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The Bardoc Tectonic Zone Gold Endowment The Goongarrie greenstone belt lies on the northern sector of the Bardoc tectonic Zone (BTZ). This is an intensely gold-mineralised regional shear zone that runs from the Kalgoorlie in the south, where it forms the Boulder Lefroy Fault (BLF), to Menzies in the north. The BTZ is part of a complex zone of gold-mineralised strike-parallel regional shears that traverse the Kalgoorlie Terrain greenstones of the Norseman-Wiluna belt. From Kalgoorlie to Menzies it is the locus of numerous large gold deposits with a total gold endowment of over 90Moz. At Goongarrie the BTZ passes beneath salt lake cover, in a similar manner to the BLF south of Kambalda. This section of the BTZ has been notably overlooked by previous explorers, but as with the BLF at Kambalda, it may be equally well mineralised. The recessive weathering and salt lake cover may even be indicative of this.[URL unfurl="true"]https://www.kingwestresources.com.au/goongarrie-project.html[/URL]
The Bardoc Tectonic Zone Gold Endowment
The Goongarrie greenstone belt lies on the northern sector of the Bardoc tectonic Zone (BTZ). This is an intensely gold-mineralised regional shear zone that runs from the Kalgoorlie in the south, where it forms the Boulder Lefroy Fault (BLF), to Menzies in the north. The BTZ is part of a complex zone of gold-mineralised strike-parallel regional shears that traverse the Kalgoorlie Terrain greenstones of the Norseman-Wiluna belt. From Kalgoorlie to Menzies it is the locus of numerous large gold deposits with a total gold endowment of over 90Moz. At Goongarrie the BTZ passes beneath salt lake cover, in a similar manner to the BLF south of Kambalda. This section of the BTZ has been notably overlooked by previous explorers, but as with the BLF at Kambalda, it may be equally well mineralised. The recessive weathering and salt lake cover may even be indicative of this.
[URL unfurl="true"]https://www.kingwestresources.com.au/goongarrie-project.html[/URL]
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