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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Main Authors: Petrit Kraipat, Klamthim Poonnapa, Duerrast Helmut
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20183401007
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spelling 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
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AT klamthimpoonnapa 3dresistivitysurveyforshallowsubsurfacefaultinvestigations
AT duerrasthelmut 3dresistivitysurveyforshallowsubsurfacefaultinvestigations
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