Age of Carbonates and Phosphorites in the Sedimentary Cover of the Tuva–Mongolian Microcontinent


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

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.

Авторлар туралы

A. Kuznetsov

Institute of Precambrian Geology and Geochronology

Хат алмасуға жауапты Автор.
Email: antonbor9@mail.ru
Ресей, St. Petersburg, 199034

I. Vasilieva

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
Ресей, St. Petersburg, 199034

D. Sitkina

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
Ресей, St. Petersburg, 199034

Z. Smirnova

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
Ресей, St. Petersburg, 199034

O. Kaurova

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
Ресей, St. Petersburg, 199034

Қосымша файлдар

Қосымша файлдар
Әрекет
1. JATS XML

© Pleiades Publishing, Ltd., 2018