Download Citation on ResearchGate | Modified Pseudo-Section for Resistivity and IP | Dipole–dipole induced-polarization measurements are commonly. A modified pseudosection for resistivity and IP Edwards L.S.. Geophysics 42(5): Dipole-dipole induced-polarization measurements are. In a dc resistivity or induced polarization (IP) survey we are generally Edwards, L. S., , A modified pseudosection for resistivity and IP: Geophysics,

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modified pseudosection for resistivity and IP | Geophysics | GeoScienceWorld

The modified pseudo-depth section as a tool in resistivity and IP prospecting; a case history. Email alerts New issue content alert. Comparing semiquantitative logic trees for archaeoseismology and paleoseismology: On measuring the electrical conductivity of the oceanic crust by a modified magnetometric resistivity MMR method. Theoretical evaluation of modified Wenner array for shallow resistivity exploration. Previous Article Next Article.

Close mobile search navigation Article navigation. The empirical coefficients are compared with Roy’s theory of ‘depth of investigation pseudoswction and support that theory, if a modified definition of ‘effective depth’ is accepted.

Citing articles via Web Of Science From Tectonics to Groundwater. Probing the resistivity of the sea floor by a modified magnetometric resistivity MMR method. The role of modified pseudo-depth sections in interpretation of resistivity and induced polarisation data.

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Processes on the Early Earth. Other August 01, Window to Mesoproterozoic Earth. It is shown, by examples, that the resulting pseudosections give consistent estimates of depth to top, within the characteristic anomaly patterns of each array.

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Seepage-induced anomalies, “false” anomalies, and implications for electrical prospecting AAPG Bulletin.

A modified pseudosection for resistivity and IP

Study on resistivity of crystalline and sedimentary samples; the influence of pore fluid resistivity and bulk surface conduction on rock resistivity. The effective depths for various arrays are compared; the results agree with the traditional applications of each array.

Petrographic and resiativity investigations for a district-scale ground-coupled heat pump—Ball State University, Indiana Geothermal Energy: Abstract Dipole-dipole induced-polarization measurements are commonly presented as pseudosections, but results using different dipole lengths cannot be combined into a single pseudosection. An evaluation of Bristow’s method for the detection of subsurface cavities Geophysics.

Edwards; A modified pseudosection for resistivity and IP.

Continuous resistivity measurement using the m borehole at the Nojima Fault in Awaji Island, Japan; resistivity change evaluation using 3D DC-resistivity modeling.

Topographic effects in resistivity and induced-polarization surveys Geophysics. Improvement to resistivity pseudosection modelling by removal of near-surface inhomogeneity effects; application to a soil system in South Cameroon. By continuing to use our website, you are agreeing to our privacy policy. Sign In or Resiistivity an Account.

This leads to an absolute depth scale for the modified pseudosection.

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A modified pseudosection for resistivity and IP. You could not be signed in. You do not currently have access to this article.

Resistivity measurement for granite and tuff samples; influence of pore fluid resistivity on rock resistivity. Effect of well casings on surface electrical surveys Geophysics. Sulfidic early basin strata as key markers of Cordilleran shortening and Eocene extension Belt Basin: Pure and Applied Geophysics 1: This site uses cookies.

Mineral discrimination and removal of inductive coupling with multifrequency IP; discussion and reply Geophysics.

Geophysics ; 42 5: Geophysics 42 5: Volume 42, Number 5. Application of these coefficients to a number of theoretical and field cases shows that they give reasonable results when applied to more complicated models.

Highly conductive horizons in the Mesoproterozoic Belt-Purcell Basin: Librarian Administrator Sign In. It is shown that rough estimates of the depth to the top of an anomalous body can be made directly on the pseudosection, at true vertical scale.

American Geophysical Union Fall Meeting, Geophysical Prospecting 47 2: