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Isotope stratigraphy and U-Pb dating of detrital zircons from the Vendian-Cambrian deposits of the North Muya block. / Vishnevskaya, I. A.; Letnikova, E. F.; Kanygina, N. A. et al.

In: Russian Geology and Geophysics, Vol. 59, No. 11, 01.11.2018, p. 1433-1449.

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

Harvard

Vishnevskaya, IA, Letnikova, EF, Kanygina, NA, Proshenkin, AI, Soloshenko, NG, Vetrov, EV & Kiseleva, VY 2018, 'Isotope stratigraphy and U-Pb dating of detrital zircons from the Vendian-Cambrian deposits of the North Muya block', Russian Geology and Geophysics, vol. 59, no. 11, pp. 1433-1449. https://doi.org/10.1016/j.rgg.2018.10.004

APA

Vishnevskaya, I. A., Letnikova, E. F., Kanygina, N. A., Proshenkin, A. I., Soloshenko, N. G., Vetrov, E. V., & Kiseleva, V. Y. (2018). Isotope stratigraphy and U-Pb dating of detrital zircons from the Vendian-Cambrian deposits of the North Muya block. Russian Geology and Geophysics, 59(11), 1433-1449. https://doi.org/10.1016/j.rgg.2018.10.004

Vancouver

Vishnevskaya IA, Letnikova EF, Kanygina NA, Proshenkin AI, Soloshenko NG, Vetrov EV et al. Isotope stratigraphy and U-Pb dating of detrital zircons from the Vendian-Cambrian deposits of the North Muya block. Russian Geology and Geophysics. 2018 Nov 1;59(11):1433-1449. doi: 10.1016/j.rgg.2018.10.004

Author

Vishnevskaya, I. A. ; Letnikova, E. F. ; Kanygina, N. A. et al. / Isotope stratigraphy and U-Pb dating of detrital zircons from the Vendian-Cambrian deposits of the North Muya block. In: Russian Geology and Geophysics. 2018 ; Vol. 59, No. 11. pp. 1433-1449.

BibTeX

@article{c0190282acfa4af78c8700b7d33abb20,
title = "Isotope stratigraphy and U-Pb dating of detrital zircons from the Vendian-Cambrian deposits of the North Muya block",
abstract = "U-Pb dating of detrital zircons from the sandstones of the Mamakan Formation has been made. Geochemical and isotope parameters of the carbonate deposits of the Yanguda Formation in the Vendian-Cambrian cover of the North Muya continental block have been estimated. It has been established that only the Neoproterozoic (630-915 Ma) rocks of the North Muya block were the provenances of terrigenous material. In the least altered carbonate rocks of the Yanguda Formation, the 87Sr/86Sr ratio is within 0.70814-0.70879 and δ13C varies from -0.4 to + 1.9‰. Comparison of the evaluated isotope parameters with those of carbonate rocks of typical Vendian-Cambrian sections shows that the carbonate deposits of the Yanguda Formation accumulated in the Early Cambrian, about 520 Ma. Sedimentation of the Mamakan and Yanguda Formations took place in the local sedimentary basin in the Vendian-Early Cambrian, in the absence of tectonic activity within the North Muya block. Detrital material that formed during the destruction of the rocks of the Siberian Platform basement and cover was not supplied into the basin.",
keywords = "isotope chemostratigraphy, passive continental margin, provenances, reconstructions, Siberian Platform, U-Pb dating of detrital zircons, KUZNETSK-ALATAU, TUVA-MONGOLIAN MICROCONTINENT, CENTRAL-ASIAN FOLDBELT, CONTINENTAL-CRUST, 3 GORGES, CHEMOSTRATIGRAPHY, provenances, reconstructions, SIBERIAN CRATON, SOUTH CHINA, SR-ISOTOPE, AGE",
author = "Vishnevskaya, {I. A.} and Letnikova, {E. F.} and Kanygina, {N. A.} and Proshenkin, {A. I.} and Soloshenko, {N. G.} and Vetrov, {E. V.} and Kiseleva, {V. Yu}",
year = "2018",
month = nov,
day = "1",
doi = "10.1016/j.rgg.2018.10.004",
language = "English",
volume = "59",
pages = "1433--1449",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "11",

}

RIS

TY - JOUR

T1 - Isotope stratigraphy and U-Pb dating of detrital zircons from the Vendian-Cambrian deposits of the North Muya block

AU - Vishnevskaya, I. A.

AU - Letnikova, E. F.

AU - Kanygina, N. A.

AU - Proshenkin, A. I.

AU - Soloshenko, N. G.

AU - Vetrov, E. V.

AU - Kiseleva, V. Yu

PY - 2018/11/1

Y1 - 2018/11/1

N2 - U-Pb dating of detrital zircons from the sandstones of the Mamakan Formation has been made. Geochemical and isotope parameters of the carbonate deposits of the Yanguda Formation in the Vendian-Cambrian cover of the North Muya continental block have been estimated. It has been established that only the Neoproterozoic (630-915 Ma) rocks of the North Muya block were the provenances of terrigenous material. In the least altered carbonate rocks of the Yanguda Formation, the 87Sr/86Sr ratio is within 0.70814-0.70879 and δ13C varies from -0.4 to + 1.9‰. Comparison of the evaluated isotope parameters with those of carbonate rocks of typical Vendian-Cambrian sections shows that the carbonate deposits of the Yanguda Formation accumulated in the Early Cambrian, about 520 Ma. Sedimentation of the Mamakan and Yanguda Formations took place in the local sedimentary basin in the Vendian-Early Cambrian, in the absence of tectonic activity within the North Muya block. Detrital material that formed during the destruction of the rocks of the Siberian Platform basement and cover was not supplied into the basin.

AB - U-Pb dating of detrital zircons from the sandstones of the Mamakan Formation has been made. Geochemical and isotope parameters of the carbonate deposits of the Yanguda Formation in the Vendian-Cambrian cover of the North Muya continental block have been estimated. It has been established that only the Neoproterozoic (630-915 Ma) rocks of the North Muya block were the provenances of terrigenous material. In the least altered carbonate rocks of the Yanguda Formation, the 87Sr/86Sr ratio is within 0.70814-0.70879 and δ13C varies from -0.4 to + 1.9‰. Comparison of the evaluated isotope parameters with those of carbonate rocks of typical Vendian-Cambrian sections shows that the carbonate deposits of the Yanguda Formation accumulated in the Early Cambrian, about 520 Ma. Sedimentation of the Mamakan and Yanguda Formations took place in the local sedimentary basin in the Vendian-Early Cambrian, in the absence of tectonic activity within the North Muya block. Detrital material that formed during the destruction of the rocks of the Siberian Platform basement and cover was not supplied into the basin.

KW - isotope chemostratigraphy

KW - passive continental margin

KW - provenances

KW - reconstructions

KW - Siberian Platform

KW - U-Pb dating of detrital zircons

KW - KUZNETSK-ALATAU

KW - TUVA-MONGOLIAN MICROCONTINENT

KW - CENTRAL-ASIAN FOLDBELT

KW - CONTINENTAL-CRUST

KW - 3 GORGES

KW - CHEMOSTRATIGRAPHY

KW - provenances, reconstructions

KW - SIBERIAN CRATON

KW - SOUTH CHINA

KW - SR-ISOTOPE

KW - AGE

UR - http://www.scopus.com/inward/record.url?scp=85056638557&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2018.10.004

DO - 10.1016/j.rgg.2018.10.004

M3 - Article

AN - SCOPUS:85056638557

VL - 59

SP - 1433

EP - 1449

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 11

ER -

ID: 17485977