Results 71 to 80 of about 109 (102)
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Stratigraphy and Geological Correlation, 2011
A new way of formation of the problematic Molar Tooth (MT) structures, which, along with stromatolites, could be considered as a “visiting card” of the Riphean, was examined on the example of carbonate sediments of the Riphean Sukhaya Tunguska Formation from the Turukhansk Uplift, Siberia.
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A new way of formation of the problematic Molar Tooth (MT) structures, which, along with stromatolites, could be considered as a “visiting card” of the Riphean, was examined on the example of carbonate sediments of the Riphean Sukhaya Tunguska Formation from the Turukhansk Uplift, Siberia.
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Lithology and Mineral Resources, 2001
The Linok Formation is made up of clayey and carbonate strata, 180–300 m thick, formed at the terminal Middle Riphean on the northwestern margin of the Siberian Platform. In the modern structure, it is exposed in the lower part of the Turukhansk Uplift section.
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The Linok Formation is made up of clayey and carbonate strata, 180–300 m thick, formed at the terminal Middle Riphean on the northwestern margin of the Siberian Platform. In the modern structure, it is exposed in the lower part of the Turukhansk Uplift section.
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Late Riphean microbial colonies adapted to desiccating environments
Doklady Earth Sciences, 2012D. V. Grazhdankin +2 more
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Evidence for Late Riphean granite formation in the Polar Urals
Doklady Earth Sciences, 2012A. A. Soboleva +6 more
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Late Riphean plagiogranites of Kuznetskii Alatau: Composition, age, and sources
Doklady Earth Sciences, 2006S. N. Rudnev +3 more
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New data on Late Riphean volcanism in northern part of the Yenisey ridge
International Geology Review, 1973A.G. Mironov, A.D. Nozhkin
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New data on Late Riphean intraplate granitoid magmatism in the Transangarian Yenisei Ridge
Doklady Earth Sciences, 2013I. I. Likhanov +2 more
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Radiation therapy‐associated toxicity: Etiology, management, and prevention
Ca-A Cancer Journal for Clinicians, 2021Kyle Wang
exaly

