Zobrazeno 1 - 10
of 12
pro vyhledávání: '"O. V. Zerkal"'
Publikováno v:
Landslides: Detection, Prediction and Monitoring ISBN: 9783031238581
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e1f5b15b8d4abdefa2480ecb07a3e660
https://doi.org/10.1007/978-3-031-23859-8_12
https://doi.org/10.1007/978-3-031-23859-8_12
Publikováno v:
Moscow University Geology Bulletin. 74:357-363
A section of Upper Carboniferous and overlying Jurassic sediments in the area of a buried karst depression in the northwestern part of Moscow was studied. According to conodont zoning, it was revealed that in the section of the karst depression the P
Publikováno v:
Engineering Geology. 13:40-53
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 833:012169
Justification of seismic triggering of large prehistoric rockslides that originated on the slopes of anticlinal ridges armoured by thick carbonate units has been performed by examples of the gigantic Seimareh rockslide in Zagros (Iran) and two struct
Publikováno v:
Moscow University Geology Bulletin. 72:255-262
Two stages are distinguished in the study of Quaternary deposits in Crimea. At the first stage (from the late 19th century to the 1960s), the stratigraphic description of Quaternary strata was based on the allocation of terraced complexes (marine ter
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :27-34
In the study of Quaternary deposits of the Crimea selected two phases. In the first stage (since the late XIX century to the sixties of XX century) stratigraphic description of the Quaternary strata was based on the allocation of terraced complexes (
Autor:
E. A. Shcherbinina, G. K. Kozlova, R. R. Gabdullin, E. V. Yakovishina, A. M. Akuba, E. N. Samarin, L. F. Kopaevich, O. V. Zerkal, N. T. Zagrachev
Publikováno v:
Moscow University Geology Bulletin. 67:218-232
For the first time, a complex lithological-stratigraphic and facial study of the Aptian-Cenomanian sediments of the Abkhazian zone of the Northwestern Caucasus was carried in sections of the Mzymta and Khipsta river valleys. As a result, the areas of