Yes looks around 50% larger plus there’s other outcrops nearby....

Yes looks around 50% larger plus there’s other outcrops nearby. Of course a lot undercover at what then is called Main Zone.Be interesting to see if they’re having a look at it to sample for spodumene.
They’re not mafic rocks ( amphibole) as it’s light not dark coloured, but similar colour to the Jamar pegmatite colour. As well it’s in a demagnetised lineament. This is where minerals loose their magnetic properties due to thermal interaction ie hot fluids.
Pegmatites form from hot water around 500 degrees carrying mineral ions , ligands and importantly flux components such as fluorine
The area I marked as high potential for FWZ in outcrop is also in a demagnetised zone ( as of course is MZ/FWZ.
Plus all those areas in topographical highs. I’ll post something to show that bit later on.