Page 224 - NEWGEN21-Proceedings-Full

Thursday’s Gossan – Our Early Exploration

Lighter S isotopes associated with the later

porphyries / M-veins / A-veins / aplite vein

dykes

Interpreted to reflect:

1. Proximity to the magmatic source

2. The strongly oxidised fluid responsible for

mineralisation

3. Given we are not yet in the ‘core’ potassic

alteration / mineralisation zone, these fluids

appear to be especially oxidised – enhanced

capacity for copper-gold mineralisation

45