Geophysical investigation across the Peel boundary fault (The Netherlands) for a paleoseismological study
Abstract In preparation of the first paleoseismic trenching in the NE border of the Roer graben (the Netherlands), site selection was carried out. Combining geological and seismological information and using existing aerial photographs, seismic reflection and geodetic levelling data, it was decided to focus on the Peel boundary fault near the village of Neer. Detailed information on the exact location of the fault was obtained through geophysical techniques, mainly ground penetrating radar (GPR) and resistivity measurements. GPR data unambiguously showed the flexuring and offset of reflectors... Mehr ...
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Dokumenttyp: | Artikel |
Erscheinungsdatum: | 2001 |
Reihe/Periodikum: | Netherlands Journal of Geosciences ; volume 80, issue 3-4, page 119-127 ; ISSN 0016-7746 1573-9708 |
Verlag/Hrsg.: |
Cambridge University Press (CUP)
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Sprache: | Englisch |
Permalink: | https://search.fid-benelux.de/Record/base-27627154 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | http://dx.doi.org/10.1017/s0016774600023787 |
Abstract In preparation of the first paleoseismic trenching in the NE border of the Roer graben (the Netherlands), site selection was carried out. Combining geological and seismological information and using existing aerial photographs, seismic reflection and geodetic levelling data, it was decided to focus on the Peel boundary fault near the village of Neer. Detailed information on the exact location of the fault was obtained through geophysical techniques, mainly ground penetrating radar (GPR) and resistivity measurements. GPR data unambiguously showed the flexuring and offset of reflectors affected by the fault. Performing eleven GPR profiles along strike allowed to obtain a 3D picture of the fault, laterally extending the information given in the trench.