Results 61 to 70 of about 119 (100)
T.A. Vovchina, A.A. Soboleva
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Stromatolites and pulsed oxygenation events in the Mesoproterozoic Longjiayuan formation of western Henan: evidence for life-environment co-evolution. [PDF]
Li Q, Zheng D, Sun F.
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Fungal remains from the Late Riphean
Paleontological Journal, 2006The paper describes organic remains of one billion years old from the Lakhanda microbiota of the Uchur-Maya Region of southeastern Siberia. The microfossils were discovered on organic sapropelic films. The preserved morphological characters and some developmental stages of the ancient organisms, which are fixed in fossil state, suggest that some of ...
Podkovyrov V N, V N Podkovyrov
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Late Riphean stage of development of the Russian plate
International Geology Review, 1979(1979). Late Riphean stage of development of the Russian plate. International Geology Review: Vol. 21, No. 2, pp. 167-180.
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Russian Geology and Geophysics, 2010
Abstract New structural, petrological, chemical, isotope, and paleomagnetic data have provided clues to the Late Riphean–Paleozoic history of the Uda–Vitim island arc system (UVIAS) in the Transbaikalian sector of the Paleoasian ocean, as part of the Transbaikalian zone of Paleozoids.
I.V. Gordienko +11 more
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Abstract New structural, petrological, chemical, isotope, and paleomagnetic data have provided clues to the Late Riphean–Paleozoic history of the Uda–Vitim island arc system (UVIAS) in the Transbaikalian sector of the Paleoasian ocean, as part of the Transbaikalian zone of Paleozoids.
I.V. Gordienko +11 more
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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.
P Yu Petrov, Petrov P Yu
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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.
P Yu Petrov, Petrov P Yu
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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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Late Riphean microbial colonies adapted to desiccating environments
Doklady Earth Sciences, 2012Dmitry Grazhdankin, Maslov A V
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