@rabbitoh does this sound familiar?
The presence of Sanukitoids is particularly significant as they represent intrusive rocks derived from enriched
magmas and hold an association with many large gold deposits globally. Their geochemical signature indicates
an enriched mantle source, similar to lamprophyre intrusives, and confirm the presence of deep-seated
structures with potential to introduce significant gold bearing fluids. The presence of Sanukitoids is another
supporting factor reflecting the broader prospectivity of the Wallbrook Gold Project.
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