Renforth Resources Inc. (CSE: RFR | OTCQ: RFHRF) has announced that it has received assay results which show that channels cut within three stripped trenches at the company’s Surimeau property, Quebec, have shown the intersection of surface battery metals mineralization.
In addition to this, Renforth has further announced that three drill holes, Prop5 (SUR-22-30), Prop4 (SUR-22-31), and Prop2 (SUR-22-31), have been completed at Lalonde in an ongoing Surimeau drill programme, successfully intersecting the surface mineralization in the undercutting drill hole.
Each hole drilled starting in the sediments to the north, drilled through the mineralized/ultramafic package to the point of contact with the sediments in the south.
Renforth has stated that due to the intersection of the complete package in each hole, a second southern or undercut hole was not required (as previously planned), instead, metres will be used to the east, based upon the analysis of the 2021 geophysical survey data which Renforth has just received.
The company commissioned an analysis and interpretation of the geophysical data obtained during the airborne survey which was flown over the Victoria mineralized system and a portion of the Lalonde mineralized system.
One of the products of this analysis was a conductivity map, showing conductive anomalies within the overall magnetic anomaly at Victoria and Lalonde.
A magnetic anomaly stretches over ~20km at Victoria, and ~9km at Lalonde, and depicts an ultramafic intrusive, which the company believes to be carrying nickel, cobalt, and some number of PGEs.
Within the location of the ultramafic Renforth has stated it has seen graphitic shale that is copper and zinc bearing, along with calc-silicate alteration carrying the same mineralization, however, the magnetic anomaly does not reflect these structures, there is potential that the conductivity map does, hence Renforth will be carrying out tests to investigate its hypothesis.
To find out more, please visit www.renforthresources.com
