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


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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.

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A. Kuznetsov

Institute of Precambrian Geology and Geochronology

编辑信件的主要联系方式.
Email: antonbor9@mail.ru
俄罗斯联邦, St. Petersburg, 199034

I. Vasilieva

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
俄罗斯联邦, St. Petersburg, 199034

D. Sitkina

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
俄罗斯联邦, St. Petersburg, 199034

Z. Smirnova

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
俄罗斯联邦, St. Petersburg, 199034

O. Kaurova

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
俄罗斯联邦, St. Petersburg, 199034

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