Geochemical Environments of the Archean–Proterozoic
- Авторы: Kuznetsov V.1
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Учреждения:
- Gubkin Russian State University of Oil and Gas
- Выпуск: Том 488, № 2 (2019)
- Страницы: 1148-1151
- Раздел: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/195482
- DOI: https://doi.org/10.1134/S1028334X19100052
- ID: 195482
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Аннотация
In the Precambrian sequence, namely, in the Proterozoic, Archean calcium and ferruginous carbonate rocks changed to magnesian carbonate ones. This correlates with the massive development of cyanobacteria, the carbon dioxide absorption and oxygen generation of which led to a change from the Archean acidic reducing environments to alkaline oxidizing environments in the Proterozoic.
Об авторах
V. Kuznetsov
Gubkin Russian State University of Oil and Gas
Автор, ответственный за переписку.
Email: vgkuz@yandex.ru
Россия, Moscow, 119991