BÁBEK, Ondřej, Jiří FAIMON, Milan GERŠL a Ondřej ŠRÁČEK. Can the Hranice Abyss, the Deepest Underwater Cave in the World, Really Reach 1 km Depth? A Comment on the Paper by Klanica et al. (2020). JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE. WASHINGTON: AMER GEOPHYSICAL UNION, 2021, roč. 126, č. 4, s. 1-5. ISSN 2169-9003. Dostupné z: https://dx.doi.org/10.1029/2020JF005916.
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Základní údaje
Originální název Can the Hranice Abyss, the Deepest Underwater Cave in the World, Really Reach 1 km Depth? A Comment on the Paper by Klanica et al. (2020)
Název česky Can the Hranice Abyss, the Deepest Underwater Cave in the World, Really Reach 1 km Depth? A Comment on the Paper by Klanica et al. (2020)
Autoři BÁBEK, Ondřej, Jiří FAIMON, Milan GERŠL a Ondřej ŠRÁČEK.
Vydání JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, WASHINGTON, AMER GEOPHYSICAL UNION, 2021, 2169-9003.
Další údaje
Originální jazyk angličtina
Typ výsledku Článek v odborném periodiku
Obor 10500 1.5. Earth and related environmental sciences
Stát vydavatele Spojené státy
Utajení není předmětem státního či obchodního tajemství
WWW Journal pages
Impakt faktor Impact factor: 4.418
Organizační jednotka Přírodovědecká fakulta
Doi http://dx.doi.org/10.1029/2020JF005916
UT WoS 000645002100024
Klíčová slova česky Article Comment; Hranice Abyss; geophysical data; epigenic/hypogenic origin; hydrogeochemistry
Klíčová slova anglicky Article Comment; Hranice Abyss; geophysical data; epigenic/hypogenic origin; hydrogeochemistry
Štítky RIV ne
Příznaky Mezinárodní význam, Recenzováno
Změnil Změnila: Mgr. Marie Šípková, DiS., učo 437722. Změněno: 17. 3. 2023 09:13.
Anotace
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 (CF) and, hence, could be similar to 1 km deep. However, the CF subsided and the abyss was uplifted due to post mid-Miocene faulting with at least 460 m vertical offset, which makes the depth estimate of Klanica et al. (2020, ) invalid. It remains unclear under which geological circumstances the HA, if formed by epigenic karstification, could be backfilled with water column reaching similar to 400 m of height.
Anotace česky
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 (CF) and, hence, could be similar to 1 km deep. However, the CF subsided and the abyss was uplifted due to post mid-Miocene faulting with at least 460 m vertical offset, which makes the depth estimate of Klanica et al. (2020, ) invalid. It remains unclear under which geological circumstances the HA, if formed by epigenic karstification, could be backfilled with water column reaching similar to 400 m of height.
VytisknoutZobrazeno: 25. 4. 2024 19:21