Aurania Reports Initial Findings From IP Survey at Kuri-Yawi

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Toronto, Ontario--(Newsfile Corp. - February 20, 2025) - Aurania Resources Ltd. (TSXV: ARU) (OTCQB: AUIAF) (FSE: 20Q) ("Aurania" or the "Company") reports that the induced polarization (IP) geophysical survey has provided invaluable information that will assist in defining the location of future drill holes at the Kuri-Yawi gold target in Ecuador. Kuri-Yawi is a geochemical anomaly with enrichments in epithermal pathfinder elements. In addition, large pieces of siliceous sinter in float were recovered from the grid signifying the presence of an extinct geothermal system. The Fruta del Norte gold deposit some 100 km to the south lies beneath a siliceous sinter unit.

The IP survey detected conductive and chargeability anomalies at the Kuri-Yawi epithermal gold target. Chargeability (or induced polarization) is a measure of the ability of the rock to temporarily retain an induced electrical charge, usually due to disseminated sulphides

Our geologists are now working to interpret the IP survey results in relation to and compared to existing field data and data from the previous Mobile MagnetoTellurics (MobileMT) airborne survey to define optimal drill hole positions. A start date for a proposed drill program at Kuri-Yawi has not yet been determined.

The IP survey at Kuri-Yawi was conducted by GexplOre in late 2024 using the Fullwaver system (from Iris Instruments). The Fullwaver is a distributed acquisition system with each system being fully independent of the other. This drastically reduces the need for cables making it optimal for challenging terrain.

Two different methods were deployed during the geophysical survey:

  • Pseudo-3D profiling using 2D DC electrical methods in Pole-dipole configuration with simultaneous measurement of apparent resistivity (ρa) and induced polarization (IP) along eleven profiles, each of 2700 m length; and

  • 3D DC electrical methods over a selected area with simultaneous measurement of apparent resistivity (ρa) and induced polarization (IP) along two grids (0.6 km²).

The collected data was processed and inverted to generate a 3D model of the ground's resistivity and chargeability.

Resistivity and Conductivity

  • The resistivity results highlight the different lithologic units with a conductive sedimentary unit to the east and a resistive volcanic unit overlying another conductive unit at depth that could correspond to an alternation of black shale, limestone and volcanic tuff. These facies are known further to the north and are suspected to be a good trap for gold mineralisation. The conductive unit at surface may correspond to the tropically weathered clay level.

  • In the southeastern area, conductive vertical structures are locally present and remain relatively consistently sub-perpendicular along the lines, forming a large vertical conductive corridor. The direction of this corridor is similar to the direction of the chalcedony veins with high grade thallium that was discovered while walking the cut lines on the survey grid.