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Rugosoopsis : a new group of Upper Riphean animals
Geological Society, London, Special Publications, 2007Abstract The Upper Riphean Lakhanda biota (from the Uchur-Mayai region of SE Siberia) contains abundant, well preserved and highly biodiverse microfossil assemblages including Rugosoopsis microfossils, characterized by a uniform shape, with prominent closely transversely spaced wrinkles on the outer ...
T. N. Hermann, V. N. Podkovyrov
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Russian Geology and Geophysics, 1993
Under consideration are the composition, structure and depositional environments of the Upper-Riphean Dzhura Reef Formation in the southeastern Yenisei Ridge. It was shown that a carbonate platform with reef-like stromatolithic rim structures has been formed in the Dzhurian time. It turned into a deep basin northward. It was shown that the evolution of
E. M. Khabarov, G. I. Tanygin
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Under consideration are the composition, structure and depositional environments of the Upper-Riphean Dzhura Reef Formation in the southeastern Yenisei Ridge. It was shown that a carbonate platform with reef-like stromatolithic rim structures has been formed in the Dzhurian time. It turned into a deep basin northward. It was shown that the evolution of
E. M. Khabarov, G. I. Tanygin
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Lithology and Mineral Resources, 2003
The paper presents mineralogical, crystallochemical, and Rb–Sr age data on globular layer silicates of the glauconitic series from lower horizons of the Upper Riphean Kil'din Group, Srednii Peninsula. Chloritization significantly changed the globular Al-glauconite in sandstones of the Parajarvinskaya Formation.
T. A. Ivanovskaya +3 more
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The paper presents mineralogical, crystallochemical, and Rb–Sr age data on globular layer silicates of the glauconitic series from lower horizons of the Upper Riphean Kil'din Group, Srednii Peninsula. Chloritization significantly changed the globular Al-glauconite in sandstones of the Parajarvinskaya Formation.
T. A. Ivanovskaya +3 more
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Russian Journal of Pacific Geology, 2017
Graphitic and graphite varieties are distinguished in the carbonaceous shales of the Riphean Upper Nyatygran Subformation in the Melgin fragment of the Turan block, eastern Bureya Massif. The protolith of the graphitic shales had a terrigenous source related to island-arc volcanism.
A. A. Cherepanov +3 more
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Graphitic and graphite varieties are distinguished in the carbonaceous shales of the Riphean Upper Nyatygran Subformation in the Melgin fragment of the Turan block, eastern Bureya Massif. The protolith of the graphitic shales had a terrigenous source related to island-arc volcanism.
A. A. Cherepanov +3 more
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Clay minerals in Upper Riphean-Wendian terrigenous rocks and in the base of the Markovsk deposit
International Geology Review, 1974D.D. Kotel'nikov, T.V. Florenskaya
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