1887
Volume 43 Number 7
  • E-ISSN: 1365-2478

Abstract

Abstract

It is seen that the apparent chargeability (M) anomaly over a 2D graphite body splits into two distinct (V) anomalies which closely follow the apparent resistivity profile. This suggests that the electric field amplitude is distorted due to a superficial inhomogeneity creating a (V) anomaly, which bears no relation to the polarized body. The target depth obtained by continuation of such a profile is therefore, not acceptable.

Loading

Article metrics loading...

/content/journals/10.1111/j.1365-2478.1995.tb00287.x
2006-04-28
2024-03-28
Loading full text...

Full text loading...

References

  1. ApparaoA. and RaoT. Gangadhara1983. The method of downward continuation of induced polarization data obtained with linear electrodes. Geophysical Research Bulletin21 (3), 271–281.
    [Google Scholar]
  2. ApparaoA., RaoT. Gangadhara and Subrahmanya SarmaV.S.1991. Field results with downward continuation technique in induced polarization profiling using point electrodes. Geophysical Prospecting39, 119–139.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/journals/10.1111/j.1365-2478.1995.tb00287.x
Loading
  • Article Type: Research Article

Most Cited This Month Most Cited RSS feed

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