Zobrazeno 1 - 10
of 29
pro vyhledávání: '"A. Verpakhovska"'
Autor:
V. Starostenko, T. Janik, W. Czuba, P. Środa, A. Murovskaya, T. Yegorova, A. Verpakhovska, K. Kolomiyets, D. Lysynchuk, D. Wójcik, V. Omelchenko, T. Amashukeli, O. Legostaeva, D. Gryn, S. Chulkov
Publikováno v:
Геофизический журнал, Vol 45, Iss 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://doaj.org/article/71a049c250ab42c39f65640883e14469
Publikováno v:
Geofizicheskiy Zhurnal. 44:3-12
For many years, the Institute of geophysics has been developing original versions of the finite-difference migration and wavefield modeling techniques for a valid reproduction of the geological cross-section. The modeling provides a practical test of
Autor:
Tomasz Janik, Vitaly Starostenko, Wojciech Czuba, Piotr Środa, Anna Murovskaya, Tamara Yegorova, Alexandra Verpakhovska, Katerina Kolomiyets, Dmytro Lysynchuk, Dariusz Wójcik, Victor Omelchenko, Tanya Amashukeli, Olga Legostaeva, Dmytro Gryn, Serhii Chulkov
Carried out in 2021, the wide-angle reflection and refraction (WARR) SHIELD’21 profile crosses, from SW to NE, the main tectonic structures of Ukraine. It targeted the structure of the Earth’s crust and upper mantle of the southwestern margin of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::17fb82f0d9b0500bf1ecd25bbfcba934
https://doi.org/10.5194/egusphere-egu23-2387
https://doi.org/10.5194/egusphere-egu23-2387
Publikováno v:
Геофізичний журнал; Том 45 № 2 (2023)
Geofizicheskiy Zhurnal; Vol. 45 No. 2 (2023)
Геофизический журнал; Том 45 № 2 (2023)
Geofizicheskiy Zhurnal; Vol. 45 No. 2 (2023)
Геофизический журнал; Том 45 № 2 (2023)
Transcarpathian depression (TD) is located in the junction zone of the eastern margin of ALCAPA terrain and the northern part of Tisza-Dacia one, buried under thick Neogene molasses. The Earth’s crust structure of the TD is not clearly understood.
Publikováno v:
Geofizicheskiy Zhurnal. 44:152-169
The method of finite-difference migration of reflected/refracted waves, applied to the PANCAKE and RomUkrSeis WARR seismic profiles, made it possible to form wave images of sedimentary layer and crystalline basement under the Carpathian orogen to a d
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
Publikováno v:
Geology and Mineral Resources of World Ocean. 18:27-39
In current seismic studies, special attention is given to the correctness of both the processing methods and the results of their using. In particularly, this applies to the migration procedure, which allows reproducing the deep structure of the rese
Autor:
O. O. Verpakhovska
Publikováno v:
Geofizicheskiy Zhurnal. 43:127-149
The method of deep seismic sounding (DSS), the observation systems in which are characterized by an irregular arrangement of both sources and receivers along the profile, a significant step between receivers, as well as maximum source-receiver distan
Publikováno v:
Geofizicheskiy Zhurnal. 43:14-27
In present-day seismic exploration the quality of the observed wave field that guarantees obtaining the most exact and complete information on the structure of the studied area plays an important role. Therefore much attention is paid to elaboration
Publikováno v:
Journal of Geodynamics. 121:76-87
The Outer Ukrainian Carpathians (OUC) are a part of the Eastern Carpathians, which is a segment of the European Alpine Belt. The OUC is crossed by recently acquired WARR PANCAKE profile that passes from the Pannonian Basin on the SW to the East Europ