The results confirm that there are thin but but correlatable zones of Zinc and Lead in all holes with best intercepts as follows:
- PAD001: 1.1m @ 5.76% Zinc (Zn) and 1.58% Lead (Pb) with associated Silver (Ag)and Cadmium (Cd) of 14.7g/t Ag and 256pp m Cd from 80-81.1m;
- PAD002: 2.2m @ 3.9% Zn and 0.86% Pb with 16.5g/t Ag and 152ppm Cd from 109-111.2m; and
- PAD003: 0.4m @ 0.96% Zn from 106.6m – 107m and 0.5m @0.87% Zn and 0.2% Pb. from 137.1-137.6m
The Cd and Ag results are also consistent with the soil a nomalism. The association continues to point to a Broken Hill type mineralisation style. For this style of mineralisation to be economic it is considered that zones of structural complexity such as flexures or fold hinges are likely positions where w ider accumulations of sulphides may occur. Further work to determine such position s will now be undertaken, via detailed mapping.
Visual observation of the core and assay results provide no explanation for the IP anomalies.
As outlined in the quarterly, infill 25m by 25m soil sam pling and XRF assaying at Pamwa suggested that the original soil anomaly has resolved into two zones orientated parallel to the regional foliation as map ped in the area.
All RAB results reported were previously reported in ASX announcement dated 26 August and 29 September 2014.
The drilling results show a number of mineralised bands marked in red on the section which coincidentally run parallel to the foliation and can be correlated from the surface soil data and down dip in the diamond holes. These zones dip around -50 to the north east.
The diamond drilling was a deeper test of the initia l RAB drilling in June and July 2014 and consisted of 3 holes for a total of 581m.
