3D resistivity survey for shallow subsurface fault investigations
The shallow subsurface is subject to various human activities, and the place of occurrence of geohazards, e.g. shallow active faults. The identification of the location and orientation of such faults can be vital for infrastructure development. The aim of this study was to develop a low-cost 3D resi...
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2018-01-01
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Online Access: | https://doi.org/10.1051/e3sconf/20183401007 |
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doaj-2bc3a5c1a7f14e58a04f043e3aae858a2021-02-02T03:17:07ZengEDP SciencesE3S Web of Conferences2267-12422018-01-01340100710.1051/e3sconf/20183401007e3sconf_cenviron2018_010073D resistivity survey for shallow subsurface fault investigationsPetrit KraipatKlamthim PoonnapaDuerrast HelmutThe shallow subsurface is subject to various human activities, and the place of occurrence of geohazards, e.g. shallow active faults. The identification of the location and orientation of such faults can be vital for infrastructure development. The aim of this study was to develop a low-cost 3D resistivity survey system, with reasonable survey time for shallow fault investigations. The study area in Songkhla Province, Thailand is located in an old quarry where faults could be identified in outcrops. The study area was designed to cover the expected fault with 100 electrodes arranged in a 10×10 square grid with an electrode spacing of 3 meters in x and y axis. Each electrode in turn was used as a current and potential electrode using a dipole-dipole array. Field data have been processed and interpreted using 3DResINV. Results, presented in horizontal depth slices and vertical xz- and yz-cross sections, revealed through differences in resistivity down to 8 m depths a complex structural setting with two shallow faults and dipping sedimentary rock layers. In conclusion, this study has shown that a 3D resistivity survey can imagine complex tectonic structures, thus providing a far more insight into the shallow subsurface.https://doi.org/10.1051/e3sconf/20183401007 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Petrit Kraipat Klamthim Poonnapa Duerrast Helmut |
spellingShingle |
Petrit Kraipat Klamthim Poonnapa Duerrast Helmut 3D resistivity survey for shallow subsurface fault investigations E3S Web of Conferences |
author_facet |
Petrit Kraipat Klamthim Poonnapa Duerrast Helmut |
author_sort |
Petrit Kraipat |
title |
3D resistivity survey for shallow subsurface fault investigations |
title_short |
3D resistivity survey for shallow subsurface fault investigations |
title_full |
3D resistivity survey for shallow subsurface fault investigations |
title_fullStr |
3D resistivity survey for shallow subsurface fault investigations |
title_full_unstemmed |
3D resistivity survey for shallow subsurface fault investigations |
title_sort |
3d resistivity survey for shallow subsurface fault investigations |
publisher |
EDP Sciences |
series |
E3S Web of Conferences |
issn |
2267-1242 |
publishDate |
2018-01-01 |
description |
The shallow subsurface is subject to various human activities, and the place of occurrence of geohazards, e.g. shallow active faults. The identification of the location and orientation of such faults can be vital for infrastructure development. The aim of this study was to develop a low-cost 3D resistivity survey system, with reasonable survey time for shallow fault investigations. The study area in Songkhla Province, Thailand is located in an old quarry where faults could be identified in outcrops. The study area was designed to cover the expected fault with 100 electrodes arranged in a 10×10 square grid with an electrode spacing of 3 meters in x and y axis. Each electrode in turn was used as a current and potential electrode using a dipole-dipole array. Field data have been processed and interpreted using 3DResINV. Results, presented in horizontal depth slices and vertical xz- and yz-cross sections, revealed through differences in resistivity down to 8 m depths a complex structural setting with two shallow faults and dipping sedimentary rock layers. In conclusion, this study has shown that a 3D resistivity survey can imagine complex tectonic structures, thus providing a far more insight into the shallow subsurface. |
url |
https://doi.org/10.1051/e3sconf/20183401007 |
work_keys_str_mv |
AT petritkraipat 3dresistivitysurveyforshallowsubsurfacefaultinvestigations AT klamthimpoonnapa 3dresistivitysurveyforshallowsubsurfacefaultinvestigations AT duerrasthelmut 3dresistivitysurveyforshallowsubsurfacefaultinvestigations |
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