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The effect of overburden on vertical component anomalies in AFMAG and VLF exploration; a computer model study

Keeva Vozoff

Open publisher page 28 citations

Abstract

Abstract New computer techniques permit the calculation of AFMAG and VLF anomalies in the vertical magnetic field component for situations which cannot be conveniently modeled with analog models. Conductivity and geometry of the 'ore' zone, the overburden, and the bedrock can all be varied independently; although all must have the same strike direction. Model results accurate to about 10 percent can be obtained at negligible cost.One example shows how a decrease in overburden resistivity from 100 ohm-m to 10 ohm-m can obliterate a distinct AFMAG anomaly. An increase of overburden thickness from 20 m to 50 m has the same effect. This study shows the importance of obtaining some direct overburden resistivity data before ruling out areas which show no anomalies.

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Abstract New computer techniques permit the calculation of AFMAG and VLF anomalies in the vertical magnetic field component for situations which cannot be conveniently modeled with analog models. Conductivity and geometry of the 'ore' zone, the overburden, and the bedrock can all be varied independently; although all must have the same strike direction. Model results accurate to about 10 percent can be obtained at negligible cost.One example shows how a decrease in overburden resistivity from 100 ohm-m to 10 ohm-m can obliterate a distinct AFMAG anomaly. An increase of overburden thickness from 20 m to 50 m has the same effect. This study shows the importance of obtaining some direct overburden resistivity data before ruling out areas which show no anomalies.

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Available abstract

Abstract New computer techniques permit the calculation of AFMAG and VLF anomalies in the vertical magnetic field component for situations which cannot be conveniently modeled with analog models. Conductivity and geometry of the 'ore' zone, the overburden, and the bedrock can all be varied independently; although all must have the same strike direction. Model results accurate to about 10 percent can be obtained at negligible cost.One example shows how a decrease in overburden resistivity from 100 ohm-m to 10 ohm-m can obliterate a distinct AFMAG anomaly. An increase of overburden thickness from 20 m to 50 m has the same effect. This study shows the importance of obtaining some direct overburden resistivity data before ruling out areas which show no anomalies.

Key concepts: Overburden, Geology, Ohm, Electrical resistivity and conductivity, Bedrock, Anomaly (physics), Component (thermodynamics), Geophysics

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The effect of overburden on vertical component anomalies in AFMAG and VLF exploration; a computer model study — Research Paper | ScholarLens