District-Scale Exploration
The Hazelton property spans over 52,600 hectares in the Skeena Arch of northwestern British Columbia, a region known for its rich mineral endowment and mining history.
Our exploration has identified seven distinct target areas across the property, each with unique geological characteristics and mineral potential. From high-grade copper-gold porphyry systems to antimony-rich zones, the Hazelton property offers diverse exploration opportunities.
✔️ 52,600 Hectares
✔️ 7 Target Areas
✔️ 100% Ownership
✔️ High Grade Potential
Hazelton Property
Red Springs
Silver-antimony, gold breccia, and copper-molybdenum porphyry zones
Netalzul Mt.
Large scale Ag-Cu-Au-Zn-Pb-Sb veins andporphyry potential with mineralization system.
Blunt
Defined high grade silver-antimony project with Ag-Sb-Au-Pb-Zn 3km polymetallic vein.
Max
Massive sulphide Ag-Zn project with Sb-Au-Pb with drilled intersections 7 meters and property wide results.
Kispiox
Three high-grade antimony quartz vein zones (Up to 29.69% Sb) and property wide.
Advanced Exploration Techniques
Jaxon’s exploration strategy combines traditional field methods with modern technology to efficiently identify and advance high-potential targets.
- Geological Mapping: Detailed mapping to understand structural controls and mineralization patterns
- Geophysical Surveys: Advanced airborne and ground geophysics to identify subsurface anomalies
- Geochemical Analysis: Systematic soil and rock sampling to identify mineralization trends
- Diamond Drilling: Targeted drilling to test high-priority areas and expand known mineralization
Regional Geological Setting
Late Cretaceous to Eocene Magmatism, Tectonics, and Mineralization in the North Cordillera
The Netalzul Mountain project lies within British Columbia’s Skeena Arch, part of a broader metallogenic belt that experienced significant magmatic and tectonic activity between 75–60 Ma. During this period, magmatism migrated northeast into the Central Gneiss Belt and southwestern Alaska, associated with major fault systems like the Denali Fault (displaced >400 km).
This tectono-magmatic setting hosts several major deposits, including Donlin Creek, Pebble, Casino, and Coffee in Alaska and Yukon. In contrast, the Skeena Arch has seen only limited discovery, with smaller systems such as Glacier Gulch and Big Onion.
The Bulkley intrusive suite in the Netalzul area is thought to be geologically linked to the Yukon-Tanana belt. Recent deep drilling at Huckleberry Mine confirms the potential for deep-seated porphyry systems in the region. Netalzul Mountain shares key geological characteristics: age, lithology, structure, and alteration, with known porphyry systems and is considered a comparable exploration setting.
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