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Almaden Minerals Ltd.

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Summary

Project:

Tuligtic

Deposit:Ixtaca
Location:Mexico
Commodities:Gold-Silver
Date:7/18/2017
Report Code:NI43-101
Report Type:Exploration/Drilling Update
Project Stage:Pursuing Feasibility Study
Report details:18-7-2017: Almaden Minerals Ltd. announces an Exploration/Drilling Update report for its Ixtaca deposit at the Tuligtic project. Drilling results incl. 118.50m @ 0.22g/t Au, 125.1g/t Ag from 86.50m. Almaden Minerals Ltd. ( Almaden or the Company; AMM: TS
Resources:(not mentioned in this report)
CP/QP:[Overall Report]: Norm Dircks (Internal)
ABSTRACT:Almaden Minerals Ltd. ( Almaden or the Company; AMM: TSX; AAU: NYSE MKT) is pleased to announce new assay results from Almaden s ongoing exploration and development program at the Company s Tuligtic project, Mexico. Results reported today are from drill holes TU-17-494, 495, 496 and 497 drilled on sections 10+500 and 10+775 East. Holes TU-17-494, 495 and 496 intersected significant mineralisation and veining inside or immediately outside of the 2017 PFS pit north of the Main Ixtaca Zone. Hole TU-17-497 expanded the Main Ixtaca Zone to depth. Highlights from these drillholes include the following intercepts: The mineralisation reported today confirms the presence of additional important zones of veining immediately adjacent to the Main Ixtaca Zone and points to the exploration potential of the project in general. The Ixtaca deposit was discovered in 2010 beneath a large area of largely barren clay alteration which has been confirmed subsequently to represent the upper portions of a gold and silver bearing epithermal vein system. Since the discovery Almaden has focussed its efforts on the development of the Ixtaca Zone, however today s results clearly show the potential for additional mineralisation, not only proximal to the deposit, but more broadly project wide beneath the high level clay alteration. J.D. Poliquin, chairman of Almaden stated, When low sulphidation epithermal precious metal deposits are formed, metal bearing fluid rises from depth, filling fractures with quartz, calcite and precious metal minerals. In the highest mineralised areas of the system, the same fluids can be dispersed through multiple smaller fractures to form a sheeted vein zone or swarm such as we have at the Main Ixtaca Zone.

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