J 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 ŠRÁČEK

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

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.

Anotace

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.