GBR and partners up the ante and acquire more tenements while the majority of Eastern Mafic results are still in assay:
The discovery of primary copper-nickel-cobalt mineralisation at Mt Venn and Eastern Mafic indicates that a magmatic sulphide system was active along the margins of this shear zone and that further intrusions may occur.
Elevated levels of nickel and copper have been identified in historical aircore drilling and these will be assessed in upcoming exploration programs.
