First annual report for EL 9856 'Gregory's Depot'

Abstract

All geophysical data has been reviewed and the source of the prominent magnetic feature has been analyzed. It appears that most likely source of the feature is a basis intrusive of post Properozoic age, possibly related to the Antrim Plateau Volcanics, though this is probably not an extrusive centre. This target could be a layered mafic intrusive, with potential for accumulations of metal sulfides deposits of Ni, Co, Cu etc. Follow up work would involve magnetic traverses, gravity, mobile ion geochemistry and subsequent drilling in year 3.