The development of an instrument that enables transient electromagnetic (TEM) measurements to be made to voltage levels of 1 μV/A and less has enabled the detection of an anomalous transient response in some areas with lateritic soil cover. This anomalous transient causes apparent resistivity values derived from the measured transient decay to decrease at late delay times in areas where the known geology indicates the values should increase with delay time toward the resistivity value of the basement. The main cause of the anomalous transient has been identified as the response of superparamagnetic material in the lateritic soil cover. Both field and laboratory measurements of the voltage M induced by this transient, show a t-1 time dependence. This is the same behavior reported previously for magnetic viscosity over a longer time scale. Measurements of magnetic susceptibility of material separated magnetically from soil samples taken at areas where a residual response is measured, show that over a wide t...
[1]
G. R. Olhoeft,et al.
Magnetic relaxation and the electromagnetic response parameter
,
1974
.
[2]
T. Lee,et al.
Transient EM Response of a Large Loop on a Layered Ground
,
1974
.
[3]
G. Buselli,et al.
SIROTEM: A New Portable Instrument for Multichannel Transient Electromagnetic Measurements
,
1977
.
[4]
M. Nabighian.
Quasi-static transient response of a conducting half-space; an approximate representation
,
1979
.
[5]
G. Buselli.
The application of SIROTEM in weathered terrain
,
1979
.
[6]
A computer model evaluation of the resistivity and IP response of the Elura deposit
,
1980
.
[7]
D. Dunlop.
Thermal enhancement of magnetic susceptibility
,
1974
.
[8]
Geoelectric properties of the Elura prospect, Cobar, NSW
,
1980
.