Go Metals Corp. C.GOCO

New IR presentation with new information

[davidmb4]

Just go to their website.
some new core pictures.

I like the following comments

- Late-stage dykes developed from fractionation of anorthosite melt

• Dykes span 10’s of km in strike length

• Classic “Sulphide Matrix Ore Breccia” textures

• Silicate-sulphide Emulsion/Net textures

Wgere do you see "sulphide matrix ore breccia"?

https://www.sciencedirect.com/science/article/abs/pii/S016913681830204X
Sulfide matrix ore breccias are particularly well developed in the Voisey’s Bay and Aguablanca deposits, where they developed by flooding of percolating sulfide melt through the silicate matrix of magmatic intrusion breccias, displacing silicate melt.