Self‐potential signals associated with preferential ground water flow pathways in a buried paleo‐channel
- 12 April 2005
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 32 (7)
- https://doi.org/10.1029/2004gl022124
Abstract
No abstract availableThis publication has 8 references indexed in Scilit:
- The hydroelectric problem of porous rocks: inversion of the position of the water table from self-potential dataGeophysical Journal International, 2004
- Groundwater redox conditions and conductivity in a contaminant plume from geoelectrical investigationsHydrology and Earth System Sciences, 2004
- Electrical resistivity ground imaging (ERGI): a new tool for mapping the lithology and geometry of channel‐belts and valley‐fillsSedimentology, 2002
- Second Generation of Lead-lead Chloride Electrodes for Geophysical ApplicationsPure and Applied Geophysics, 2000
- Imaging the Water Table by Filtering Self‐Potential ProfilesGroundwater, 1998
- Electrical Imaging of Saline Tracer Migration for the Investigation of Unsaturated Zone Transport MechanismsHydrology and Earth System Sciences, 1997
- Rapid least-squares inversion of apparent resistivity pseudosections by a quasi-Newton methodGeophysical Prospecting, 1995
- SPONTANEOUS POTENTIALS AND RESISTIVITY SURVEYS APPLIED TO HYDROGEOLOGY IN A VOLCANIC AREA: CASE HISTORY OF THE CHAÎNE DES PUYS (PUY‐DE‐DÔME, FRANCE)1Geophysical Prospecting, 1989