Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia)

Standard

Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia). / Gibsher, N. A.; Sazonov, A. M.; Travin, A. V. et al.

In: Geochemistry International, Vol. 57, No. 5, 01.05.2019, p. 593-599.

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

Harvard

Gibsher, NA, Sazonov, AM, Travin, AV, Tomilenko, AA, Ponomarchuk, AV, Sil’yanov, SA, Nekrasova, NA, Shaparenko, EO, Ryabukha, MA & Khomenko, MO 2019, 'Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia)', Geochemistry International, vol. 57, no. 5, pp. 593-599. https://doi.org/10.1134/S0016702919050033

APA

Gibsher, N. A., Sazonov, A. M., Travin, A. V., Tomilenko, A. A., Ponomarchuk, A. V., Sil’yanov, S. A., Nekrasova, N. A., Shaparenko, E. O., Ryabukha, M. A., & Khomenko, M. O. (2019). Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia). Geochemistry International, 57(5), 593-599. https://doi.org/10.1134/S0016702919050033

Vancouver

Gibsher NA, Sazonov AM, Travin AV, Tomilenko AA, Ponomarchuk AV, Sil’yanov SA et al. Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia). Geochemistry International. 2019 May 1;57(5):593-599. doi: 10.1134/S0016702919050033

Author

Gibsher, N. A. ; Sazonov, A. M. ; Travin, A. V. et al. / Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia). In: Geochemistry International. 2019 ; Vol. 57, No. 5. pp. 593-599.

BibTeX

@article{889bec32319e41d990ea1d87720a9cc9,

title = "Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia)",

abstract = "Abstract: 40Ar/39Ar dates on the quartz–micaceous–sulfide, quartz–gold–arsenopyrite–pyrrhotite, and quartz–gold–stibium associations at the superlarge (>1000 t Au) Olimpiada gold deposit, the Yenisei Ridge, are compared. It is established that the hydrothermal activity at the deposit has continued for no less than 150 Ma from 817 to 660 Ma.",

keywords = "Ar-Ar age, gold, gold deposits, BEARING",

author = "Gibsher, {N. A.} and Sazonov, {A. M.} and Travin, {A. V.} and Tomilenko, {A. A.} and Ponomarchuk, {A. V.} and Sil{\textquoteright}yanov, {S. A.} and Nekrasova, {N. A.} and Shaparenko, {E. O.} and Ryabukha, {M. A.} and Khomenko, {M. O.}",

year = "2019",

month = may,

day = "1",

doi = "10.1134/S0016702919050033",

language = "English",

volume = "57",

pages = "593--599",

journal = "Geochemistry International",

issn = "0016-7029",

publisher = "PLEIADES PUBLISHING INC",

number = "5",

}

RIS

TY - JOUR

T1 - Age and Duration of the Formation of the Olimpiada Gold Deposit (Yenisei Ridge, Russia)

AU - Gibsher, N. A.

AU - Sazonov, A. M.

AU - Travin, A. V.

AU - Tomilenko, A. A.

AU - Ponomarchuk, A. V.

AU - Sil’yanov, S. A.

AU - Nekrasova, N. A.

AU - Shaparenko, E. O.

AU - Ryabukha, M. A.

AU - Khomenko, M. O.

PY - 2019/5/1

Y1 - 2019/5/1

N2 - Abstract: 40Ar/39Ar dates on the quartz–micaceous–sulfide, quartz–gold–arsenopyrite–pyrrhotite, and quartz–gold–stibium associations at the superlarge (>1000 t Au) Olimpiada gold deposit, the Yenisei Ridge, are compared. It is established that the hydrothermal activity at the deposit has continued for no less than 150 Ma from 817 to 660 Ma.

AB - Abstract: 40Ar/39Ar dates on the quartz–micaceous–sulfide, quartz–gold–arsenopyrite–pyrrhotite, and quartz–gold–stibium associations at the superlarge (>1000 t Au) Olimpiada gold deposit, the Yenisei Ridge, are compared. It is established that the hydrothermal activity at the deposit has continued for no less than 150 Ma from 817 to 660 Ma.

KW - Ar-Ar age

KW - gold

KW - gold deposits

KW - BEARING

UR - http://www.scopus.com/inward/record.url?scp=85066946802&partnerID=8YFLogxK

U2 - 10.1134/S0016702919050033

DO - 10.1134/S0016702919050033

M3 - Article

AN - SCOPUS:85066946802

VL - 57

SP - 593

EP - 599

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 5

ER -

ID: 20533299