Minaurum Gold Inc. 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 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. 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. Lower Cretaceous limestone is the oldest geological unit known at the Alamos project, stratigraphically underling the Tertiary andesitic volcanic rocks that are the principal epithermal vein hosts. Limestone crops out extensively on the property in fault-bounded blocks, and drilling has revealed considerable thicknesses of limestone under the volcanics.

The limestone is folded, so thickness ranges from a few tens of metres to an estimated 400 metres. The district was intruded by Laramide granodiorite and granite, so the limestone is nearly always strongly recrystallized. In many areas, particularly those adjacent to the Promontorio and Alessandra vein zones, it is skarn altered and mineralized, suggesting blind CRD mineralization may be more widely developed throughout the district.