Annual report for EL 29827 SXB Project 29 August 2014 to 28 August 2015

Abstract

During the past year exploration desktop geology and geophysics studies have been completed. The rocks in the area consist of a sequence of calc-silicate rocks with interbedded marbles striking approximately 340 degrees and dipping north easterly at 30 - 50 degrees. The sequence has been heavily invaded by numerous quartz-feldspar pegmatite. Several occurrences of an actinolite-rich rock were delineated within the area. These are probably derived from metasomatic alteration of an originally impure calcareous sediment. Several conformable dykes approaching micro-granodiorite in composition were also delineated. Mineralisation in the area consists of weak malachite staining within, two pegmatites and within one outcrop of an actinolite-rich rock, which bears some resemblance to that occurring within the Johnnies Reward copper prospect.