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

Result code in 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>
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Fissure caves and other gravitationally-induced discontinuities detected by 2D electrical resistivity tomography. Case studies from Flysch Carpathians
Original language description
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.
Czech name
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Czech description
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Publication year
2010
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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