1887
ASEG2007 - 19th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

Resistivity and induced polarisation data are very useful for defining lithological boundaries, shear zones (often with conductive and chargeable graphite), and sulphide alteration zones. The useful depth for interpretation depends upon the magnitude of the measured voltages and the effective current penetration, which in turn are determined most often by surface conditions at the electrode locations and subsurface electrical structure. Downhole resistivity and IP measurements are relatively quick to acquire, and can add significantly to the depth information of the surrounding surface survey. Bottomof-hole to surface surveying can be performed without any specialised downhole IP equipment. Examples over shear zones in southern Mali demonstrate the added information from inverting surface data with data from bottom-of-hole current injection with surface receiver electrodes.

Loading

Article metrics loading...

/content/journals/10.1071/ASEG2007ab160
2007-12-01
2026-01-18
Loading full text...

Full text loading...

References

  1. Asch, T., and Morrison H.F., 1989, Mapping and monitoring electrical resistivity with surface and subsurface electrode arrays: Geophysics, 54, 235-244.
  2. Loke, M.H., 2004, Tutorial : 2-D and 3-D electrical imaging surveys: http://www.geoelectrical.com/coursenotes.zip.
  3. Oldenburg, D.W., and Li, Y., 1999, Estimating depth of investigation in DC resistivity and IP surveys: Geophysics, 64, 403-416.
/content/journals/10.1071/ASEG2007ab160
Loading
  • Article Type: Research Article
Keyword(s): downhole geophysics.; electrical geophysics; Induced polarisation; inversion
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error