These mineralised dykes ( probably overprinting earlier non...

These mineralised dykes ( probably overprinting earlier non mineralised dykes) are structurally controlled first moderately by the ultramafic contact to the east but absolutely by the LAS below which acts as a offset fault .
59 is to 51 what 55/56 were to 50 ie to test the dykes intercept where it’s been faulted by the LAS, the width, grades etc.Like this I’d gather.


At the moment it’s just been interpreted.What really interesting if the width/grades of 50/51 are repeated on contact with the LAS. If they are then to find where it’s been faulted down lower will be a complete game changer. This will also give further vectors to finding the Cu/Au porphyry if it’s there ( or if it’s a Butte Mo style system).