NiCAN Confirms New Gold Discovery in Thompson Manitoba, Intersecting 27.6 Meters of 1.25g/t Gold
Diamond drill hole PIPY25-04, the first to test the target, intersected mineralized silicified biotite gneiss and silicate facies iron formation with disseminated pyrrhotite, pyrite and minor visible galena. A 27.6m section returned 1.25 g/t Au and 12.5 g/t Ag from 20.4m downhole, including 14.2m averaging 2.14 g/t Au and 19.8 g/t Ag.
Table 1. Highlights from Diamond Drill Holes PIPY25-04 and PIPY25-05 on the Pipy South Property
|
Hole # |
From (m) |
To (m) |
Length (m) |
Gold g/t |
Silver g/t |
|
PIPY25-04 |
20.4 |
48.0 |
27.6 |
1.25 |
12.5 |
|
PIPY25-04 incl. |
21.4 |
35.7 |
14.3 |
2.14 |
19.8 |
|
PIPY25-04 incl. |
33.7 |
35.7 |
2.0 |
5.39 |
7.10 |
|
PIPY25-05 |
9.6 |
19.1 |
9.5 |
0.65 |
8.40 |
Diamond drill hole PIPY25-05 was drilled to the west and above PIPY25-04 and is interpreted to have overshot the zone but still returned 9.5m averaging 0.65 g/t Au and 8.4 g/t Ag.
The 50-gram fire assay results were subsequently verified by photon assaying on approximately 500-gram samples. The correlation between the two-assay methods was very high with the photon assaying of PIPY25-04 returning 1.28 g/t Au over 27.6m and PIPY25-05 returning 0.66 g/t over 9.5m. The correlation between the 50-gram and 500-gram samples suggest a well disseminated mineralized body with a low nugget effect on the gold.
Holes PIPY25-07 and PIPY25-08 were drilled 25m to the south and both intersected a broad zone of silicification and mineralization. Assays are pending. The zone is interpreted to strike to the north, remains open in all directions, and appears to dip steeply to the west.
The gold mineralization is hosted within a silicate facies iron formation and a silicified biotite gneiss, which visually contains an estimated 1% to 5% disseminated pyrrhotite as well as up to 1% galena and minor chalcopyrite. Alteration is marked by bleaching and silicification that has not been completely defined by the limited 2025 drilling and hole PIPY25-07 displayed alteration along its entire length of over 80m. The presence of gold mineralization in iron formation and associated alteration is analogous to other iron formation hosted gold camps including Homestake, Musselwhite,
The iron formation hosting the gold mineralization is magnetic and can be traced throughout the property utilizing an historical airborne magnetic survey reprocessed by
A historical diamond drill hole in the same vicinity, 17BN01, returned 6.63 g/t Au over 5.6m within a wider zone of 1.20 g/t Au over 47.0m starting at 27.0m downhole hosted by similar rock types to those seen in the
Table 2. Historical Gold Intercept on the Pipy South Property
|
Hole # |
From (m) |
To (m) |
Length (m) |
Gold g/t |
Silver g/t |
|
17BN01 |
27.0 |
74.0 |
47.0 |
1.20 |
5.90 |
|
17BN01 incl. |
55.4 |
61.0 |
5.6 |
6.63 |
10.13 |
|
17BN01 incl. |
57.4 |
59.4 |
2.0 |
15.35 |
14.80 |
From historical reports
A second 2017 historical diamond drill hole, located 500m north of hole 17BN01, targeted an extensive north-south trending magnetic anomaly interpreted to be a nickel target. A garnet bearing amphibolite was encountered at a depth of 153.4m to 160.2m that contained sufficient disseminated pyrrhotite to explain the magnetic signature. No significant nickel assays were returned in the interval but a 2.0m long portion assayed 0.39 g/t gold at 157.4m, indicating other gold bearing zones are present.
Pipy Project Overview
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