Imaging the Marianske Lazne Fault (Czech Republic) by 3-D ground-penetrating radar and electric resistivity tomography

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F12%3A10132235" target="_blank" >RIV/00216208:11310/12:10132235 - isvavai.cz</a>
Alternative codes found
RIV/67985530:_____/12:00381710 RIV/67985891:_____/12:00381710
Result on the web
<a href="http://dx.doi.org/10.1007/s11200-012-0825-z" target="_blank" >http://dx.doi.org/10.1007/s11200-012-0825-z</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s11200-012-0825-z" target="_blank" >10.1007/s11200-012-0825-z</a>

Result language
angličtina
Original language name
Imaging the Marianske Lazne Fault (Czech Republic) by 3-D ground-penetrating radar and electric resistivity tomography
Original language description
Geodynamic activity in the area of West Bohemia is typified by the occurrence of earthquake swarms, Quaternary volcanism and high flux of mantle-derived CO2. The highest swarm activity occurs beneath the eastern edge of the Cheb basin, which is delineated by the NW-SE trending morphologically pronounced Marianske Lazne. Fault (WE) controlling the formation of the basin. The previous trenching survey across the MLF zone has identified several fault strands with possible Quaternary activity. In this paperwe present the results of the geophysical survey focused to trace the faults signatures in geophysical sections and to build an image of near surface tectonics. The method of electric resistivity tomography (ERT) along two profiles parallel to the trench identified a strong resistivity contrast between the bodies of sandy gravels in the middle and conductive clayey sands to the west and weathered crystalline basement to the east. The 2-D ground penetration radar (GPR) sections show dire
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DC - Seismology, volcanology and Earth structure
OECD FORD branch
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Project
<a href="/en/project/IAA300120905" target="_blank" >IAA300120905: Dynamics of crustal fluids in the western part of the Bohemian Massif as a probe of the stress changes</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)

Publication year
2012
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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