Map 1. The merged grid-based and regional gravity data indicate that Junction appears to be underlain by an apophasis of a large intrusion and associated gravity high located immediately to the west. The Hall deposit (Mo-Cu-Au quartz veins in diorite) and Ashdown deposit (Cu-Ag quartz veins in granodiorite) are located at the north and south end of the intrusion, respectively.
Map 1. The merged grid-based and regional gravity data indicate that Junction appears to be underlain by an apophasis of a large intrusion and associated gravity high located immediately to the west. The Hall deposit (Mo-Cu-Au quartz veins in diorite) and Ashdown deposit (Cu-Ag quartz veins in granodiorite) are located at the north and south end of the intrusion, respectively.