Interpretation of regional geophysics can help find a new mining district
The McFaulds Lake stratiform Cr-Ni-Cu-PGE deposit is hosted in a layered mafic-ultramafic intrusion.
A regional aeromagnetic survey revealed a linear magnetic high that was not associated with any known deposits. A time-domain electromagnetic survey was flown and anomalies followed up with ground geophysics.
Follow up drilling resulted in the discovery of multiple Cr-Ni-Cu-PGE lenses.
A detailed gravity survey was conducted to explore the flanks of this newly discovered intrusion.
A 0.5 mGal gravimetric Bouguer anomaly was detected and investigated by drilling.
Cookie Policy
We use cookies to tailor your experience, measure site performance and market our products. By clicking ‘Allow’ or on any content on this site, you agree to our use of cookies as described here. You can read our Privacy Policies or change your cookie settings.