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Main stages of tectonomagmatic activity of the Tuva–Mongolian microcontinent in the Precambrian : data on the U–Pb age of zircons. / Letnikova, E. F.; Shkolnik, S. I.; Letnikov, F. A. et al.

In: Doklady Earth Sciences, Vol. 474, No. 2, 01.06.2017, p. 668-673.

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

Harvard

Letnikova, EF, Shkolnik, SI, Letnikov, FA, Karakovskii, EA, Kostitsyn, YA, Vishnevskaya, IA, Reznitskii, LZ, Ivanov, AV & Prochenkin, AI 2017, 'Main stages of tectonomagmatic activity of the Tuva–Mongolian microcontinent in the Precambrian: data on the U–Pb age of zircons', Doklady Earth Sciences, vol. 474, no. 2, pp. 668-673. https://doi.org/10.1134/S1028334X17060113

APA

Letnikova, E. F., Shkolnik, S. I., Letnikov, F. A., Karakovskii, E. A., Kostitsyn, Y. A., Vishnevskaya, I. A., Reznitskii, L. Z., Ivanov, A. V., & Prochenkin, A. I. (2017). Main stages of tectonomagmatic activity of the Tuva–Mongolian microcontinent in the Precambrian: data on the U–Pb age of zircons. Doklady Earth Sciences, 474(2), 668-673. https://doi.org/10.1134/S1028334X17060113

Vancouver

Letnikova EF, Shkolnik SI, Letnikov FA, Karakovskii EA, Kostitsyn YA, Vishnevskaya IA et al. Main stages of tectonomagmatic activity of the Tuva–Mongolian microcontinent in the Precambrian: data on the U–Pb age of zircons. Doklady Earth Sciences. 2017 Jun 1;474(2):668-673. doi: 10.1134/S1028334X17060113

Author

Letnikova, E. F. ; Shkolnik, S. I. ; Letnikov, F. A. et al. / Main stages of tectonomagmatic activity of the Tuva–Mongolian microcontinent in the Precambrian : data on the U–Pb age of zircons. In: Doklady Earth Sciences. 2017 ; Vol. 474, No. 2. pp. 668-673.

BibTeX

@article{1dd8a01f5b8f4e2aa2a002504a141f3b,
title = "Main stages of tectonomagmatic activity of the Tuva–Mongolian microcontinent in the Precambrian: data on the U–Pb age of zircons",
abstract = "The U–Pb age of zircons from Ediacaran sandstones of the cover of the Tuva–Mongolian microcontinent and the rocks of its Early Precambrian basement (Gargan block) was analyzed by the LA–ICP–MS method. The major stages of tectonomagmatic activity of this block include the Neoarchean, Paleoproterozoic (no younger than 2 Ga), and Neoproterozoic. Comparison of the age of zircons from Ediacaran terrigenous rocks of the Tuva–Mongolian microcontinent and sandstones of the reference sections of the Ediacaran shelf of the Siberian platform undeniably indicates their independent accumulation.",
author = "Letnikova, {E. F.} and Shkolnik, {S. I.} and Letnikov, {F. A.} and Karakovskii, {E. A.} and Kostitsyn, {Yu A.} and Vishnevskaya, {I. A.} and Reznitskii, {L. Z.} and Ivanov, {A. V.} and Prochenkin, {A. I.}",
year = "2017",
month = jun,
day = "1",
doi = "10.1134/S1028334X17060113",
language = "English",
volume = "474",
pages = "668--673",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Main stages of tectonomagmatic activity of the Tuva–Mongolian microcontinent in the Precambrian

T2 - data on the U–Pb age of zircons

AU - Letnikova, E. F.

AU - Shkolnik, S. I.

AU - Letnikov, F. A.

AU - Karakovskii, E. A.

AU - Kostitsyn, Yu A.

AU - Vishnevskaya, I. A.

AU - Reznitskii, L. Z.

AU - Ivanov, A. V.

AU - Prochenkin, A. I.

PY - 2017/6/1

Y1 - 2017/6/1

N2 - The U–Pb age of zircons from Ediacaran sandstones of the cover of the Tuva–Mongolian microcontinent and the rocks of its Early Precambrian basement (Gargan block) was analyzed by the LA–ICP–MS method. The major stages of tectonomagmatic activity of this block include the Neoarchean, Paleoproterozoic (no younger than 2 Ga), and Neoproterozoic. Comparison of the age of zircons from Ediacaran terrigenous rocks of the Tuva–Mongolian microcontinent and sandstones of the reference sections of the Ediacaran shelf of the Siberian platform undeniably indicates their independent accumulation.

AB - The U–Pb age of zircons from Ediacaran sandstones of the cover of the Tuva–Mongolian microcontinent and the rocks of its Early Precambrian basement (Gargan block) was analyzed by the LA–ICP–MS method. The major stages of tectonomagmatic activity of this block include the Neoarchean, Paleoproterozoic (no younger than 2 Ga), and Neoproterozoic. Comparison of the age of zircons from Ediacaran terrigenous rocks of the Tuva–Mongolian microcontinent and sandstones of the reference sections of the Ediacaran shelf of the Siberian platform undeniably indicates their independent accumulation.

UR - http://www.scopus.com/inward/record.url?scp=85024120354&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17060113

DO - 10.1134/S1028334X17060113

M3 - Article

AN - SCOPUS:85024120354

VL - 474

SP - 668

EP - 673

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 10092136