Logging and interpretation of drill core indicates that Callisto is a separate mineralised sill that has intruded the pre-existing parent sill. The parent
sill has a strong magnetic signature which trends north-northeast with the parent sill outcropping over the five kilometre prospective horizon to the north. Drilling at Callisto is now focussed on determining the size and grade of the sulphide zone, and understanding the relationship with the much larger host sill, while looking for a possible source of the discovery
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