Zobrazeno 1 - 10
of 73
pro vyhledávání: '"Ondřej Bábek"'
Publikováno v:
Heliyon, Vol 10, Iss 3, Pp e25262- (2024)
Understanding the spatial variation in lithology is crucial for characterizing reservoirs, as it governs the distribution of petrophysical characteristics. This study focuses on predicting the lithology of carbonate rocks (limestone, argillaceous lim
Externí odkaz:
https://doaj.org/article/7066e2d57f6c452cad56ebefbedf3359
Publikováno v:
Hydrological Sciences Journal. 68:685-699
Publikováno v:
Sedimentology.
Autor:
Tomáš Kumpan, Markéta Holá, Ondřej Bábek, Stanislava Vodrážková, Jiří Kalvoda, Lukáš Ackerman
Publikováno v:
Sedimentology. 68:3523-3548
Publikováno v:
Theoretical and Applied Climatology. 142:85-101
Microclimatic processes were studied in the soil of the well-defined “breathing spot” named Půlhodina (BSP) in the Hranice Karst (Czech Republic). The results have indicated that air is exchanged between the external atmosphere and a supposed un
Autor:
Balázs Komoróczy, Zuzana Lenďáková, Marek Vlach, Ondřej Bábek, Claus-Michael Hüssen, Ján Rajtár
Publikováno v:
Geoarchaeology. 35:729-747
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 101:473-485
The continuous and well-accessible Devonian-Carboniferous boundary successions of the Czech Republic are part of the Brunovistulian Unit, which belongs to the Variscan Rhenohercynian Zone of the Bohemian Massif. The well-studied sections, with almost
Publikováno v:
Sedimentary Geology. 440:106262
Publikováno v:
Journal of Geophysical Research: Earth Surface. 126
Based on shallow geophysical data, Klanica et al. (2020, ) argued that the deepest undewater cave in the world, the Hranice Abyss (HA) had formed by epigenic karstification related to mid-Miocene opening of similar to 1 km deep Carpathian Foredeep (C
Publikováno v:
Geomorphology. 333:16-29
Oxbow lakes represent important geomorphic and depositional units of meandering river systems, whose rates of sediment accumulation may significantly exceed those of surrounding floodplains. Natural and artificial oxbow lakes may differ considerably,