Coppernico Metals Inc. (TSX: COPR, OTCQB: CPPMF, FSE: 9I3) has provided an exploration update on the Tipicancha epithermal-porphyry copper-gold target at its Sombrero Project in Peru. Geological mapping has defined a large hydrothermal alteration footprint containing locally developed advanced argillic cores, now extending over more than four kilometers. This is consistent with a district-scale hydrothermal framework that suggests potential for a porphyry-related source at depth.
Exploration Update Highlights
Shallow excavation sampling has confirmed near-surface copper enrichment and further refined the continuity of the sulfide-rich hydrothermal horizon. Ongoing mapping increasingly defines vertical and lateral alteration zonation and structural controls, which will inform the upcoming drill program.
Hydrothermal Footprint Expansion and Definition
Systematic mapping is materially refining the scale, geometry, and structural framework of the Tipicancha hydrothermal footprint, now interpreted to extend over more than 4 km in length.
Continuous Pyrite Horizon and Copper Enrichment Confirmed
Shallow excavation sampling has further defined continuity of a laterally extensive pyrite-rich hydrothermal horizon and confirmed localized copper enrichment within mixed oxide-sulfide zones.
Geochemistry Supports Potential Porphyry Mineralization at Depth
Multi-element geochemistry (Cu-Mo-Se-S) and pathfinder enrichment characteristic of high-sulfidation environments continue to support the interpretation of a vertically zoned magmatic-hydrothermal system with potential for deeper porphyry-related mineralization.
Structural Corridors Provide Drill Targeting Vectors
Structural interpretation identifies ENE-WSW corridors and intersecting NNE-trending structures that appear to focus alteration, sulfide development, and copper enrichment, providing explicit vectors for initial drill targeting.
Ivan Bebek, Chair and CEO of Coppernico, commented: “The partially outcropping Tipicancha target is emerging as one of our most compelling exploration targets at Sombrero, which we plan to drill test in the coming months. The strong correlation between surface sampling in areas of limited bedrock exposure, recent geophysical studies, and these latest results continues to strengthen our confidence in the near-surface continuity of the pyrite-copper horizon.”
For the purposes of this news release, Coppernico uses “lithocap” to describe the broad contiguous footprint of strongly hydrothermally altered volcanic rocks at Tipicancha, characterized by pervasive argillic alteration and locally developed zones of silicification, residual silica, pyrite enrichment, and higher-temperature advanced argillic assemblages. Advanced argillic alteration refers here to acid-sulfate assemblages including quartz–alunite (Na- and K-bearing), quartz–kaolinite ± plagioclase, abundant pyrite, locally developed residual to vuggy silica, and locally associated native sulfur. Surface mineral assemblages may locally reflect oxidation and supergene overprint of earlier hydrothermal assemblages.
