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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.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Zhimulev, FI, Kalinin, YA, Sukhorukov, VP, De Pelsmaeker, E, Poujol, M, Kovalev, KR, Glorie, S, Naumov, EA, Seltmann, R & De Grave, J 2018, 'Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan)', Doklady Earth Sciences, Том. 481, № 2, стр. 1033-1036. https://doi.org/10.1134/S1028334X18080238

APA

Zhimulev, F. I., Kalinin, Y. A., Sukhorukov, V. P., De Pelsmaeker, E., Poujol, M., Kovalev, K. R., Glorie, S., Naumov, E. A., Seltmann, R., & De Grave, J. (2018). Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan). Doklady Earth Sciences, 481(2), 1033-1036. https://doi.org/10.1134/S1028334X18080238

Vancouver

Zhimulev FI, Kalinin YA, Sukhorukov VP, De Pelsmaeker E, Poujol M, Kovalev KR и др. Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan). Doklady Earth Sciences. 2018 авг. 1;481(2):1033-1036. doi: 10.1134/S1028334X18080238

Author

Zhimulev, F. I. ; Kalinin, Yu A. ; Sukhorukov, V. P. и др. / Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan). в: Doklady Earth Sciences. 2018 ; Том 481, № 2. стр. 1033-1036.

BibTeX

@article{b65fc76c02774f1ebc1a8cdcaabbaf9c,
title = "Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan)",
abstract = "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{\textquoteright}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.",
author = "Zhimulev, {F. I.} and Kalinin, {Yu A.} and Sukhorukov, {V. P.} and {De Pelsmaeker}, E. and M. Poujol and Kovalev, {K. R.} and S. Glorie and Naumov, {E. A.} and R. Seltmann and {De Grave}, J.",
note = "Publisher Copyright: {\textcopyright} 2018, Pleiades Publishing, Ltd.",
year = "2018",
month = aug,
day = "1",
doi = "10.1134/S1028334X18080238",
language = "English",
volume = "481",
pages = "1033--1036",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Age of the Raygorodok Au-bearing Gabbro—Monzodiorite Massif (Northern Kazakhstan)

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.

N1 - Publisher Copyright: © 2018, Pleiades Publishing, Ltd.

PY - 2018/8/1

Y1 - 2018/8/1

N2 - 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.

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.

UR - http://www.scopus.com/inward/record.url?scp=85052823620&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18080238

DO - 10.1134/S1028334X18080238

M3 - Article

AN - SCOPUS:85052823620

VL - 481

SP - 1033

EP - 1036

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 16360622