2021
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)
BÁBEK, Ondřej, Jiří FAIMON, Milan GERŠL a Ondřej ŠRÁČEKZákladní 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
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
Odkazy
Impakt faktor
Impact factor: 4.418
Organizační jednotka
Přírodovědecká fakulta
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
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 17. 3. 2023 09:13, Mgr. Marie Šípková, DiS.
V originále
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.
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.