Cross section of the Brunswick South deposit with the Costerfield Leapfrog geology model sliced at 5200N, where the greatest number of new high-grade intercepts are located. The spread of intercepts away from the model slice is due to the strike of the Brunswick South deposit being approximately 15 degrees east of mine grid north (as seen in Figure 3).
Cross section of the Brunswick South deposit with the Costerfield Leapfrog geology model sliced at 5200N, where the greatest number of new high-grade intercepts are located. The spread of intercepts away from the model slice is due to the strike of the Brunswick South deposit being approximately 15 degrees east of mine grid north (as seen in Figure 3).