The two completed drill holes intersected mafic metavolcanic tuffs and flows at the amphibolite grade of metamorphism. Both holes contained sufficient sulphide minerals, mainly pyrrhotite to account for the IP chargeability anomalies, however, the quantity and type of sulphides (dominantly pyrrhotite) are such that the intersected zones are considered to be non-economic and no further work is recommended directed at the localization of sulphide mineralization of economic interest.