Geophysical responses over the Mount Ararate Prospect

A. J. Willocks

doi:10.1071/ASEGSpec11_06

Geophysical Signatures of Base Metal Deposits in Victoria

ISSN: 2202-0586
E-ISSN:

oa Geophysical responses over the Mount Ararate Prospect
Authors A. J. Willocks^a
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^a Geological Survey of Victoria, Department of Natural Resources and Environment, , PO Box 500 East Melbourne Victoria, 3002, .
Publisher: Australian Society of Exploration Geophysicists
Source: ASEG Extended Abstracts, Volume 1999, Issue Geophysical Signatures of Base Metal Deposits in Victoria, Dec 1999, p. 18 - 98
DOI: https://doi.org/10.1071/ASEGSpec11_06
- Published online: 01 Dec 1999

Abstract

The Mount Ararat Prospect is hosted in Cambrian greenstones in western Victoria. Early exploration showed excellent correlation between the soil geochemical copper peaks and electromagnetic anomalies over a gossan. Follow-up drilling resulted in discovery of the Mount Ararat Prospect by Pennzoil in 1975. Massive banded and disseminated chalcopyrite-pyrrhotite-sphalerite minerahsation occurs in mafic and pelitic schists. The deposit is uneconomic, with an inferred resource of approximately 1 million tonnes with grades of 2.7% copper, 10 g/t silver and 0.6 g/t gold. Chalcocite is common in a zone of supergene enrichment.

Geophysical surveys, including airborne electromagnetic (INPUT) survey, vertical-loop electromagnetics, ground magnetic surveys, magnetic induced polarization, induced polarization and rapid reconnaissance magnetic induced polarization RRMIP, were used to delineate the extent of minerahsation. The INPUT survey and gradient-array induced polarzation results were disappointing due to a very conductive surface layer. Magnetic induced polarization surveys were effective in delineating an anomalous conductive zone corresponding to the minerahsation.

Downhole resistivity and induced polarization logs show the mineralised zone has coincident chargeability and resisitivity responses but the chargeability response is broader and more extensive indicating a possible disseminated pyrite halo in a broader zone around the massive sulphides.

Experimental time domain electromagnetic surveys using the UTEM and SIROTEM systems recorded responses over the minerahsation but these techniques have not been routinely used for exploration. The early-time electromagnetic data is affected by a highly conductive near surface layer.

The magnetic responses associated with the deposit are caused by the host rocks, and are not a direct response from the mineralisation. These units remain prospective along strike for base metals and gold.

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References

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