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Great Western Exploration (ASX: GTE) has announced highly encouraging results from its latest diamond drilling at the Oval Copper-Gold Target, with preliminary observations indicating a potentially large Volcanic Hosted Massive Sulphide (VHMS) system. Drilling has intersected multiple prospective horizons that appear similar to the high-grade DeGrussa Copper-Gold Deposit in the adjacent Bryah Basin.
The latest diamond drill hole at Oval successfully intercepted a 35m-wide sedimentary-volcanic unit containing multiple sulphide lenses at a depth of 824m. This unit, combined with altered basaltic volcanics below, strongly suggests the drill hole is positioned close to a potentially metal-rich central zone of a VHMS deposits system.
Key observations from the geological logging include:
The combination of rock types, alteration patterns, and sulphide mineralisation closely resembles the characteristics of DeGrussa-style VHMS systems, which are known for their high-grade copper-gold mineralisation.
The Oval Target’s location appears to be particularly favourable for major mineral system development:
These geological features create an ideal structural setting for the development of significant VHMS mineralisation, similar to factors that contributed to the formation of the DeGrussa deposit.
Volcanic Hosted Massive Sulphide (VHMS) deposits represent some of the world’s most valuable mineral systems, often containing high-grade accumulations of copper, gold, zinc, and other metals. These deposits typically form on the seafloor where hydrothermal fluids from volcanic activity interact with seawater, creating “black smoker” vents that precipitate metal-rich sulphides.
What makes VHMS systems particularly attractive to investors:
The nearby DeGrussa deposit, discovered by Sandfire Resources in 2009, contained approximately 742,000 tonnes of copper and 1 million ounces of gold, highlighting the potential economic significance of these systems.
VHMS deposits are characterised by their formation in submarine volcanic environments where metal-rich hydrothermal fluids circulate through volcanic rocks and are discharged onto the seafloor. The metals precipitate as sulphide minerals when the hot, acidic, metal-bearing solutions mix with cold seawater. This process creates stratiform lenses of massive sulphide mineralisation that can be exceptionally rich in copper, zinc, lead, gold, and silver.
Geologists recognise several key zones within VHMS systems:
The presence of carbonate matrix breccia observed in Great Western’s drilling is particularly significant as these features often indicate proximity to feeder zones, which can host substantial mineralisation.
Great Western is well-positioned to advance exploration at Oval with:
The combination of promising geological indicators, strategic positioning, and financial capability puts Great Western in an advantageous position to pursue what could be a significant copper-gold discovery.
Great Western Exploration presents a compelling investment opportunity based on several key factors:
The next few months represent a pivotal period for Great Western as assay results from Oval will provide crucial data points to evaluate the economic potential of this discovery. Investors should closely monitor developments at this emerging copper-gold target, which has the hallmarks of a significant discovery in the making.
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