Aspects of equivalence in two-dimensional resistivity imaging and modelling

dc.contributor.authorOlayinka, A.I.
dc.date.accessioned2021-08-06T11:15:20Z
dc.date.available2021-08-06T11:15:20Z
dc.date.issued2000
dc.description.abstractThe 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.en_US
dc.identifier.issn1116-2775
dc.identifier.otherui_art_olayinka.a.i_aspects_2000
dc.identifier.otherJournal of Mining and Geology 36(1) 2000, Pp. 67 - 76
dc.identifier.urihttp://ir.library.ui.edu.ng/handle/123456789/5429
dc.language.isoen_USen_US
dc.publisherNigerian Mining and Geosciences Societyen_US
dc.titleAspects of equivalence in two-dimensional resistivity imaging and modellingen_US
dc.typeArticleen_US

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