This is the part of the announcement that has me interested.
"Similar to the previous hole a substantial zone of massive hematite and hematite breccias was intersected
from 1302 to 1623m downhole with a very high frequency of 1m to 20m wide intervals of mafic dyke. The
remainder of the hole comprised mostly altered felsic gneiss with mafic dykes and thin hydrothermal hematite
breccias.
The substantial downhole thicknesses of dense hematite breccias, a cumulative downhole thickness of approx.
200m in VUD018 and 300m in VUD019 is considered a very successful test of the Vulcan North density
anomaly".
This is the part of the announcement that has me...
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