Aztec Identifies High Priority Carbonate Replacement Targets (CRD) at Tombstone Project, Arizona

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VANCOUVER, BRITISH COLUMBIA - March 20, 2025 (NEWMEDIAWIRE) - Aztec Minerals Corp. (AZT: TSX-V, OTCQB: AZZTF) ("Aztec" or the "Company") announces that recent drilling and 3D data modelling at the Tombstone Property in Southeastern Arizona, USA has generated an enhanced understanding of potential CRD mineralization below the near-surface gold-silver oxide mineralization discovery zone. Aztec has previously identified several large, strong, conductive bodies, underneath the historic gold-silver district through NSAMT (natural-source audio-frequency magneto-telluric surveys) anomalies(1). Aztec has now integrated recent drilling and 3D modelling exploration data with the NSAMT geophysics data producing several high-priority drill-ready CRD targets at the property.

The 2024 exploration program has developed a stronger understanding of the district's CRD potential and has substantiated the 2020 geophysical NSAMT survey identification of anomalous conductivity as possible mineralization at depth in the southern portion of the project (see Figure 1)(1). The geologic modelling for the Westside zone was successful with blind targeting and confirmed the historic reporting of underground mine workings as well as Aztec's modelling. The Westside zone's first pass exploration drilling program encountered oxide silver-gold mineralization in every drillhole to-date and nearly doubled the area of drill demonstrated exploration potential from the Contention zone alone.

The Tombstone gold-silver district was historically focused on mining relatively shallow, oxidized silver-gold CRD-related deposits formed in a complex structural and intrusive environment. The structural complex underlying the district is the same Paleozoic limestone sequence that hosts the massive Taylor CRD zinc-silver-lead deposit of South32 located only 65 kilometers west of Tombstone and the extensive Bisbee CRD and skarn copper-gold-zinc-silver-lead deposits 39 kilometers to the south*.

Tombstone shares many similarities with the two neighboring major CRD deposits, Hermosa-Taylor and Bisbee in alteration zoning, mineralization, host rocks, and trace element relationships. Positive indications for deeper, underground CRD mineralization at Tombstone include:

  1. The Bisbee sediments exhibit widespread fracturing, silica-pyrite-sericite-clay alteration, oxidation and incipient hornfels, and in the limey sediments, skarn development

  2. The Contention open pit mine is centered along a strong NNE fault structure with large, mineralized felsic dikes possibly related to a deeper intrusion

  3. Multistage mesothermal mineralization

  4. The underground Contention mine mined the mineralization to over 300m depth

  5. Historic drilling by Newmont and Santa Fe to over 700 m depth intersected narrow to wide, high grade CRD mantos, evidence that the Paleozoic limestones are prospective

  6. The presence of several manganese-silver rich mines that surround the Property are considered indicative of distal mineralization to CRD deposits worldwide

  7. One of the strongest indicators for such a deposit is the natural source vector AMT geophysical study Aztec contracted from Zonge in 2020 that found significant anomalies at depth in the center and south of the project (Figure 1)(1). Zonge interpreted the main anomaly to be a "Moderate to strong conductor, stratabound and below Historic underground workings"

  8. (Southern Contention pit). The term stratabound suggests CRD-type mineralization could be present in the conductive anomaly.