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New Data on the Age of Detrital Zircons from the Kokdjot Group and Bolshekaroi Formation, Malyi Karatau (Southern Kazakhstan). / Khudoley, A. K. Khudoley; Alexeiev, D. V. ; DuFrane, S.A.; Degtyarev, K. E. ; Letnikova, E. F. .

In: Doklady Earth Sciences, Vol. 479, No. 1, 03.2018, p. 316-319.

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

Harvard

Khudoley, AKK, Alexeiev, DV, DuFrane, SA, Degtyarev, KE & Letnikova, EF 2018, 'New Data on the Age of Detrital Zircons from the Kokdjot Group and Bolshekaroi Formation, Malyi Karatau (Southern Kazakhstan)', Doklady Earth Sciences, vol. 479, no. 1, pp. 316-319. https://doi.org/10.1134/S1028334X18030182

APA

Khudoley, A. K. K., Alexeiev, D. V., DuFrane, S. A., Degtyarev, K. E., & Letnikova, E. F. (2018). New Data on the Age of Detrital Zircons from the Kokdjot Group and Bolshekaroi Formation, Malyi Karatau (Southern Kazakhstan). Doklady Earth Sciences, 479(1), 316-319. https://doi.org/10.1134/S1028334X18030182

Vancouver

Khudoley AKK, Alexeiev DV, DuFrane SA, Degtyarev KE, Letnikova EF. New Data on the Age of Detrital Zircons from the Kokdjot Group and Bolshekaroi Formation, Malyi Karatau (Southern Kazakhstan). Doklady Earth Sciences. 2018 Mar;479(1):316-319. https://doi.org/10.1134/S1028334X18030182

Author

Khudoley, A. K. Khudoley ; Alexeiev, D. V. ; DuFrane, S.A. ; Degtyarev, K. E. ; Letnikova, E. F. . / New Data on the Age of Detrital Zircons from the Kokdjot Group and Bolshekaroi Formation, Malyi Karatau (Southern Kazakhstan). In: Doklady Earth Sciences. 2018 ; Vol. 479, No. 1. pp. 316-319.

BibTeX

@article{a33ccacf165f40b885b39fe618ea0361,
title = "New Data on the Age of Detrital Zircons from the Kokdjot Group and Bolshekaroi Formation, Malyi Karatau (Southern Kazakhstan)",
abstract = "U-Pb dating of detrital zircon from the Kokdjot Group and Bolshekaroi Formation (Malyi Karatau) yielded for all the samples age clusters at about 800-805, 855-890, 1980-2100, and 2440-2470 Ma. The Kolmogorov-Smirnov test suggests they have identical provenance sources. The Kokdjot Group and Bolshekaroi Formation ages are presumably Neoproterozoic, not older than 800 Ma, though a somewhat younger age (not older 770 Ma) cannot be ruled out.",
keywords = "SHAN",
author = "Khudoley, {A. K. Khudoley} and Alexeiev, {D. V.} and S.A. DuFrane and Degtyarev, {K. E.} and Letnikova, {E. F.}",
year = "2018",
month = mar,
doi = "10.1134/S1028334X18030182",
language = "Английский",
volume = "479",
pages = "316--319",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - New Data on the Age of Detrital Zircons from the Kokdjot Group and Bolshekaroi Formation, Malyi Karatau (Southern Kazakhstan)

AU - Khudoley, A. K. Khudoley

AU - Alexeiev, D. V.

AU - DuFrane, S.A.

AU - Degtyarev, K. E.

AU - Letnikova, E. F.

PY - 2018/3

Y1 - 2018/3

N2 - U-Pb dating of detrital zircon from the Kokdjot Group and Bolshekaroi Formation (Malyi Karatau) yielded for all the samples age clusters at about 800-805, 855-890, 1980-2100, and 2440-2470 Ma. The Kolmogorov-Smirnov test suggests they have identical provenance sources. The Kokdjot Group and Bolshekaroi Formation ages are presumably Neoproterozoic, not older than 800 Ma, though a somewhat younger age (not older 770 Ma) cannot be ruled out.

AB - U-Pb dating of detrital zircon from the Kokdjot Group and Bolshekaroi Formation (Malyi Karatau) yielded for all the samples age clusters at about 800-805, 855-890, 1980-2100, and 2440-2470 Ma. The Kolmogorov-Smirnov test suggests they have identical provenance sources. The Kokdjot Group and Bolshekaroi Formation ages are presumably Neoproterozoic, not older than 800 Ma, though a somewhat younger age (not older 770 Ma) cannot be ruled out.

KW - SHAN

U2 - 10.1134/S1028334X18030182

DO - 10.1134/S1028334X18030182

M3 - статья

VL - 479

SP - 316

EP - 319

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 35200511