticlinorium and the northern closure of the Magnitogorsk megazone (Siratur ore field, Chernoe Ozero gold occurrence) (Fig. 1), the maximum С org content is up to 4% (2% on average, based on the data for 4 samples) and the δ 13 С org (5 samples) is -27.28…-24.84‰ [20,21,22]. These values are characteristic of the bottom sediments in the marginal-marine zone.…”
Section: Black Shales As Oil Source Rocks and Analogues Of Shelf Carbonatesmentioning
confidence: 99%
“…They represent a very favorable geochemical environment for the primary chemical adsorption of noble and rare metals and are the source of such metals during metamorphic alteration [1][2][3][4][5][6]. Black shale sediments are associated with gold deposits in the world and in the Southern Ural [7][8][9][10]. In the Orenburg Region of the Southern Ural, gold-bearing ore occurs in carbon deposits of Kumak ore field adjoining the Anikhovsky Graben of the East Ural Uplift.…”
Section: Introductionmentioning
confidence: 99%