Quartz-stibnite veins at Goddell Gully represent only a few of the several antimony occurrences on Carbon Hill. Strong east-trending structures contain the showings over at least five kilometres of strike length. Deep drilling on the Goddell Shear Zone has encountered significant gold grades over wide intersections. The gold however is not in quartz-stibnite veins, but instead is associated with porphyry copper style alteration and densely disseminated pyrite and arsenopyrite. This report introduces and documents this previously unrecognized and potentially significant style of mineralization.