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Please use this identifier to cite or link to this item: http://paper.sci.ui.ac.id/jspui/handle/2808.28/238
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dc.contributor.authorMardiyati, Sri-
dc.date.accessioned2016-10-18T03:13:18Z-
dc.date.available2016-10-18T03:13:18Z-
dc.date.issued2016-09-30-
dc.identifier.issn20928637-
dc.identifier.urihttp://paper.sci.ui.ac.id/jspui/handle/2808.28/238-
dc.description.abstractThe electrical potential measurement on the ground surface using Schlumberger configuration can be used to estimate the conductivity model of the earth. The Conductivity in transversely isotopic earth is a conductivity type which has the same value in all horizontal directions but have different value in vertical current flow. This conductivity type is discussed in this research and the liniarized inverse theory of Backus and Gilbert is used to create an iterative method for constructing a conductivity model whose calculated potential response are in agreement with the observations.en_US
dc.language.isoen_USen_US
dc.publisherAdvanced Institute of Convergence Information Technology Research Centeren_US
dc.relation.ispartofseriesVolume 7;Number 3-
dc.sourceJournal of Next Generation Information Technology, Volume 7 Number 3, Pp. 61-69 (30 September 2016)en_US
dc.subjectConductivityen_US
dc.subjectSchlumberger configurationen_US
dc.subjecttransversely isotopicen_US
dc.titleConductivity Model Construction for a Transversely Isoropic Earthen_US
dc.typeArticleen_US
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