Zobrazeno 1 - 10
of 178
pro vyhledávání: '"A. N. Terekhov"'
Autor:
E. N. Terekhov, N. B. Kuznetsov, T. V. Romanyuk, M. A. Matveev, A. B. Makeev, A. S. Novikova, M. Yu. Gushchina, A. S. Dubenskiy, V. S. Sheshukov, A. A. Iurmanov
Publikováno v:
Геодинамика и тектонофизика, Vol 15, Iss 4 (2024)
The paper presents the results of U-Pb isotope dating of zircons extracted from rocks of the southern part of the Baltic Shield (Early Riphean conglomerates and Paleoproterozoic secondary quartzites) and makes a comparison of these results with the a
Externí odkaz:
https://doaj.org/article/3de724217cd44598bb98e9bfd2c093aa
Autor:
N. B. Kuznetsov, S. Yu. Kolodyazhnyi, T. V. Romanyuk, A. V. Strashko, A. S. Baluev, E. N. Terekhov, S. V. Mezhelovskaya, A. S. Dubensky, V. S. Sheshukov
Publikováno v:
Геодинамика и тектонофизика, Vol 14, Iss 1 (2023)
The first results of U-Pb isotope dating of detrital zircons (dZr) from red-colored quartzitic-sandstones of the Shoksha formation (Shoksha horizon) are presented. The Shoksha formation completes the Vepsian sub-horizon (Vepsian) of the Lower Protero
Externí odkaz:
https://doaj.org/article/474b985cc91b436cbe478a6c969107c6
Autor:
N. B. Kuznetsov, A. S. Baluev, E. N. Terekhov, S. Yu. Kolodyazhnyi, E. S. Przhiyalgovskii, T. V. Romanyuk, A. S. Dubensky, V. S. Sheshukov, S. M. Lyapunov, T. B. Bayanova, P. A. Serov
Publikováno v:
Геодинамика и тектонофизика, Vol 12, Iss 3, Pp 570-607 (2021)
Initially, the age and stratigraphic position of the Tersk formation were determined with respect to the fact that this formation overlaps the Early Proterozoic granitoids. Its top was marked by the rocks penetrated by the Late Devonian alkaline intr
Externí odkaz:
https://doaj.org/article/b4f0c15493b545728e5f64b49d6e8135
Autor:
Bahdan V. Ranishenka, Andrei Yu. Panarin, Irina A. Chelnokova, Sergei N. Terekhov, Peter Mojzes, Vadim V. Shmanai
Publikováno v:
Beilstein Journal of Nanotechnology, Vol 12, Iss 1, Pp 902-912 (2021)
This work studies the impact of the electrostatic interaction between analyte molecules and silver nanoparticles (Ag NPs) on the intensity of surface-enhanced Raman scattering (SERS). For this, we fabricated nanostructured plasmonic films by immobili
Externí odkaz:
https://doaj.org/article/087970ab5ada46f49773cac8c2cabef6
Publikováno v:
Геодинамика и тектонофизика, Vol 13, Iss 3 (2022)
Detailed studies of the deeply metamorphosed Early Precambrian rocks of the Northern Ladoga region allowed us to distinguish three deformation stages of the Svecofennian tectogenesis during which there occurred significant structural and compositiona
Externí odkaz:
https://doaj.org/article/06feba377aa04b4aa98b229bf15b040d
Autor:
Evgenii N. Terekhov, Aleksandr B. Makeev, Aleksandr S. Baluev, Aleksandr N. Konilov, Konstantin V. Van
Publikováno v:
Записки Горного института, Vol 248, Pp 232-242 (2021)
Complex mineralogical, geochemical, and geological-structural characteristics of a rare collection stone of violet color, phyolithite, in the southwestern part of the Kola Peninsula. This is a metasomatic rock formed under the conditions of brittle d
Externí odkaz:
https://doaj.org/article/b2878f8c7dbe4cf98122a9ef126f6089
Publikováno v:
LITHOSPHERE (Russia). 23:247-269
Research subject. The chemical composition and spectroscopic properties of almandine jewelry garnets from the Kite-lya deposit in the Northern Ladoga region (Karelia). Materials and methods. The chemical composition, impurity elements, mineral inclus
Publikováno v:
Doklady Earth Sciences. 509:118-132
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 5, Pp 5-11 (2018)
Kandalaksha graben, located in the water-area of the White sea, is a part of the Onega-Kandalaksha paleorift of the Riphean time of foundation. It is filled with the terrigenous formations of the Terskaya suites ranging from 3 to 8 km by depth, while
Externí odkaz:
https://doaj.org/article/b3affdd59eee4fb4bf1739559fb9d8f8
Publikováno v:
WSEAS TRANSACTIONS ON SYSTEMS AND CONTROL. 17:527-534
In this paper, we have developed a new approach to the local improvement of an approximate solution which has been obtained with the finite element method. The proposed improvement is adaptive, and it minimizes the energy functional. The discussed al