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Age of carbonates and phosphorites in the sedimentary cover of the Tuva-Mongolian microcontinent. / Kuznetsov, A. B.; Vasilieva, I. M.; Sitkina, D. R.; Smirnova, Z. B.; Kaurova, O. K.

в: Doklady Earth Sciences, Том 479, № 1, 2018, стр. 282-285.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Kuznetsov, AB, Vasilieva, IM, Sitkina, DR, Smirnova, ZB & Kaurova, OK 2018, 'Age of carbonates and phosphorites in the sedimentary cover of the Tuva-Mongolian microcontinent', Doklady Earth Sciences, Том. 479, № 1, стр. 282-285. https://doi.org/10.1134/S1028334X18030030

APA

Kuznetsov, A. B., Vasilieva, I. M., Sitkina, D. R., Smirnova, Z. B., & Kaurova, O. K. (2018). Age of carbonates and phosphorites in the sedimentary cover of the Tuva-Mongolian microcontinent. Doklady Earth Sciences, 479(1), 282-285. https://doi.org/10.1134/S1028334X18030030

Vancouver

Kuznetsov AB, Vasilieva IM, Sitkina DR, Smirnova ZB, Kaurova OK. Age of carbonates and phosphorites in the sedimentary cover of the Tuva-Mongolian microcontinent. Doklady Earth Sciences. 2018;479(1):282-285. https://doi.org/10.1134/S1028334X18030030

Author

Kuznetsov, A. B. ; Vasilieva, I. M. ; Sitkina, D. R. ; Smirnova, Z. B. ; Kaurova, O. K. / Age of carbonates and phosphorites in the sedimentary cover of the Tuva-Mongolian microcontinent. в: Doklady Earth Sciences. 2018 ; Том 479, № 1. стр. 282-285.

BibTeX

@article{5ac6c8a7c4284dbd8a4f9a7c6afeba7a,
title = "Age of carbonates and phosphorites in the sedimentary cover of the Tuva-Mongolian microcontinent",
abstract = "The ages of the two main stages of carbonate cover formation within the Tuva-Mongolian microcontinent have been determined. The Pb-Pb age and Sr-chemostratigraphic characteristics of the carbonate rocks of the Irkutnaya, Agaringol, and Zabita formations, as well as of the Zabita Formation phosphorite, demonstrate that the first stage began in the Middle Riphean (Late Ectasian) at about 1290 Ma and the second stage started in the Early Vendian (Early Ediacaran) at 630-600 Ma. The accumulation of phosphorite deposits started in the Ediacaran at about 580 Ma.",
author = "Kuznetsov, {A. B.} and Vasilieva, {I. M.} and Sitkina, {D. R.} and Smirnova, {Z. B.} and Kaurova, {O. K.}",
note = "Publisher Copyright: {\textcopyright} Pleiades Publishing, Ltd., 2018 & A.B. Kuznetsov, I.M. Vasilieva, D.R. Sitkina, Z.B. Smirnova, O.K. Kaurova, 2018.. Copyright: Copyright 2019 Elsevier B.V., All rights reserved.",
year = "2018",
doi = "10.1134/S1028334X18030030",
language = "English",
volume = "479",
pages = "282--285",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - Age of carbonates and phosphorites in the sedimentary cover of the Tuva-Mongolian microcontinent

AU - Kuznetsov, A. B.

AU - Vasilieva, I. M.

AU - Sitkina, D. R.

AU - Smirnova, Z. B.

AU - Kaurova, O. K.

N1 - Publisher Copyright: © Pleiades Publishing, Ltd., 2018 & A.B. Kuznetsov, I.M. Vasilieva, D.R. Sitkina, Z.B. Smirnova, O.K. Kaurova, 2018.. Copyright: Copyright 2019 Elsevier B.V., All rights reserved.

PY - 2018

Y1 - 2018

N2 - The ages of the two main stages of carbonate cover formation within the Tuva-Mongolian microcontinent have been determined. The Pb-Pb age and Sr-chemostratigraphic characteristics of the carbonate rocks of the Irkutnaya, Agaringol, and Zabita formations, as well as of the Zabita Formation phosphorite, demonstrate that the first stage began in the Middle Riphean (Late Ectasian) at about 1290 Ma and the second stage started in the Early Vendian (Early Ediacaran) at 630-600 Ma. The accumulation of phosphorite deposits started in the Ediacaran at about 580 Ma.

AB - The ages of the two main stages of carbonate cover formation within the Tuva-Mongolian microcontinent have been determined. The Pb-Pb age and Sr-chemostratigraphic characteristics of the carbonate rocks of the Irkutnaya, Agaringol, and Zabita formations, as well as of the Zabita Formation phosphorite, demonstrate that the first stage began in the Middle Riphean (Late Ectasian) at about 1290 Ma and the second stage started in the Early Vendian (Early Ediacaran) at 630-600 Ma. The accumulation of phosphorite deposits started in the Ediacaran at about 580 Ma.

UR - http://www.scopus.com/inward/record.url?scp=85063877044&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18030030

DO - 10.1134/S1028334X18030030

M3 - Article

AN - SCOPUS:85063877044

VL - 479

SP - 282

EP - 285

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 75979037