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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A modified pseudosection for resistivity and IP
Sulfidic early basin strata as key markers of Cordilleran shortening and Eocene extension Belt Basin: Study on resistivity of crystalline and sedimentary samples; the influence of pore fluid resistivity and pswudosection surface conduction on rock resistivity.
Geophysical Research Bulletin 20 3: Abstract Dipole-dipole induced-polarization measurements are commonly presented as pseudosections, but results using different dipole lengths cannot be combined into a single pseudosection.
American Geophysical Union Fall Meeting, Pure and Applied Geophysics 1: Resistivity measurement for granite and tuff samples; influence of pore fluid resistivity on rock resistivity. Probing the resistivity of the sea floor by a modified magnetometric resistivity MMR method.
Window to Mesoproterozoic Earth.
modified pseudosection for resistivity and IP | Geophysics | GeoScienceWorld
Electrical resistivity imaging of hydrologic changes in an anthropogenically modified arid environment. Geophysics 42 5: Improvement to resistivity pseudosection modelling by removal of near-surface inhomogeneity effects; application to a soil system in South Cameroon. The effective depths for various arrays are compared; the results agree with the traditional applications of each array.
Other August 01, Petrographic and hydrogeologic investigations for a district-scale ground-coupled heat pump—Ball State University, Indiana Geothermal Energy: Librarian Administrator Sign In. 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.
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. Engineering Geology Special Publication: Geochimica et Cosmochimica Acta Geophysics ; 42 5: From Tectonics to Groundwater. Dipole-dipole induced-polarization measurements are commonly presented as pseudosections, but results using different dipole lengths cannot be combined into a single pseudosection.
On: “A modified pseudosection for resistivity and IP” by L. S. Edwards (GEOPHY
The modified pseudo-depth section as a tool in resistivity and IP prospecting; a case history. Processes on the Early Earth. View Full GeoRef Record. Citing articles via Web Of Science Previous Article Next Article.
Eos, Transactions, American Geophysical Union 62 8: On measuring the electrical conductivity of the oceanic crust by a modified magnetometric resistivity MMR method.
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This definition of effective depth is applied to other electrode arrays. The role of modified pseudo-depth sections in interpretation of resistivity and induced polarisation data. A modified pseudosection for resistivity and IP L.
This leads to an absolute depth scale for the modified pseudosection.