NiCAN - Additional Assays from New Near Surface Gold Discovery in Thompson Manitoba, Intersecting 19.45 Meters Averaging 1.0g/t Au and 12.2 g/t Ag
Diamond drill hole PIPY25-08, intersected mineralized silicified biotite gneiss and silicate facies iron formation with disseminated pyrrhotite, pyrite and significant visible galena. Individual 1.0m assays returned 1.0g/t Au, 51.4g.t Ag and 3.74% Pb.
Table 1. Highlights from Diamond Drill Holes on the Pipy South Property
|
Drill Hole |
From (m) |
To (m) |
Length (m) |
Au g/t |
Ag g/t |
|
PIPY25-04 |
20.4 |
48.0 |
27.60 |
1.25 |
12.5 |
|
PIPY25-04 incl. |
21.4 |
35.7 |
14.30 |
2.14 |
19.8 |
|
PIPY25-04 incl. |
33.7 |
35.7 |
2.00 |
5.39 |
7.1 |
|
PIPY25-05 |
9.6 |
19.1 |
9.50 |
0.65 |
8.4 |
|
PIPY25-07 |
30.0 |
38.0 |
8.00 |
0.21 |
1.2 |
|
PIPY25-07 |
81.5 |
85.5 |
4.00 |
1.25 |
3.64 |
|
PIPY25-08 |
6.4 |
11.8 |
5.40 |
0.69 |
4.5 |
|
PIPY25-08 |
17.9 |
37.3 |
19.45 |
1.00 |
12.2 |
|
PIPY25-08 incl. |
31.8 |
36.8 |
5.00 |
2.17 |
28.7 |
Brad Humphrey, President and CEO of
Diamond drill holes PIPY25-07 and PIPY25-08 were drilled 25m to the south and both intersected a broad zone of silicification and varying quantities of mineralization. The mineralized zone is interpreted to strike to the north and south and remains open in all directions, dipping steeply to the west.
Diamond drill hole PIPY25-07 was drilled 25m south of PIPY25-04 and is interpreted to have overshot the zone but still returned 4.0m averaging 1.25g/t Au and 3.64g/t Ag within a pyrrhotite breccia. The hole was interpreted to be highly silicified throughout its length. Work permit restrictions limited the drill placement at the time. The Company has applied for and received a work permit allowing for a significant number of additional drill pads in this area for follow-up drilling.
PIPY25-08 was collared at -80 degrees from the same site as PIPY25-07. The hole intersected 19.5m averaging 1.0g/t Au, 12.2g/t Ag which included 5.0m near the bottom of the hole that returned 2.17g/ Au, 28.7g/t Ag and 2.07% Pb.
The gold mineralization is largely 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 3% galena and minor chalcopyrite. Alteration is marked by bleaching and silicification that has not been completely defined by the limited 2025 drilling. 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 (17BN01) in the same vicinity returned 6.63g/t Au over 5.6m within a wider zone of 1.20g/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 0.39g/t gold at 157.4m, indicating other gold bearing zones are present.
Pipy Project Overview
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