Blue Lagoon Resources Inc.
Is awarded the 2026 Sustainability Award by PDAC for its Dome Mountain Au-Ag Project, Smithers, BC, Lake Babine
Copper Quest Exploration Inc.
Completes and AI-driven geological analysis of the Kitimat Cu-Au Project, Kitimat, BC
Note:
'Confirming a large conductive anomaly consistent with a buried porphyry center' lacks drilling. 'Very large', 'significant', and 'near-surface' lack metrics. 'Open' lacks geological context. Kitimat intervals lack 'from' distances. The figure indicates that the Jeanette Zone is a low-sulfidation deposit model. Core size, sample length, true width, collar table, prep & assay method, generative AI probabilities, and a QA/QC description are missing. Intervals lack Maximum Internal Dilution and minimum grade.
The AI modelled a 1.5 km x 1.5 km conductive body extending 1 km vertically by integrating historical drilling, airborne magnetics, VTEM conductivity, geological mapping, structural data, and soil/rock geochemistry into a probabilistic 3D framework. It evaluated thousands of subsurface scenarios to rank probability clusters for concealed intrusive centres and sulfide-rich alteration zones.
Key Technical Risks:
Interpretive Offset Risk - Hanson (2020 NI 43-101) describes the Jeannette Zone as phyllic (silica-sericite-pyrite) alteration with quartz-pyrite-chalcopyrite and Cu-Au grades (0.33–0.54% Cu and 0.41–1.03 g/t Au), fitting a peripheral porphyry or intermediate-sulfidation setting. The deposit model figure places it in a low-sulfidation epithermal zone. Linking it as 'peripheral' to a 1.5 km-scale AI conductor assumes precise EM inversion and a single large intrusive centre — rare in BC, where typical porphyry cores are ~300–900 m and larger footprints reflect porphyry clusters rather than a single body.
Non-Independent Inputs - VTEM, magnetics, drilling, mapping, and geochem often respond to the same geology, so combining them without new drilling risks amplifying signals into locally unvalidated 'high-probability' clusters.
Inversion Non-Uniqueness - Conductive and magnetic targets lack true volume and depth constraints due to inversion ambiguity (e.g., a small deep conductor mimics a large shallow one; VTEM depth resolution is limited to ~500 m). The 2010 IM-1 to IM-3 DDHs confirmed clay overburden — not sulfides — as the source of a strong VTEM anomaly east of the Jeannette Zone, with background Cu throughout (0.002–0.043%). Because the AI ingested the same VTEM dataset, the flagged conductor is unlikely to distinguish from a similar clay source without new drilling.
Model Limitations - The 1.5 km 'highest-probability' conductor is a statistical output, not drilled geology. It could be porphyry-related, a separate system, or non-economic — consistent with the clay and background geochemistry confirmed in the IM holes.
'Confirming a large conductive anomaly consistent with a buried porphyry center' lacks drilling. 'Very large', 'significant', and 'near-surface' lack metrics. 'Open' lacks geological context. Kitimat intervals lack 'from' distances. The figure indicates that the Jeanette Zone is a low-sulfidation deposit model. Core size, sample length, true width, collar table, prep & assay method, generative AI probabilities, and a QA/QC description are missing. Intervals lack Maximum Internal Dilution and minimum grade.
The AI modelled a 1.5 km x 1.5 km conductive body extending 1 km vertically by integrating historical drilling, airborne magnetics, VTEM conductivity, geological mapping, structural data, and soil/rock geochemistry into a probabilistic 3D framework. It evaluated thousands of subsurface scenarios to rank probability clusters for concealed intrusive centres and sulfide-rich alteration zones.
Key Technical Risks:
Interpretive Offset Risk - Hanson (2020 NI 43-101) describes the Jeannette Zone as phyllic (silica-sericite-pyrite) alteration with quartz-pyrite-chalcopyrite and Cu-Au grades (0.33–0.54% Cu and 0.41–1.03 g/t Au), fitting a peripheral porphyry or intermediate-sulfidation setting. The deposit model figure places it in a low-sulfidation epithermal zone. Linking it as 'peripheral' to a 1.5 km-scale AI conductor assumes precise EM inversion and a single large intrusive centre — rare in BC, where typical porphyry cores are ~300–900 m and larger footprints reflect porphyry clusters rather than a single body.
Non-Independent Inputs - VTEM, magnetics, drilling, mapping, and geochem often respond to the same geology, so combining them without new drilling risks amplifying signals into locally unvalidated 'high-probability' clusters.
Inversion Non-Uniqueness - Conductive and magnetic targets lack true volume and depth constraints due to inversion ambiguity (e.g., a small deep conductor mimics a large shallow one; VTEM depth resolution is limited to ~500 m). The 2010 IM-1 to IM-3 DDHs confirmed clay overburden — not sulfides — as the source of a strong VTEM anomaly east of the Jeannette Zone, with background Cu throughout (0.002–0.043%). Because the AI ingested the same VTEM dataset, the flagged conductor is unlikely to distinguish from a similar clay source without new drilling.
Model Limitations - The 1.5 km 'highest-probability' conductor is a statistical output, not drilled geology. It could be porphyry-related, a separate system, or non-economic — consistent with the clay and background geochemistry confirmed in the IM holes.