Magmatic shingle breccias adjacent to the copper-silver occurrence at Golden Bear property. The complex intrusive relationships and breccia textures indicate a dynamic and powerful intrusive system with evidence of differentiation from a quartz gabbro to granodiorite through to felsic aplite dyke swarms associated with quartz veining.
Magmatic shingle breccias adjacent to the copper-silver occurrence at Golden Bear property. The complex intrusive relationships and breccia textures indicate a dynamic and powerful intrusive system with evidence of differentiation from a quartz gabbro to granodiorite through to felsic aplite dyke swarms associated with quartz veining.