Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Amashukeli, T. A."'
Autor:
Starostenko, V., Janik, T., Murovskaya, A., Czuba, W., Środa, P., Yegorova, T., Aleksandrowski, P., Verpakhovska, O., Kolomiyets, K., Lysynchuk, D., Amashukeli, T., Burakhovych, T., Wójcik, D., Omelchenko, V., Legostaeva, O., Gryn, D., Chulkov, S.
Publikováno v:
In Tectonophysics 6 December 2024 892
Autor:
Starostenko, V., Janik , T., Czuba , W., Środa, P., Murovskaya, A., Yegorova, T., Verpakhovska, A., Kolomiyets, K., Lysynchuk, D., Wójcik, D., Omelchenko, V., Amashukeli, T., Legostaeva, O., Gryn, D., Chulkov, S.
Publikováno v:
Геофізичний журнал; Том 45 № 1 (2023)
Geofizicheskiy Zhurnal; Vol. 45 No. 1 (2023)
Геофизический журнал; Том 45 № 1 (2023)
Geofizicheskiy Zhurnal; Vol. 45 No. 1 (2023)
Геофизический журнал; Том 45 № 1 (2023)
The wide-angle reflection and refraction (WARR) SHIELD’21 profile carried out in 2021 crosses from SW to NE the main tectonic of Ukraine. The SHIELD’21 targeted the structure of the Earth’s crust and upper mantle of the southwestern margin of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::69bd797bc618874808a390cde2943ca2
https://doi.org/10.24028/gj.v45i1.275126
https://doi.org/10.24028/gj.v45i1.275126
Autor:
Janik, T., Starostenko, V., Aleksandrowski, P., Yegorova, T., Czuba, W., Środa, P., Murovskaya, A., Zajats, K., Kolomiyets, K., Lysynchuk, D., Wójcik, D., Mechie, J., G łuszyński, A., Omelchenko, V., Legostaeva, O., Tolkunov, A., Amashukeli, T., Gryn, D., Chulkov, S.
Publikováno v:
Geofizicheskiy Zhurnal; Том 42, № 3 (2020); 3-15
Геофизический журнал; Том 42, № 3 (2020); 3-15
Геофізичний журнал; Том 42, № 3 (2020); 3-15
Геофизический журнал; Том 42, № 3 (2020); 3-15
Геофізичний журнал; Том 42, № 3 (2020); 3-15
The wide-angle reflection and refraction (WARR) TTZ-South transect carried out in 2018 crosses the SW region of Ukraine and the SE region of Poland. The TTZ-South profile targeted the structure of the Earth’s crust and upper mantle of the Trans-Eur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::f885f7729541e46f01774b3d7e838e47
http://journals.uran.ua/geofizicheskiy/article/view/204698
http://journals.uran.ua/geofizicheskiy/article/view/204698
Publikováno v:
Geofizicheskiy Zhurnal; Том 41, № 6 (2019); 203-212
Геофизический журнал; Том 41, № 6 (2019); 203-212
Геофізичний журнал; Том 41, № 6 (2019); 203-212
Геофизический журнал; Том 41, № 6 (2019); 203-212
Геофізичний журнал; Том 41, № 6 (2019); 203-212
The monitoring hazardous natural processes in order to assess risks to the public and industrial facilities and ensure safety has become the starting point for the creation of appropriate monitoring systems. The development of a modern hardware base
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::c7e105419f6e4887a2e228adf792236d
http://journals.uran.ua/geofizicheskiy/article/view/190077
http://journals.uran.ua/geofizicheskiy/article/view/190077
Publikováno v:
Geofizicheskiy Zhurnal; Том 41, № 2 (2019); 84-98
Геофизический журнал; Том 41, № 2 (2019); 84-98
Геофізичний журнал; Том 41, № 2 (2019); 84-98
Геофизический журнал; Том 41, № 2 (2019); 84-98
Геофізичний журнал; Том 41, № 2 (2019); 84-98
The studies include the materials of the field tectonophysical observations of 2013―2018 and reinterpreted field data of 1990―1995. In order to determine the stress tensor structural-paragenetic and kinematic tectonophysical methods were used. Ap
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::5fcae0f5ff037a5a700b65e021a5cba1
http://journals.uran.ua/geofizicheskiy/article/view/164455
http://journals.uran.ua/geofizicheskiy/article/view/164455
Publikováno v:
Geofizicheskiy Zhurnal; Том 41, № 1 (2019); 153-171
Геофизический журнал; Том 41, № 1 (2019); 153-171
Геофізичний журнал; Том 41, № 1 (2019); 153-171
Геофизический журнал; Том 41, № 1 (2019); 153-171
Геофізичний журнал; Том 41, № 1 (2019); 153-171
The tectonic structure of Dobrogea and Fore-Dobrogea trough are considered on the basis of geological and geophysical data. Dobrogea and Fore-Dobrogea trough are the key areas for understanding of Central Europe geodynamics, because they are located
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::696653f8f5510eb9ef07f78ba11f60e1
http://journals.uran.ua/geofizicheskiy/article/view/158869
http://journals.uran.ua/geofizicheskiy/article/view/158869