1887
ASEG2001 - 15th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Multi-parameter logging at Marvel Loch gold mine in the Yilgarn Craton of Western Australia indicated that the mineralisation was more conductive than the host rocks and thus potentially targeted using downhole electrical methods. Borehole MMR was the preferred to borehole EM due to the lack of large zones of consistently conductive mineralisation and the lack of conductive features within the surrounding host rock.

The drilling program consisted of a parent hole with a number of wedges. Two of these wedge holes were surveyed with borehole MMR however the upper portion of the hole through the overburden/regolith (ie.the parent hole) could not be surveyed due to steel casing and thus the nature of the conductive overburden could not be readily determined. Hence an empirical approach was initially taken whereby stripping the raw total MMR field with a layered-earth field was computed for a range of different overburden conductivities until a credible background to the axial component of the anomalous MMR response is obtained. TEM soundings acquired post survey in the vicinity of the drillhole collar to assist in determining the overburden characteristics and improved the stripping process.

The results of the two wedge holes were similar with subtle negative axial anomalies related to the upper and lower mineralised zones and thus attributable to conductors below the drillholes. The modelling indicates a southerly plunge to the lower conductive zone which is consistent with the southerly plunge of the mineralisation within the pit. The adjacent pit has been modelled as conductor carrying current in the reverse direction to simulate a resistor producing a minimum at around 150m and influences the shape and amplitude of the anomaly due to the upper alteration zone.

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/content/journals/10.1071/ASEG2001ab063
2001-12-01
2026-01-19
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References

  1. Asten M.W., 1988, The downhole magnetometric resistivity method. Exploration Geophysics 19, 12-17.
  2. Asten, M.W.,2000, Magnetometric and inductive EM modeling in 3D using tubes of electric current: Expanded Abstracts, SEG 2000 International Exposition and 70th Annual Meeting, 6-11 August 2000, Calgary.
  3. Bishop, L, Lewis, R., and Stoltz, N, 2000, Horses for (conductive) courses: Exploration Geophysics 31, 192-199.
  4. Meyers, I, Cooper, M., Bishop, J.R. and Hatch, M., 2000, Downhole MMR surveying for refractory gold ore at Wiluna gold mine, W.A.m Abstracts of ASEG Conference, Perth: Preview 84,p.79.
  5. Veitch D., Asten M.W, and van Leeuwen E. H., 1990, Electrical and magnetometric fields in a layered earth containing buried electrodes. Geophysics 55 , 1605-1612.
  6. Witt W.K. , 2000, Two Separate Hydrothermal Events at Marvel Loch Gold Deposit, Western Australia. Geological Society of Australia, Abstracts No. 59, 15th Australian Geological Convention, Sydney, July 2000.
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  • Article Type: Research Article
Keyword(s): borehole magnetometric resistivity; gold
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