Thanks Brett to your contributions in helping G2 Goldfields unlock the structural controls of the very high grade mineralization across their beautiful gold district in Guyana.
Thanks for uploading this talk. I notice that for the Hammerdown and Cape Ray shear zone examples, both have an estimated change in far field stress of 15-20 degrees. I am curious if this is a sweet spot or if a greater change in orientation can also sponsor mineralisation?
Thanks Brett to your contributions in helping G2 Goldfields unlock the structural controls of the very high grade mineralization across their beautiful gold district in Guyana.
Thanks for uploading this talk. I notice that for the Hammerdown and Cape Ray shear zone examples, both have an estimated change in far field stress of 15-20 degrees. I am curious if this is a sweet spot or if a greater change in orientation can also sponsor mineralisation?
Ggp going to be a monster