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Balmoral Resources Ltd.

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Summary

Project:

Grasset

Deposit:Grasset
Location:Canada
Commodities:Gold
Date:1/17/2019
Report Code:NI43-101
Report Type:Exploration/Drilling Update
Project Stage:Pursuing Resource Increase/Upgrade
Report details:17-1-2019: Balmoral Resources Ltd. announces an Exploration/Drilling Update report for its Grasset deposit at the Grasset project. Drilling results incl. 42.10m @ 0.31% NI, 0.01% Cu. 0.015 Co, 0.04g/t Pt, 0.09g/t Pd from 180.05m. (Vancouver, January 17, 2
Resources:(not mentioned in this report)
CP/QP:[Overall Report]: Michael Tucker, Darin Wagner (Internal)
ABSTRACT:(Vancouver, January 17, 2019) Balmoral Resources Ltd. (“Balmoral” or the “Company”) (TSX: BAR; OTCQX: BALMF) today announced the discovery of numerous nickel-copper-cobalt-PGE sulphide mineralized zones within the central portion of the Grasset Ultramafic Complex (“GUC”) in Quebec. The new discoveries are located 7 kilometres northwest of, and along strike from, Balmoral’s Grasset nickelcopper-cobalt-platinum-palladium deposit (Figure 1). These discoveries reinforce the district scale and multi-deposit potential of the GUC. Results are highlighted by an intercept of 7.58 metres grading 1.05% nickel, 0.31% copper, 0.05% cobalt, 0.20 g/t platinum and 0.48 g/t palladium from one of three new discoveries, each of which returned greater than 1% nickel, intersected in drill hole FAB-18-58. A massive sulphide intercept returning 4.14% nickel, 0.26% copper, 0.18% cobalt, 0.81 g/t platinum and 1.93 g/t palladium over 0.65 metres occurs at the base of this intercept (Photo 1). A second intercept, located approximately 100 metres shallower and along the same stratigraphic horizon in drill hole FAB-18-56, returned 1.35% nickel over 3.94 metres, including 3.59% nickel over 1.03 metres with similar copper, cobalt, platinum, and palladium values (see Table 1 below). The central ultramafic (komatiite) volcanic unit that hosts these discoveries remains largely untested on the property. Follow-up borehole EM work has identified strong conductors associated with these new semi-massive to massive sulphide discoveries in multiple holes. The conductors indicate the potential for additional alongstrike, up-dip and down-dip/plunge continuity of the sulphide horizons. Off-hole EM anomalies, indicating the potential for additional massive to semi-massive sulphide discoveries within the host ultramafic volcanic sequence, have also been identified. These geophysical anomalies provide immediate targets for follow-up drilling.

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