So I have previously done research on how the ore body may have been formed and spoken to several geologists, including one who used to be a competent person who estimated mineral resources under the JORC code.
Hydrothermal breccia occurs when a void opens due to volcanic activity. The void fills with boiling water or hydrothermal fluid (200-300 deg C) and rock etc. As the solution cools the ore minerals precipitate out across the fault. Because the ore minerals were dissolved in water, as I understand, the mineralisation should be fairly homogenous throughout.
So I have previously done research on how the ore body may have...
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