Since the acquisition of the Property in 2012, NexGen has systematically developed the property through numerous
geophysical surveys, including:
- Radiometric and VLF-EM (2013)
- VTEM (2014 and 2016)
- Airborne Gravity (2015 and 2016)
- ZTEM (2016 and 2018)
- HeliSAM (2018)
- HeliSAM (2018)
- HeliTEM (2019)
The geophysical surveys have defined numerous conductive corridors with gravity anomalies coincident with
breaks
in the conductors. Several of the conductors lie parallel or proximal to the Dufferin Lake Fault, a known
mineralized system that hosts Cameco’s Centennial Deposit. The geophysical signatures on the property and
interpreted structural kinematics of the Virgin River Shear Zone and Dufferin Lake Fault has highlighted
numerous prospective areas for uranium mineralization.