Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Evgeny S. SOBOLEV"'
Publikováno v:
Axioms, Vol 12, Iss 6, p 594 (2023)
Dynamic loading causes (1) a substantial change in the strength and deformation parameters of sandy soil and (2) excessive viscoplastic deformation. The goal of this study is to create a new analytical solution to the problem of the settlement of (1)
Externí odkaz:
https://doaj.org/article/cdf106f0456e4700bebc46d347710cc8
Autor:
Nikolay G. ZVERKOV, Dmitry V. GRIGORIEV, Andrzej S. WOLNIEWICZ, Alexey G. KONSTANTINOV, Evgeny S. SOBOLEV
Publikováno v:
Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 113:51-74
The first ichthyosaurian specimens discovered from the Upper Triassic of the Russian Arctic (Kotelny Island, New Siberian Islands) are described herein. They include the remains of large- to small-bodied ichthyosaurians originating from six stratigra
Publikováno v:
Interexpo GEO-Siberia. 2:201-206
The volcanogenic formations of the middle part of the Pronchishchev ridge are considered. Based on new data from the lithological, petrographic, geochemical studies of igneous and volcanogenic sedimentary rocks and stratigraphic studies of the Upper
Autor:
Alexander L. Beisel, Evgeny S. Sobolev
Publikováno v:
Interexpo GEO-Siberia. 2:3-7
In the south of Western Siberia, there are lakes of a specific shape - teardrop-shaped, with a convex rounded side facing northeast and a pointed end-to the southwest. They are found only in the distribution area of the definite grivas relief. There
Autor:
Evgeny S. Sobolev, R. V. Kutygin, Alexander S. Biakov, Yuri D. Zakharov, David P.G. Bond, Micha Horacek
Publikováno v:
Morphogenesis, Environmental Stress and Reverse Evolution ISBN: 9783030472788
We propose an updated ammonoid zonation for the Permian–Triassic boundary succession (the lower Nekuchan Formation) in the Verkhoyansk region of Siberia: (1) Otoceras concavum zone (uppermost Changhsingian); (2) Otoceras boreale zone (lowermost Ind
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::692bd802fc657e523a9e52b0eb0c06f2
https://doi.org/10.1007/978-3-030-47279-5_10
https://doi.org/10.1007/978-3-030-47279-5_10
Autor:
Evgeny S. Sobolev, Eugen Grădinaru
Publikováno v:
Central European Geology. 53:261-309
The occurrence of the heteromorphic ammonoid Rhabdoceras suessi Hauer, 1860, is recorded for the first time in the Upper Triassic limestone of the Timon-Ciungi olistolith in the Rarau Syncline, Eastern Carpathians. A single specimen of Rhabdoceras su