Minaurum Discovers Zinc-Rich Carbonate-Replacement (CRD) Mineralization at Alamos

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Vancouver, British Columbia--(Newsfile Corp. - April 25, 2024) - Minaurum Gold Inc. (TSXV: MGG) (OTCQX: MMRGF) ("Minaurum" or "Company") is pleased to report the discovery of Zinc-rich carbonate-replacement ("CRD")/skarn mineralization associated with the Promontorio and Promontorio Sur epithermal silver-zinc-lead-copper-gold veins at its 100%-owned, fully production-permitted Alamos Silver Project ("Alamos") in the State of Sonora, Mexico.

Relogging of existing drill core with a focus on Strategic Metals outlined a continuous 2.4 km-long zone of Zinc-rich CRD-style mineralization and skarn alteration developed in recrystallized limestone beneath high-grade silver veins in the Promontorio and Promontorio Sur zones. The CRD mineralization was never targeted but was cut coincidentally at the bottom of several holes. Drill holes with the strongest CRD mineralization include:

  • Hole AL19-020: 3.21% Zn and 1.05% Pb over 3.0 m

  • Hole AL19-024 (800 m southwest of AL19-020): 1.73% Zn and 3.98% Pb over 0.20 m

  • Hole AL19-025 (250 m northeast of AL19-020): 2.18% Zn and 0.62% Pb over 7.75 m

"Recognizing that Alamos hosts CRD mineralization in addition to our existing high-grade silver veins, creates a significant new target for us," stated Darrell Rader, President and CEO of Minaurum Gold. "While carbonate rocks are known throughout the project area, CRD mineralization has never been directly targeted. We're especially excited by what's been found so far because it lies immediately adjacent to the Promontorio where we hope to block out a resource. We are adding these CRD targets to our upcoming drill program slated to start as soon as we complete the current financing."

"Many of Mexico's biggest epithermal vein camps, including Fresnillo and Santa Barbara, show extensive development of zinc-lead-silver CRD and skarn mineralization where the veins cross limestone. In most cases these manifest as relatively flat-lying sheets (mantos) of massive sulphides that locally sprout off the veins," said Dr. Peter Megaw, co-founder and advisor to Minaurum. "We have strong indications of this along nearly 2.5 km of some of the district's main veins. These represent great places to start applying modern CRD exploration approaches to this system."

CRD mineralization cut so far at Alamos is characterized by zinc and lead sulfides that replace recrystallized limestone in the footwall of the Promontorio and Promontorio Sur vein zones (Figure 1). These veins are emplaced along and parallel to north-northeast faults that juxtapose andesitic agglomerate, recrystallized limestone, and granodiorite. Intersections of this footwall carbonate-replacement mineralization were reported along with vein mineralization in Minaurum Gold's news release dated August 22, 2019 (Table 1), but not pursued due to the company's focus on silver and gold.