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The possibility for geoelectrical equivalence in two-dimensional (2-D) inversion of apparent resistivity data has been investigated. This involved the calculation of synthetic pscudosection data for simple geological structures using a finite difference approach. With the aid of statistical F-test,...
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| Published: |
2000
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| LEADER | 00000njm a2000000a 4500 | ||
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| 001 | oai:repository.ui.edu.ng:123456789/5429 | ||
| 042 | |a dc | ||
| 720 | |a Olayinka, A.I. |e author | ||
| 260 | |c 2000 | ||
| 520 | |a The possibility for geoelectrical equivalence in two-dimensional (2-D) inversion of apparent resistivity data has been investigated. This involved the calculation of synthetic pscudosection data for simple geological structures using a finite difference approach. With the aid of statistical F-test, it is shown that identical or near-identical pseudosections can be generated from more than one 2-D model. In particular, the apparent resistivity pscudosection measured over2-D structures like basement fault, trough and horst resemble those arising from lateral variations In the overburden resistivity. | ||
| 024 | 8 | |a 1116-2775 | |
| 024 | 8 | |a ui_art_olayinka.a.i_aspects_2000 | |
| 024 | 8 | |a Journal of Mining and Geology 36(1) 2000, Pp. 67 - 76 | |
| 024 | 8 | |a http://ir.library.ui.edu.ng/handle/123456789/5429 | |
| 245 | 0 | 0 | |a Aspects of equivalence in two-dimensional resistivity imaging and modelling |