Annual report on 1984 exploration for EL 2362

Abstract

With in the EL the only sediments outcropping are from the Finniss River Group. These are siltstones, shales, greywackes and conglomerates of the Burrell Creek Formation. Quartz veining associated with faulting and shearing provides the focus for any possible mineralisation. Small anomalies within the area were investigated and examined during the year. Their potential lies in their proximity to the major anomaly at Bundey 1.