To characterize fractured rocks which is principal in
hydrological studies, requires knowledge of the orientation of fractures and
for this aim there is not too many geophysical tools. For the geophysical
determination of the prevailing orientations, so-called azimuthal geoelectric
measurements seemed to be a feasible method until their disadvantages (in many
cases wrong fracture orientations) were revealed.
Author(s) Details:
Szalai S.,
Institute of Earth Physics and Space Science (ELKH-EPSS), Sopron,
Hungary and Department of Geophysics, University of Miskolc,
Miskolc-Egyetemváros, Hungary.
Kósa
I.,
Institute
of Earth Physics and Space Science (ELKH-EPSS), Sopron, Hungary.
Gribovszki Z.,
University of West Hungary, Geomatikai, Erdofeltarasi es
Vizgazdalkodasi Intezet, Hungary.
Nagy T.,
Institute of Earth Physics and Space Science (ELKH-EPSS), Sopron,
Hungary.
Baracza M. K.,
Research
Institute of Applied Earth Sciences (RIAES), University of Miskolc,
Miskolc-Egyetemváros, Hungary.
Szarka
L.,
Institute
of Earth Physics and Space Science (ELKH-EPSS), Sopron, Hungary.
Szucs P.,
University of Miskolc, Institute of Environmental Management,
Hungary and MTA-ME Geoengineering Research Group, Miskolc-Egyetemváros,
Hungary.
Lemperger I.,
Institute of Earth Physics and Space Science (ELKH-EPSS), Sopron,
Hungary.
Gribovszki K.,
Institute of Earth Physics and Space Science (ELKH-EPSS), Sopron, Hungary.
Please see the link here: https://stm.bookpi.org/CPPSR-V5/article/view/13037
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