Annual report for EL 27663 for the period 28 July 2014 to 27 July 2015

Abstract

Four field trips to obtain sample material were undertaken. Most of the area of interest at the centre of the syncline is covered in calcrete, with limited soil cover to sample. While the focus has been on identifying KIM's, this is only one of a number of interpretations of the source of the magnetic high and potential mineralisation. The depth of burial, of the magnetic anomaly, the occurrence of other volcanics in the synclinal structure and the occurrence of anomalous Cu and Zn in the vicinity of the Limbla Syncline may indicate other types of deposit.