RE: Ernest Giles Research Thread14 Apr 2024 20:06
Thanks Magic that article does sound like EG
“ Banded iron formation-hosted gold deposits are attractive targets thanks to their potential for large, district-scale gold mining.”
Meadows could be 5km long and may stretch to 9km or more.
https://polaris.brighterir.com/public/greatland_gold/news/rns/story/x2vkg6w
The blue lines in a NW-SE trend is the banded iron formation with granotoids following it.
How they describe what’s there is very interesting :-
“Drilling confirmed that gold anomalism is hosted within altered basalts, banded iron formation (BIF) and syenite (Figure 1). The mineralised zone of 8m @ 0.12g/t Au from 316m in EGD006 is associated with thin quartz - carbonate veinlets in silica-sericite-chlorite and albite alteration in the basalt host (Figure 2). Hematite alteration was also observed. The syenite intersected in EGD005 shows gold is associated with disseminated pyrite with silica-sericite, albite and hematite alteration and quartz-carbonate veining.
”
“ The results indicate an encouraging broad, weak (Au-Ag-Cu-Zn) mineralisation. This could be the edge of a larger system. The anomalism is geologically controlled by generally east-dipping vein sets and vein-associated alteration. A correlation was noted between the weak gold-silver mineralised intercepts, geochemically anomalous, low order bismuth (Bi) values and the chlorite-carbonate alteration zones. The peak Cu value of 1,178ppm from 390.2m in EGD006 was in a highly sulphidic altered BIF unit. These associations can be used to better target further drilling.”
All looking very interesting.