Geophysical evidence of the Mariánské Lázně Fault (Cheb Basin, Czech Republic)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F16%3A10332704" target="_blank" >RIV/00216208:11310/16:10332704 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Geophysical evidence of the Mariánské Lázně Fault (Cheb Basin, Czech Republic)
Original language description
A subsurface manifestation of the Mariánské Lázně Fault was investigated by means of combined geophysical surveying and integrated interpretations of measured data sets. The integrated results of the electrical resistivity tomography, shallow refraction seismics and gravity survey indicate a wide steeply inclined fault zone, likely formed of intensively disrupted and weathered crystalline rocks, and delimiting the sedimentary infill of the Cheb basin from the crystalline rocks of the Krušné hory Mts. Importance of employing more than a single geophysical technique and subsequent integrated interpretation of the various geophysical data sets was confirmed.
Czech name
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Czech description
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Classification
Type
O - Miscellaneous
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2016
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů