Torr Metals Confirms Copper and Gold Mineralization in Outcrop and Expands Geophysical Targeting at Kolos Project

TORR Metals, Inc.
TORR Metals, Inc.

In This Article:

Figure 1. Kolos Project Area

Kolos Project area with highly anomalous 2023 rock grab samples overlying ZTEM resistivity inversion at 200m vertical depth. Recently identified grassroots exploration target areas are delineated by the red dashed line. A to A’ cross-section line for Figure 2 outlined. Note that gaps in the ZTEM resistivity data were caused by powerline disruption and the location of Highway 5.
Kolos Project area with highly anomalous 2023 rock grab samples overlying ZTEM resistivity inversion at 200m vertical depth. Recently identified grassroots exploration target areas are delineated by the red dashed line. A to A’ cross-section line for Figure 2 outlined. Note that gaps in the ZTEM resistivity data were caused by powerline disruption and the location of Highway 5.

Figure 2. ZTEM 3D Resistivity Inversion Model

ZTEM 3D Resistivity Inversion Model voxel slice through the Kirby and Vik Zones. Additional untested geophysical exploration targets annotated to the southwest and northeast together with outlined dimensions of moderate to high resistivity targets that extend to-surface. View looking northwest.
ZTEM 3D Resistivity Inversion Model voxel slice through the Kirby and Vik Zones. Additional untested geophysical exploration targets annotated to the southwest and northeast together with outlined dimensions of moderate to high resistivity targets that extend to-surface. View looking northwest.

Figure 3. Kolos Project Location

Kolos Project location within the prolific porphyry belt of the Quesnel Terrane in south-central British Columbia. Figure including locations of Late Triassic Alkaline and Calc-Alkaline intrusions modified from Mitchinson et al. 20224. Note comparisons with regional porphyry deposits are not indicative of mineralization on the Kolos Project.
Kolos Project location within the prolific porphyry belt of the Quesnel Terrane in south-central British Columbia. Figure including locations of Late Triassic Alkaline and Calc-Alkaline intrusions modified from Mitchinson et al. 20224. Note comparisons with regional porphyry deposits are not indicative of mineralization on the Kolos Project.

VANCOUVER, British Columbia, June 13, 2024 (GLOBE NEWSWIRE) -- via IBN – Torr Metals Inc. (“Torr” or the "Company") (TSX-V: TMET.V) is pleased to announce the final assay results from the 2023 rock sampling program and delineation of a robust ZTEM geophysical anomaly at the newly-defined Vik Zone, within the eastern portion of the 100% owned 240 km2 Kolos Copper-Gold Project (the “Project”) (Figure 1, Figure 2). Additionally, the Company has completed its early reconnaissance field sampling program that includes coverage over newly acquired ground to the north and east (see May 29, 2024 news release) with assays pending for 27 outcrop and float rock grab samples.

The Vik Zone is a new discovery of copper (Cu) and molybdenum (Mo) mineralization in outcrop, on the margins of one of three highly prospective and untested moderate to high resistivity anomalies identified across a >2.5 kilometer (km) trend (Figure 1). No historical records exist of prior surface mapping or sampling in this area, suggesting significant potential for future grassroots discoveries within similarly unexplored areas of the recently expanded Kolos Project. The Project is located on Highway 5 just 23 kilometers (km) north-northeast of the city of Merritt, British Columbia (Figure 3).

Highlights: 

  • Outcrop Mineralization Coincident with 2023 Soil Anomalies: Recent rock grab samples have confirmed anomalous Cu ± gold (Au) ± Mo in outcrop coincident with 2023 soil sampling (see March 25, 2024 news release) and ZTEM geophysical anomalies. Of a total 47 rock grab samples assayed 22 yielded >100 ppm Cu with 9 samples >500 ppm Cu; the highest value returned 4240 ppm Cu within the Clapperton Zone. A total of 8 rock grab samples returned >0.1 g/t Au with 2 samples >0.2 g/t Au; the highest value of 1.07 g/t Au occurred within the Kirby Zone (Figure 1). Untested outcrop mineralization offers prime starting points, greatly mitigating risk in future drill targeting efforts.

  • New Robust ZTEM Geophysical Anomalies in the East: Within the Vik Zone anomalous Cu-Mo mineralization occurs in outcrop coincident with the trend of a highly prospective west-dipping moderate to high resistivity anomaly that measures greater than (>) 500 m in width and 800 metres in-depth.

    • A large high resistivity signature at-depth, interpreted as a potential underlying source intrusion, appears to link the Vik mineral occurrence with a larger (>1.5 km) moderate to high resistivity anomaly coming to the surface to the northeast (Figure 2); planning is in progress for this area to be covered by soil sampling in 2024.