dc.contributor.author |
Van Schoor, Michael
|
en_US |
dc.date.accessioned |
2007-02-06T08:37:19Z |
en_US |
dc.date.accessioned |
2007-06-07T10:02:43Z |
|
dc.date.available |
2007-02-06T08:37:19Z |
en_US |
dc.date.available |
2007-06-07T10:02:43Z |
|
dc.date.copyright |
|
en_US |
dc.date.issued |
2002-07 |
en_US |
dc.identifier.citation |
Van Schoor, M. 2002. Detection of sinkholes using 2D electrical resistivity imaging. Journal of applied geophysics, vol 50(4), pp 393-399 |
en_US |
dc.identifier.issn |
0926-9851 |
en_US |
dc.identifier.uri |
http://hdl.handle.net/10204/1474
|
en_US |
dc.identifier.uri |
http://hdl.handle.net/10204/1474
|
|
dc.description.abstract |
Sinkholes in dolomitic areas are notoriously difficult geophysical targets, and selecting an appropriate geophysical solution is not straightforward. Electrical resistivity imaging or tomography (RESTOM) is well suited to mapping sinkholes because of the ability of the technique for detecting resistive features and discriminating subtle resistivity variations. RESTOM surveys were conducted at two sinkhole sites near Pretoria, South Africa. The survey areas are located in the dolomites of the Lyttelton Formation, which forms part of the Malamani Subgroup and Chuniespoort Group of the Transvaal Super group. The survey results suggest that RESTOM is an ideal geophysical tool to aid in the detection and monitoring of sinkholes and other subsurface cavities. |
en_US |
dc.format.extent |
327791 bytes |
en_US |
dc.format.mimetype |
application/pdf |
en_US |
dc.language.iso |
en |
en_US |
dc.publisher |
Elsevier Science BV |
en_US |
dc.rights |
Copyright: 2002 Elsevier Science Ltd |
en_US |
dc.source |
|
en_US |
dc.subject |
Cavities |
en_US |
dc.subject |
Dolomite |
en_US |
dc.subject |
Sinkholes |
en_US |
dc.subject |
RESTOM |
en_US |
dc.subject |
Geoelectric imaging |
en_US |
dc.subject |
Resistivity tomographies |
en_US |
dc.title |
Detection of sinkholes using 2D electrical resistivity imaging |
en_US |
dc.type |
Article |
en_US |
dc.identifier.apacitation |
Van Schoor, A. M. (2002). Detection of sinkholes using 2D electrical resistivity imaging. http://hdl.handle.net/10204/1474 |
en_ZA |
dc.identifier.chicagocitation |
Van Schoor, Abraham M "Detection of sinkholes using 2D electrical resistivity imaging." (2002) http://hdl.handle.net/10204/1474 |
en_ZA |
dc.identifier.vancouvercitation |
Van Schoor AM. Detection of sinkholes using 2D electrical resistivity imaging. 2002; http://hdl.handle.net/10204/1474. |
en_ZA |
dc.identifier.ris |
TY - Article
AU - Van Schoor, Abraham M
AB - Sinkholes in dolomitic areas are notoriously difficult geophysical targets, and selecting an appropriate geophysical solution is not straightforward. Electrical resistivity imaging or tomography (RESTOM) is well suited to mapping sinkholes because of the ability of the technique for detecting resistive features and discriminating subtle resistivity variations. RESTOM surveys were conducted at two sinkhole sites near Pretoria, South Africa. The survey areas are located in the dolomites of the Lyttelton Formation, which forms part of the Malamani Subgroup and Chuniespoort Group of the Transvaal Super group. The survey results suggest that RESTOM is an ideal geophysical tool to aid in the detection and monitoring of sinkholes and other subsurface cavities.
DA - 2002-07
DB - ResearchSpace
DP - CSIR
KW - Cavities
KW - Dolomite
KW - Sinkholes
KW - RESTOM
KW - Geoelectric imaging
KW - Resistivity tomographies
LK - https://researchspace.csir.co.za
PY - 2002
SM - 0926-9851
T1 - Detection of sinkholes using 2D electrical resistivity imaging
TI - Detection of sinkholes using 2D electrical resistivity imaging
UR - http://hdl.handle.net/10204/1474
ER - |
en_ZA |