Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan)

F. I. Zhimulev; Yu A. Kalinin; V. P. Sukhorukov; E. De Pelsmaeker; M. Poujol; K. R. Kovalev; S. Glorie; E. A. Naumov; R. Seltmann; J. De Grave

doi:10.1134/S1028334X18080238

Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan)

F. I. Zhimulev, Yu A. Kalinin, V. P. Sukhorukov, E. De Pelsmaeker, M. Poujol, K. R. Kovalev, S. Glorie, E. A. Naumov, R. Seltmann, J. De Grave

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

Аннотация

Accessory zircon from the polyphase Raygorodok stock (Northern Kazakhstan) has been dated by local U–Pb analysis (SIMS and LA-ICP-MS). This Au-bearing intrusion has been dated to 442–447 Ma, suggesting its emplacement at the very end of the Ordovician and Early Silurian, allowing the stock’s correlation with the Stepnyak Complex of small intrusions. Thus, control of small intrusions of the Stepnyak type over gold mineralization has been corroborated permitting their use as a regional prospecting characteristic.

Язык оригинала	английский
Страницы (с-по)	1033-1036
Число страниц	4
Журнал	Doklady Earth Sciences
Том	481
Номер выпуска	2
DOI	https://doi.org/10.1134/S1028334X18080238
Состояние	Опубликовано - 1 авг. 2018

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10.1134/S1028334X18080238

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Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan). / Zhimulev, F. I.; Kalinin, Yu A.; Sukhorukov, V. P. и др.

В: Doklady Earth Sciences, Том 481, № 2, 01.08.2018, стр. 1033-1036.

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

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AU - Zhimulev, F. I.

AU - Kalinin, Yu A.

AU - Sukhorukov, V. P.

AU - De Pelsmaeker, E.

AU - Poujol, M.

AU - Kovalev, K. R.

AU - Glorie, S.

AU - Naumov, E. A.

AU - Seltmann, R.

AU - De Grave, J.

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AB - Accessory zircon from the polyphase Raygorodok stock (Northern Kazakhstan) has been dated by local U–Pb analysis (SIMS and LA-ICP-MS). This Au-bearing intrusion has been dated to 442–447 Ma, suggesting its emplacement at the very end of the Ordovician and Early Silurian, allowing the stock’s correlation with the Stepnyak Complex of small intrusions. Thus, control of small intrusions of the Stepnyak type over gold mineralization has been corroborated permitting their use as a regional prospecting characteristic.

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