San Pablo Zone lies approximately 1.5 km south of San Albino Gold Zone. In January 2013
the Company announced the discovery of a new massive sulphide mineralization zone at San Pablo.
The Company has identified 5 priority drill targets within the San Pablo Zone for testing during its planned 2013 drilling program.
San Pablo Exploration Pits
In 2012, two exploration pits were excavated to expose the mineralized veins intersected by trenching along strike and down dip in trenches SP11-TR-02 and SP11-TR-04. Samples collected across the true thickness of the intersected veins returned values ranging from 3.46 g/t to 28.29 g/t gold and 0.21 g/t to 3.75 g/t gold
for trenches SP11-TR-02 and SP11-TR-04, respectively.
The exploration pit at SP11-TR-02 exposed structurally controlled, heavily mineralized sulphide masses (bodies) intercalated with quartz veins. These bodies carry significant gold values ranging from 1.50 g/t to 31.78 g/t gold with gold mineralization appearing to be more uniformly distributed. This is a new style of mineralization, significantly different from the quartz veins mineralization found at other prospects throughout the Property.
Trenching has outlined 4 parallel NE/SW trending structurally controlled mineralized zones (see Table 2 below and attached map) ranging from 300 to 1,500 metres in length, located approximately 1.5 kilometres south of the San Albino Gold Deposit and covering a 2.5 square kilometre area.
Significantly, the mineralized zones within all seven trenches consisted of intercalated quartz and schist, not just quartz veins. Gold mineralization, ranging from under 1 g/t to 37.37 g/t gold
, occurs not only in mineralized veins but also in the surrounding phyllite. Trench SAM12-TR-09 returned values from 1.66 g/t to 20.41 g/t gold within the quartz vein and 2.85 g/t to 6.48 g/t gold
within the host rock (weathered phyllite). Samples collected from weathered wall rock within the trenches returned high gold values, ranging from 1.11 g/t to 20.60 g/t gold
. This style of mineralization is the same as that at the San Albino Gold Deposit, where thicker intersections in drill core consist of anastomising quartz veins in schist.