Image of 3D magnetic inversion model showing zone of high magnetics in sediment adjacent to the contact with low magnetic granite. An approximately 1 km long zone of high magnetics is coincident with the occurrence of iron-oxide rich breccia containing anomalous Cu-Zn-Pb.
Image of 3D magnetic inversion model showing zone of high magnetics in sediment adjacent to the contact with low magnetic granite. An approximately 1 km long zone of high magnetics is coincident with the occurrence of iron-oxide rich breccia containing anomalous Cu-Zn-Pb.