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Paleoproterozoic Age of Carbonates and Trondhjemites of the Central Azov Group : Sr Isotope Chemostratigraphy and U–Pb Geochronology. / Kuznetsov, A. B.; Lobach–Zhuchenko, S. B.; Kaulina, T. V.; Konstantinova, G. V.

в: Doklady Earth Sciences, Том 484, № 2, 01.08.2019, стр. 142-145.

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

Harvard

Kuznetsov, AB, Lobach–Zhuchenko, SB, Kaulina, TV & Konstantinova, GV 2019, 'Paleoproterozoic Age of Carbonates and Trondhjemites of the Central Azov Group: Sr Isotope Chemostratigraphy and U–Pb Geochronology', Doklady Earth Sciences, Том. 484, № 2, стр. 142-145. https://doi.org/10.1134/S1028334X19020211

APA

Kuznetsov, A. B., Lobach–Zhuchenko, S. B., Kaulina, T. V., & Konstantinova, G. V. (2019). Paleoproterozoic Age of Carbonates and Trondhjemites of the Central Azov Group: Sr Isotope Chemostratigraphy and U–Pb Geochronology. Doklady Earth Sciences, 484(2), 142-145. https://doi.org/10.1134/S1028334X19020211

Vancouver

Kuznetsov AB, Lobach–Zhuchenko SB, Kaulina TV, Konstantinova GV. Paleoproterozoic Age of Carbonates and Trondhjemites of the Central Azov Group: Sr Isotope Chemostratigraphy and U–Pb Geochronology. Doklady Earth Sciences. 2019 Авг. 1;484(2):142-145. https://doi.org/10.1134/S1028334X19020211

Author

Kuznetsov, A. B. ; Lobach–Zhuchenko, S. B. ; Kaulina, T. V. ; Konstantinova, G. V. / Paleoproterozoic Age of Carbonates and Trondhjemites of the Central Azov Group : Sr Isotope Chemostratigraphy and U–Pb Geochronology. в: Doklady Earth Sciences. 2019 ; Том 484, № 2. стр. 142-145.

BibTeX

@article{24a20158693c440d94401eee6695faf1,
title = "Paleoproterozoic Age of Carbonates and Trondhjemites of the Central Azov Group: Sr Isotope Chemostratigraphy and U–Pb Geochronology",
abstract = "Abstract: The Sr isotope characteristic of carbonate rocks in the Central Azov Group has been reported (0.70322–0.70352), the Nd model age of silicate sediments has been calculated (2.34–2.31 Ga), and the U–Pb age of trondhjemites (2052 ± 5 Ma) breaking through carbonates was determined. According to the data obtained, the marine sedimentary cover of the Azov block making up the Early Precambrian Sarmatia Continent was formed in the Early Paleoproterozoic 2.23–2.34 Ga ago.",
author = "Kuznetsov, {A. B.} and Lobach–Zhuchenko, {S. B.} and Kaulina, {T. V.} and Konstantinova, {G. V.}",
note = "Publisher Copyright: {\textcopyright} 2019, Pleiades Publishing, Ltd. Copyright: Copyright 2019 Elsevier B.V., All rights reserved.",
year = "2019",
month = aug,
day = "1",
doi = "10.1134/S1028334X19020211",
language = "English",
volume = "484",
pages = "142--145",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Paleoproterozoic Age of Carbonates and Trondhjemites of the Central Azov Group

T2 - Sr Isotope Chemostratigraphy and U–Pb Geochronology

AU - Kuznetsov, A. B.

AU - Lobach–Zhuchenko, S. B.

AU - Kaulina, T. V.

AU - Konstantinova, G. V.

N1 - Publisher Copyright: © 2019, Pleiades Publishing, Ltd. Copyright: Copyright 2019 Elsevier B.V., All rights reserved.

PY - 2019/8/1

Y1 - 2019/8/1

N2 - Abstract: The Sr isotope characteristic of carbonate rocks in the Central Azov Group has been reported (0.70322–0.70352), the Nd model age of silicate sediments has been calculated (2.34–2.31 Ga), and the U–Pb age of trondhjemites (2052 ± 5 Ma) breaking through carbonates was determined. According to the data obtained, the marine sedimentary cover of the Azov block making up the Early Precambrian Sarmatia Continent was formed in the Early Paleoproterozoic 2.23–2.34 Ga ago.

AB - Abstract: The Sr isotope characteristic of carbonate rocks in the Central Azov Group has been reported (0.70322–0.70352), the Nd model age of silicate sediments has been calculated (2.34–2.31 Ga), and the U–Pb age of trondhjemites (2052 ± 5 Ma) breaking through carbonates was determined. According to the data obtained, the marine sedimentary cover of the Azov block making up the Early Precambrian Sarmatia Continent was formed in the Early Paleoproterozoic 2.23–2.34 Ga ago.

UR - http://www.scopus.com/inward/record.url?scp=85064906675&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19020211

DO - 10.1134/S1028334X19020211

M3 - Article

AN - SCOPUS:85064906675

VL - 484

SP - 142

EP - 145

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 75951166