Fissure caves and other gravitationally-induced discontinuities detected by 2D electrical resistivity tomography. Case studies from Flysch Carpathians

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F10%3AA1100ZWV" target="_blank" >RIV/61988987:17310/10:A1100ZWV - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Fissure caves and other gravitationally-induced discontinuities detected by 2D electrical resistivity tomography. Case studies from Flysch Carpathians

Popis výsledku v původním jazyce

Fissure caves as well as other subsurface dislocations can represent initial forms of the gravi-tational disintegration of rock massif ranging from shallow to deep-seated (>40 m) gravitational slope deformations. Presence of pseudokarst forms, such as crevice-type caves, trenches, escarpments, tension cracks or sinkhole-type depressions is frequent in the massifs of the Outer Western Carpathians which are formed by anisotropic flysch rock. Detailed research of these landforms can significantly contribute to understanding to the processes transforming a relief of the medium-high mountains in the Carpathian flysch belt. Method of electrical resistivity tomography (ERT) based on various resistivity values of particular subsurface structures offers a non-invasive way to display the situation beneath the surface.

Název v anglickém jazyce

Fissure caves and other gravitationally-induced discontinuities detected by 2D electrical resistivity tomography. Case studies from Flysch Carpathians

Popis výsledku anglicky

Fissure caves as well as other subsurface dislocations can represent initial forms of the gravi-tational disintegration of rock massif ranging from shallow to deep-seated (>40 m) gravitational slope deformations. Presence of pseudokarst forms, such as crevice-type caves, trenches, escarpments, tension cracks or sinkhole-type depressions is frequent in the massifs of the Outer Western Carpathians which are formed by anisotropic flysch rock. Detailed research of these landforms can significantly contribute to understanding to the processes transforming a relief of the medium-high mountains in the Carpathian flysch belt. Method of electrical resistivity tomography (ERT) based on various resistivity values of particular subsurface structures offers a non-invasive way to display the situation beneath the surface.

Druh

D - Stať ve sborníku

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2010

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název statě ve sborníku

Geomorfologický sborník 9

ISBN

978-80-86561-32-5

ISSN

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e-ISSN

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Počet stran výsledku

2

Strana od-do

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Název nakladatele

Univerzita Karlova

Místo vydání

Praha

Místo konání akce

Branná

Datum konání akce

11. 5. 2010

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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