NR: initial take-aways are very positive, imoI am not sure what the negatives are.
The following is expecially encouraging to me:
- Disseminated, interstitial, net-textured, semi-massive, sulphide mineralization occurring at 304 - 384.5m1 in GL23009 (Photo 3)1 significantly extends the historic Gochager Lake deposit at depth.
as is the reference to the source/feeder zone made by Ian.
Bb