Remote remanence estimation (RRE)
David A. Pratt 1 2 K. Blair McKenzie 1 Tony S. White 11 Tensor Research Pty Ltd, PO Box 8159, Greenwich, NSW 2065, Australia.
2 Corresponding author. Email: David.Pratt@tensor-research.com.au
Exploration Geophysics 45(4) 314-323 https://doi.org/10.1071/EG14031
Submitted: 19 March 2014 Accepted: 2 August 2014 Published: 17 September 2014
Abstract
The remote determination of magnetic remanence in rocks is a method that has largely been ignored because of the ambiguity associated with the estimation of both the Koenigsberger ratio and remanent magnetisation direction. Our research shows that the resultant magnetisation direction can be derived directly through inversion of magnetic data for an isolated magnetic anomaly from a compact magnetic source. The resultant magnetisation direction is a property of the target magnetic rocks and a robust inversion parameter. The departure angle of the resultant magnetisation vector from that of the inducing magnetic field is an important indicator of the existence of remanent magnetisation and the inversion process can detect departures that are not easily detected by visual inspection. This departure angle is called the apparent resultant rotation angle or ARRA.
The induced field vector, remanent magnetisation vector and resultant magnetisation vector lie on the plane of a great circle. We find the intersection of the transformed polar wander vector trace with the great circle plane to obtain one or more possible solutions for the remanent magnetisation vector. Geological deduction will normally allow us to reduce the ambiguity for multiple solutions to obtain the most likely remanent magnetisation direction. Once the remanent magnetisation direction is established, it is then possible to determine the Koenigsberger ratio and magnetic susceptibility for the target.
We illustrate the methodology using survey data over the Black Hill Norite which also has extensive palaeomagnetic data available for comparison with the inversion results. We then apply the remote remanence estimation (RRE) method to a systematic study of a large number of intrusive pipes in the Thomson Orogen, New South Wales. The corrected magnetic susceptibility and remanence properties, spatial distribution and underlying uncertainties are evaluated for their potential use by diamond explorers. The additional information assists with differentiating kimberlites from other intrusive pipes based on age and remanence properties.
Key words: inversion, kimberlite, magnetisation, remanence, resultant, susceptibility.
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