Biostratigraphy of deposits upper riphean in the Biryusa structure-facial zone by stromatolites and microphitolites
Authors:
About authors
- post-graduate student National Mineral Resources University (Mining University)
Abstract
Riphean deposits in the Biryusa Structure-Facial Zone is represented by the Karagass Group consist of the Tagul and Ipsit Formations. Stromatolites and microphitolites are common in the Prisayan region. Upper Riphean complex of Stromatolites and microphitolites is determinate in Biryusa Structure-Facial Zone. Each is compared with same of association in the stratotype section of Patom’s Zone.
Область исследования:
(Archived) Geology and metallogeny
References
- Dolnik Т.А. Stromatolites of bases sicvens in the Precambrian of Sayan-Baikal Area: Irkutsk: Vostochno-Sibirskya Pravda, 1982. 183 p.
- Dolnik Т.А. Stromatolites and micro-phytolites in Riphean and Vendian stratigraphy of the folded periphery of the southern Siberian craton: Novosibirsk: Publishing officeof the SB RA S. 2000. 320 p.
- Gladkochub D.P., Donskaya T.V., Mazukabzov A.M., Stanevich A.M., Sklyarov E.V., Ponomarchuk V.A.Signature of Precambrian extension events in the Southern Siberian Craton // Russian geology and geophysics. 2007, V.48. N.1. P.22-41.
- The orders Interdepartmental Stratigraphic Committee and its constant commissions. The State investigation of stratigraphy Precambrian and Phanerozoic of Russia / VSEGEY. Saint Peter burg, 2008. Iss.38. 131 p.
- The Stratigraphic code of Russia / VSEGEY. Saint Petersburg, 2006. 96 p.
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