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Depositional environments and diagenesis of devonian black shales (Case study volga-ural Region, Russia) of Upper Devonian formations from Volga-Ural region, Russian Federation. The main purpose of studying was a
Bryozoans and Brachiopods from the Famennian (Upper Devonian) of the Central Russian Platform of the Zadonsk Regional horizon (Lower Famennian, Upper Devonian) have yielded two species of trepostome
Traditional and precision methods for studying porous space of oil-bearing formation (Upper Devonian), and Tula and Bobrikovskian (Lower Carboniferous) horizons, as well as carbonate
Traditional and precision methods for studying porous space of oil-bearing formation (Upper Devonian), and Tula and Bobrikovskian (Lower Carboniferous) horizons, as well as carbonate
Oldest known naiaditid bivalve from the high-latitude Late Devonian (Famennian) of South Africa offers clues to survival strategies following the Hangenberg mass extinction) marked the end of the Devonian period and had a significant impact on the palaeoecology and faunal
Oldest known naiaditid bivalve from the high-latitude Late Devonian (Famennian) of South Africa offers clues to survival strategies following the Hangenberg mass extinction) marked the end of the Devonian period and had a significant impact on the palaeoecology and faunal
A new genus of ptyctodont (Placodermi) from the late Devonian of Baltic area to as Chelyophorus pskovensis Obruchev, 1947 from the Early Frasnian (Late Devonian) of Velikaya River, Pskov Region
The Dzerzhinka Section (eastern slope of the South Urals): An overview of the fauna and facies around the Devonian-Carboniferous boundaryTheDevonian-Carboniferous boundary section near the village of Dzerzhinka (vicinity of
Palaeoecology of Famennian-Tournaisian (Late Devonian-Early Carboniferous) bryozoans from central and southern regions of Russia. The palaeoecology of Famennian-Tournaisian (Late Devonian-Early Carboniferous) bryozoans from central and southern
Sedimentary characteristics and evolution of Domanik facies from the Devonian–Carboniferous regression in the southern Volga-Ural Basin Devonian to Lower Carboniferous age in the Volga-Ural and Timan-Pechora petroleum provinces. Different
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