Zobrazeno 1 - 6
of 6
pro vyhledávání: '"A. L. Dorozhko"'
Publikováno v:
Vestnik Permskogo Universiteta: Seriâ Geologiâ, Vol 16, Iss 4, Pp 354-369 (2017)
Рассматривается новейшая структура территории Верхнекамского месторождения калийных солей (ВКМКС), которая может влиять на современно
Externí odkaz:
https://doaj.org/article/87a2175906f6476b807da6bc1b43a778
Publikováno v:
Геоэкология. Инженерная геология. Гидрогеология. Геокриология. :68-76
The paper deals with the probabilistic approach to modelling the thermokarst processes induced by linear engineering structures. We have improved the previously published model and have determined the mathematical laws for the two semi-axes of the th
Publikováno v:
Вестник Пермского университета. Геология. 16:354-369
Рассматривается новейшая структура территории Верхнекамского месторождения калийных солей (ВКМКС), которая может влиять на современно
Autor:
L. A. Matveeva, K. I. Fesel, G. I. Batrak, I. A. Kostikova, Oleg Mironov, A. L. Dorozhko, I. V. Galitskaya, Irina Pozdnyakova
Publikováno v:
Water Resources. 43:1012-1022
An original procedure for mapping hydrogeological windows is based on studying the geological structure of the massif overlaying the Podol’sko-Myachkovskii aquifer, changes in the hydrodynamic and hydrogeochemical conditions in the zone of “windo
Autor:
T. V. Sukhanova, E. A. Karfidova, V. M. Makeev, N. V. Makarova, I. V. Korobova, A. L. Dorozhko
Publikováno v:
Moscow University Geology Bulletin. 70:8-17
The neotectonic structures in the southwest limb of the Voronezh Anteclise have been studied; they are very gentle bends of positive (uplift) and negative (depression) types and occur as deformations of the base of the modern Poltava Formation. These
Autor:
P. S. Miklyaev, V. M. Makeev, I. V. Korobova, T. V. Sukhanova, A. L. Dorozhko, N. V. Makarova
Publikováno v:
Moscow University Geology Bulletin. 67:209-217
The neotectonic structures of the Lower Oka (Nizhneokskii) Region formed under different geodynamic conditions. This is attested by the morphology, orientation, internal structure, and jointing of the structures. The Oka-Tsna arc formed under the eff