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New Data on the Age of Gold Mineralization in the Southeastern Part of Eastern Sayan. / Damdinov, B. B.; Zhmodik, S. M.; Travin, A. V. et al.

In: Doklady Earth Sciences, Vol. 479, No. 2, 01.04.2018, p. 429-432.

Research output: Contribution to journal › Article › peer-review

Harvard

Damdinov, BB, Zhmodik, SM, Travin, AV, Yudin, DS & Goryachev, NA 2018, 'New Data on the Age of Gold Mineralization in the Southeastern Part of Eastern Sayan', Doklady Earth Sciences, vol. 479, no. 2, pp. 429-432. https://doi.org/10.1134/S1028334X18040116

APA

Damdinov, B. B., Zhmodik, S. M., Travin, A. V., Yudin, D. S., & Goryachev, N. A. (2018). New Data on the Age of Gold Mineralization in the Southeastern Part of Eastern Sayan. Doklady Earth Sciences, 479(2), 429-432. https://doi.org/10.1134/S1028334X18040116

Vancouver

Damdinov BB, Zhmodik SM, Travin AV, Yudin DS, Goryachev NA. New Data on the Age of Gold Mineralization in the Southeastern Part of Eastern Sayan. Doklady Earth Sciences. 2018 Apr 1;479(2):429-432. doi: 10.1134/S1028334X18040116

Author

Damdinov, B. B. ; Zhmodik, S. M. ; Travin, A. V. et al. / New Data on the Age of Gold Mineralization in the Southeastern Part of Eastern Sayan. In: Doklady Earth Sciences. 2018 ; Vol. 479, No. 2. pp. 429-432.

BibTeX

@article{5a17dbf631654f4aaf6a305609d0a83c,
title = "New Data on the Age of Gold Mineralization in the Southeastern Part of Eastern Sayan",
abstract = "This article presents new data on the age of the largest gold deposits in the southeastern part of Eastern Sayan. The dates have been obtained by Ar–Ar analysis of micas occurring in gold-bearing quartz veins and mineralized zones. The obtained Ar–Ar ages of fuchsite and sericite from the tectonized and mineralized zones of the Zun–Holba deposit (ore body Severnoye-3), range within 353.9–386.4 Ma; a similar result of 352.9 Ma was yielded by Ar–Ar dating of Cr–muscovite from mylonitized listvenite in the veins of the periphery of the Zun–Ospa gold deposit. However, muscovite from the ore-bearing quartz vein of the Pioneer gold–quartz deposit, located near Zun–Holba, has been dated to 421.9 Ma. The obtained new data on isotopic age of the gold–quartz ores and gold–sulphide–quartz deposits allow recognition of the Early Palaeozoic accretion–collision and the Late Palaeozoic shearing stages of formation of gold mineralization in the SE Eastern Sayan.",
author = "Damdinov, {B. B.} and Zhmodik, {S. M.} and Travin, {A. V.} and Yudin, {D. S.} and Goryachev, {N. A.}",
year = "2018",
month = apr,
day = "1",
doi = "10.1134/S1028334X18040116",
language = "English",
volume = "479",
pages = "429--432",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - New Data on the Age of Gold Mineralization in the Southeastern Part of Eastern Sayan

AU - Damdinov, B. B.

AU - Zhmodik, S. M.

AU - Travin, A. V.

AU - Yudin, D. S.

AU - Goryachev, N. A.

PY - 2018/4/1

Y1 - 2018/4/1

N2 - This article presents new data on the age of the largest gold deposits in the southeastern part of Eastern Sayan. The dates have been obtained by Ar–Ar analysis of micas occurring in gold-bearing quartz veins and mineralized zones. The obtained Ar–Ar ages of fuchsite and sericite from the tectonized and mineralized zones of the Zun–Holba deposit (ore body Severnoye-3), range within 353.9–386.4 Ma; a similar result of 352.9 Ma was yielded by Ar–Ar dating of Cr–muscovite from mylonitized listvenite in the veins of the periphery of the Zun–Ospa gold deposit. However, muscovite from the ore-bearing quartz vein of the Pioneer gold–quartz deposit, located near Zun–Holba, has been dated to 421.9 Ma. The obtained new data on isotopic age of the gold–quartz ores and gold–sulphide–quartz deposits allow recognition of the Early Palaeozoic accretion–collision and the Late Palaeozoic shearing stages of formation of gold mineralization in the SE Eastern Sayan.

AB - This article presents new data on the age of the largest gold deposits in the southeastern part of Eastern Sayan. The dates have been obtained by Ar–Ar analysis of micas occurring in gold-bearing quartz veins and mineralized zones. The obtained Ar–Ar ages of fuchsite and sericite from the tectonized and mineralized zones of the Zun–Holba deposit (ore body Severnoye-3), range within 353.9–386.4 Ma; a similar result of 352.9 Ma was yielded by Ar–Ar dating of Cr–muscovite from mylonitized listvenite in the veins of the periphery of the Zun–Ospa gold deposit. However, muscovite from the ore-bearing quartz vein of the Pioneer gold–quartz deposit, located near Zun–Holba, has been dated to 421.9 Ma. The obtained new data on isotopic age of the gold–quartz ores and gold–sulphide–quartz deposits allow recognition of the Early Palaeozoic accretion–collision and the Late Palaeozoic shearing stages of formation of gold mineralization in the SE Eastern Sayan.

UR - http://www.scopus.com/inward/record.url?scp=85047440747&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18040116

DO - 10.1134/S1028334X18040116

M3 - Article

AN - SCOPUS:85047440747

VL - 479

SP - 429

EP - 432

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 13593944