Hannan Discovers 2.4 km Long Geophysical IP Anomaly at the Vista Alegre Epithermal Prospect at Valiente, Peru

In This Article:

VANCOUVER, BC / ACCESSWIRE / December 5, 2024 / Hannan Metals Limited ("Hannan" or the "Company") (TSXV:HAN)(OTC PINK:HANNF) is pleased to report the identification of a significant IP anomaly at the Vista Alegre epithermal prospect within the Company's 100%-owned Valiente copper-gold project in Peru (Figure 1).

Highlights:

  • Broadly, two distinct types of anomalies were identified in the IP geophysical survey (Figures 2 to 7):

    • High chargeability - low resistivity zone over 2.4 km strike and up to 500 m deep coinciding with up to 0.23 ppm gold in soils (Figures 3 to 7) suggesting mineralization is associated with sulphide assemblages and argillic clay alteration;

    • High chargeability - high resistivity zones over 1 km strike coinciding with mineralized silicified boulders containing white milky quartz, arsenopyrite, chalcopyrite and pyrite assaying up to 1.98 g/t Au and 29 g/t Ag. (reported here) (Figures 3 to 7) suggesting epithermal-style mineralization associated with strongly silicified structures.

  • The target is drill-ready with 12 platforms approved as part of the recently granted DIA permit (reported here).

  • Drilling is anticipated to commence in Q2 2025.

Michael Hudson, CEO, states: "The identification of large scale and coherent IP geophysical anomaly at Vista Alegre represents another significant milestone in the development of the Valiente Project. The correlation between the geophysical anomaly, surface mineralization, and soil geochemistry provides us with compelling and de-risked drill targets. With our recently approved DIA permit including 12 drill platforms at Vista Alegre, we are well-positioned to test this extensive epithermal system in Q2 2025."

Geophysical Interpretation

Vista Alegre represents a significant epithermal target controlled by a prominent northwest-trending thrust fault that juxtaposes sedimentary sequences against phaneritic intrusive rocks. This structural corridor has been intruded by later-stage porphyritic intrusions and small massive to semi-massive magnetite bodies.

The integration of induced polarization (IP), resistivity, high-resolution aeromagnetic data (Figure 2), and surface geochemistry (Figure 3) has identified a substantial anomaly coincident with the thrust zone. Analysis of horizontal depth slices through the 3D IP inversion model (Figures 4 to 7) reveals multiple target types with distinct geophysical signatures correlating with surface geochemical anomalies up to 500 m below surface:

  1. High chargeability - low resistivity zone over 2.3 km strike coinciding with up to 0.23 ppm gold in soils (Figures 3 to 7) suggesting mineralization is associated with sulphide assemblages and argillic clay alteration. No surface outcrops are present, although gold soil values are higher, especially in the northern sector. The structure dips southwest at approximately 60 degrees with some chargeable highs located on thrust bends, which may potentially be significant.

  2. High chargeability - high resistivity zones over 1 km strike coinciding with mineralized silicified boulders containing white milky quartz, arsenopyrite, chalcopyrite and pyrite assaying up to 1.98 g/t Au and 29 g/t Ag. (reported here) (Figures 3 to 7) suggesting mineralization of epithermal character associated with strongly silicified structures.