Nicola Mining Announces The Completion Of The Ubc Master’s Thesis Concluding That Craigmont Is Part Of A Porphyry-Linked Skarn System
Executive Summary
The study employed advanced analytical techniques including field observations, petrography, whole-rock and mineral chemistry, and integrated geochronology to redefine Craigmont's geological model. Key findings include identification of two discrete hydrothermal stages: massive calcsilicate skarn alteration at approximately 215 million years ago related to early Border Phase intrusions, and overprinting vein-hosted porphyry-type mineralization at 209 million years ago from later oxidized intrusions. The presence of multiple alteration styles and elevated porphyry indicator trace elements in epidote minerals provides strong evidence for a proximal porphyry system separate from the Highland Valley district.
The research has immediate practical applications for Nicola's exploration strategy, narrowing focus to two primary target areas: West Craigmont containing the Draken target, and east of the historical mine where the Jotun target is located. The study emphasizes the importance of structural permeability and reactive host rocks in controlling mineralization distribution, providing valuable vectoring tools for the company's ongoing exploration efforts.
This academic validation carries significant strategic value for Nicola Mining, particularly given the project's location within the same Guichon Batholith that hosts Highland Valley Copper, Canada's largest copper mine. The confirmation of a separate porphyry center at New Craigmont, supported by rigorous scientific methodology and peer review through UBC's respected MRDU program, strengthens the geological case for the 10,800-hectare property. With the company preparing to launch its 2026 exploration program, this research provides both technical direction and increased confidence in the project's potential to host significant porphyry-style copper mineralization.
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