CSE : REDC | OTCQB : REDRF
Peak
B.C
Initial drill program completed June 2024.
Tested two southern areas along an important structural setting for Cu-Au porphyry systems.
Drilling encountered altered alkaline intrusive rocks – the source of the 2% copper mineralization observed at surface remains open.
Excellent infrastructure.
Peak Central
Drilling identified megacrystic porphyritic rocks with intense sericite alteration.
Surface rock samples return grades of over 2.0% Cu. Rock-chip sampling has returned 25 metres grading 0.44% Cu.
Source of copper mineralization remains open.
Peak Central – IP Anomaly
Drill holes at Peak Central intersected a series of mixed sediments including black graphitic shales, sandstones and polymictic conglomerates. The sedimentary package is intruded throughout by a series of porphyry dykes and the highly chargeable zone outlined by IP geophysics is likely due to graphitic sediments and zones with up to 5% pyrite. In addition, a deep resistive centre targeted in RC-PG-02 is interpreted to be caused by quartz-rich sandstones, conglomerates and late porphyry dykes.
Peak North
Soil geochemistry outlines highly anomalous Cu, Ag values.
Elevated geochemistry is associated with interpreted intrusive-related magnetic highs and lows.
The area is bounded to the west by the Pinchi fault, an important NW regional structure associated with Cu-Au deposits.
