CopAur Minerals Inc. announced new drill targets generated from the recently completed induced polarization (IP) /resistivity geophysical surveying at the Company's Kinsley Mountain Gold Project (the "Kinsley Mountain Project" or "Kinsley Mountain") in Elko County, Nevada. In total, 80 line-km of geophysical surveys have been completed at Kinsley, over a 9 km north-south strike length, covering an area of approximately 30 km. Interpretation of the survey data has identified a minimum of eight untested high-priority targets at Kinsley North.

The final phase of IP/resistivity surveying announced here specifically targeted the frontier Kinsley North Range, which contains a significant strike length of prospective,faulted Pogonip Group and upper Notch Peak Formation carbonate rocks that are known to host significant gold mineralization at the Long Canyon Mine located 90 km north of Kinsley. The observed chargeability and resistivity anomalies indicate potentially significant fault displacement coincident with mapped faults, arsenic ± antimony ± gold in soil anomalies, and prospective known gold hosting rock units. New Drill Target Highlights: IP/resistivity survey defined 8 untested high-priority targets within 20 km2 underexplored area north of high-grade Western Flank gold deposit.

Kinsley North Range chargeability and/or resistivity anomalies: Are coincident with broad arsenic ± antimony ± gold in soil anomalies up to 1,000 by 500 metres in size, Indicate significant displacement along property-scale north to northwest-trending fault structures analogous to the Kinsley NW fault, a critical controlling structure of Western Flank Zone gold resources, Correlate with northeast to northwest-trending block faulting that exposes prospective lower Pogonip Group and upper Notch Peak Formation geology, known to host gold mineralization at Long Canyon, Associated with mapped jasperoid alteration. The Pogonip Group and upper Notch Peak Formation represent significant untested greenfield targets that are known to host gold-bearing systems elsewhere in Nevada, including at Long Canyon, and have not been tested to date at Kinsley. These rocks are exposed primarily in the under explored Kinsley North Range.

The Kinsley mineral resources are hosted stratigraphically lower, primarily within the Dunderberg Shale, Hamburg Formation, and Secret Canyon Shale units. The new geophysical anomalies, together with mapped fault structures and geochemic anomalies, provide compelling exploration targets within the stratigraphically higher Pogonip and Notch Peak units within the Kinsley North Range.