"GBR’s hole 23SBRC002, collared approximately 20m west of the historic hole intersected a broader zone of mineralisation at a similar depth, with 9m @ 5.20g/t Au from 15m in 23SBRC002 compared to 3m @ 7.42g/t Au from 14m in SJPRC002; this may reflect supergene dispersion of gold mineralisation within the weathering profile.'
If it is supergene enrichment , then could that dike they show be barren of ore ,below the redox boundary ie where oxidation has occurred ?
IF that has occurred have they found a tabular north striking lode of high grade mineralisation but with little vertical depth .
Not a geo so welcome to be corrected
"GBR’s hole 23SBRC002, collared approximately 20m west of the...
-
- There are more pages in this discussion • 18 more messages in this thread...
You’re viewing a single post only. To view the entire thread just sign in or Join Now (FREE)
