Paleoproterozoic Age of Carbonates and Trondhjemites of the Central Azov Group: Sr Isotope Chemostratigraphy and U–Pb Geochronology
- Авторлар: Kuznetsov A.B.1, Lobach–Zhuchenko S.B.1, Kaulina T.V.2, Konstantinova G.V.2
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Мекемелер:
- Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences
- Geological Institute, Kola Science Center, Russian Academy of Sciences
- Шығарылым: Том 484, № 2 (2019)
- Беттер: 142-145
- Бөлім: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/194591
- DOI: https://doi.org/10.1134/S1028334X19020211
- ID: 194591
Дәйексөз келтіру
Аннотация
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.
Авторлар туралы
A. Kuznetsov
Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences
Хат алмасуға жауапты Автор.
Email: antonbor9@mail.ru
Ресей, St. Petersburg, 199034
S. Lobach–Zhuchenko
Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences
Email: antonbor9@mail.ru
Ресей, St. Petersburg, 199034
T. Kaulina
Geological Institute, Kola Science Center, Russian Academy of Sciences
Email: antonbor9@mail.ru
Ресей, Apatity, 184200
G. Konstantinova
Geological Institute, Kola Science Center, Russian Academy of Sciences
Email: antonbor9@mail.ru
Ресей, Apatity, 184200
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