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

N. A. Gibsher; A. M. Sazonov; A. V. Travin; A. A. Tomilenko; A. V. Ponomarchuk; S. A. Sil’yanov; N. A. Nekrasova; E. O. Shaparenko; M. A. Ryabukha; M. O. Khomenko

doi:10.1134/S0016702919050033

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

N. A. Gibsher, A. M. Sazonov, A. V. Travin, A. A. Tomilenko, A. V. Ponomarchuk, S. A. Sil’yanov, N. A. Nekrasova, E. O. Shaparenko, M. A. Ryabukha, M. O. Khomenko

Результат исследования: Научные публикации в периодических изданиях › статья

2 Цитирования (Scopus)

Аннотация

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.

Язык оригинала	английский
Страницы (с-по)	593-599
Число страниц	7
Журнал	Geochemistry International
Том	57
Номер выпуска	5
DOI	https://doi.org/10.1134/S0016702919050033
Состояние	Опубликовано - 1 мая 2019

Доступ к документу

10.1134/S0016702919050033

Link to publication in Scopus

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Цитировать

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

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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.",

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

В: Geochemistry International, Том 57, № 5, 01.05.2019, стр. 593-599.

Результат исследования: Научные публикации в периодических изданиях › статья

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

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JO - Geochemistry International

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