oa Drape Related Problems in Aeromagnetic Surveys: The Need for Tight-Drape Surveys

The trend towards higher flight height and loose-drape fixed wing surveys has important implications for high-resolution aeromagnetic surveys for mineral exploration, especially for targets such as kimberlites. The IAGSA specifications, implemented by leading airborne geophysical contractors and some Governments, make it virtually impossible to acquire adequate data in areas of even moderate relief using conventional aircraft. Variations in survey elevation give rise to changes in magnetic relief and magnetic texture that are not related to magnetic sources but are simply artifacts produced by varying depth-to-source. Important high frequency and low amplitude magnetic signals are absent in areas of high survey elevation and cannot be recovered by drape corrections which involve intrinsically unstable downward continuation.

Geophysicists are well aware of the loss of horizontal spatial resolution as survey elevation increases but the loss of subtle information on depth extent is even more serious in exploration for pipe-like bodies such as kimberlites. Aeromagnetic data are relatively insensitive to depth extent because of the rapid decay of the kernel function with depth. At shallow depths there is a clear difference in anomaly shape between a pipe source and a thin sheet but as depth-to-source increases these differences become much less obvious.

For cost-effective high-resolution aeromagnetic surveys for kimberlites we need to fly tight-drape surveys at low level, using aircraft designed to fly at low level such as the Pacific Aerospace Cresco and Fletcher FU-24. The terrain following ability of these aircraft is impressive.

Comparison of loose-drape and tight-drape data shows a dramatic improvement in high frequency content for tight-drape surveys with both magnetic relief and magnetic texture of small local anomalies being preserved. The loose-drape examples show significant variations in magnetic texture due entirely to variations in survey elevation.