Zobrazeno 1 - 10
of 33
pro vyhledávání: '"Vladimír BEZÁK"'
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 53, Iss 4, Pp 413-424 (2023)
In Slovakia, we singled out thirty areas in which flash floods occurred repeatedly. The aim of our analysis was to assess the influence of geological and geomorphological factors on the occurrence of such floods. Two areas were selected as an example
Externí odkaz:
https://doaj.org/article/6e607aa36fa4472ab5641f75dc4e9958
Autor:
Vladimír BEZÁK, Dušan MAJCIN
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 48, Iss 4, Pp 349-363 (2018)
Our contribution presents the geological analysis results of the lithological composition for deep geothermal sources characterized by the thermal conditions suitable for application of classic hydrothermal sources exploitation and specialized EGS te
Externí odkaz:
https://doaj.org/article/c6f7eeafdbbc4c6fa30b3dca6ee861da
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 50, Iss 4, Pp 463‒474-463‒474 (2020)
2D integrated modelling approach was applied to determine the lithospheric structure along transect HT-1 located in the Carpathian-Pannonian Basin–European platform region. Our approach combines simultaneous interpretation of surface heat flow, top
Externí odkaz:
https://doaj.org/article/198e964d80294069891729a7c161316e
Extensometric observation of Earth tides and local tectonic processes at the Vyhne station, Slovakia
Autor:
Ladislav BRIMICH, Martin BEDNÁRIK, Vladimír BEZÁK, Igor KOHÚT, Dóra BÁN, Ildikó EPER-PÁPAI, Gyula MENTES
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 46, Iss 2, Pp 75-90 (2016)
The Vyhne Tidal Station of the Earth Science Institute of the Slovak Academy of Sciences is located in the former mining gallery of St. Anthony of Padua in the Vyhne valley, Štiavnick´e vrchy Mts., Central Slovakia. It is equipped with a 20.5 metre
Externí odkaz:
https://doaj.org/article/b4a5fc5b2e5a4846938dbc519100aa04
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 46, Iss 1, Pp 33-49 (2016)
The contribution presents the results acquired both by direct cognitive geothermic methods and by modelling approaches of the lithosphere thermal state in the region of the Transcarpathian depression and surrounding units. The activities were aimed a
Externí odkaz:
https://doaj.org/article/6a70ced1a1ec462897b215b5c5114cf9
Autor:
Vladimír BEZÁK, Josef PEK, Dušan MAJCIN, Jana BUČOVÁ, Tomáš ŠOLTIS, Dušan BILČÍK, Radek KLANICA
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 45, Iss 1, Pp 1-11 (2015)
In this paper we present a geological interpretation of magnetotelluric sounding along the southern part of the seismic 2T profile situated in the southern Central Slovakia. The complexes with higher conductivity are imaged in the shallow depths, for
Externí odkaz:
https://doaj.org/article/8d0738ec0e3947478e1df44d79777ec4
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 44, Iss 4, Pp 271-292 (2014)
The locality of the northeastern most part of Slovakian Flysch belt belongs to interesting areas in terms of the interpretation of geothermal conditions in mutual relation with the lithosphere structure and their tectonic development. The evaluation
Externí odkaz:
https://doaj.org/article/2db055d1ba4e4d9db359980b4d421548
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 42, Iss 4, Pp 283-294 (2012)
A positive gravity anomaly was observed in the Flysch belt realm. Based on this fact and available geological knowledge we suppose that the source of gravity anomaly might be carbonate rocks lying perhaps in the footwall of Flysch sediments. The carb
Externí odkaz:
https://doaj.org/article/9e1c01b410f14b029e533360bc85173c
Publikováno v:
Contributions to Geophysics and Geodesy, Vol 41, Iss 4, Pp 297-306 (2011)
Magnetotelluric measurements (MT) in the southeast (SE) part of MT–15 profile in the frame of CELEBRATION 2000 project identified a subhorizontal zone with higher conductivity in the depth of cca 2–6 km below the Tribeč Mts. surface. This zone i
Externí odkaz:
https://doaj.org/article/7cd21085c4e743e9a50176900c716a54
During the last 21 Ma, widespread and geo-chemically variable volcanism took place in the Pannonian Basin and surrounding areas. The Nógrád-Gömör Volcanic Field (NGVF) is the northernmost Neogene monogenetic alkali basalt volcanic field of the Ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0897664583bbb0a16d2344623acad37a
https://doi.org/10.5194/egusphere-egu23-11855
https://doi.org/10.5194/egusphere-egu23-11855