Latest Proterozoic to Earliest Cambrian and Devonian to Mississippian strata underlie the Plata-Inca property. The sedimentary rocks are folded and cut by thrust faults and younger normal faults, which host veins containing galena, sphalerite, and tetrahedrite. Silver-lead ratios from ore shipments range from 55.5 g/t Ag : 1% Pb to 137.1 g/t Ag : 1% Pb.
Use Cases
- Analyze structural controls on mineralization based on descriptions of thrust faults and normal faults.
- Model silver-lead ratios based on reported ore shipment grade ranges.
- Study mineral assemblages in veins based on listed minerals galena, sphalerite, and tetrahedrite.
- Investigate geological context based on described strata and intrusions.
- Map potential mineralization zones based on fault-hosted vein descriptions.
Strengths
- Specific silver-lead ratios are provided, ranging from 55.5 g/t Ag : 1% Pb to 137.1 g/t Ag : 1% Pb.
- Detailed geological context includes descriptions of strata, faults, and mineral assemblages.
- Source is the Government of Yukon, suggesting authoritative origin.
Limitations
- Column-level documentation is absent; field semantics must be inferred after download.
- Row count is unknown, which may limit suitability assessment.
- Data may reflect geographic bias inherent to a single property study.
Provenance
- Source
- Government of Yukon | Gouvernement du Yukon
- Freshness
- Last updated 2026-04-17 16:04:48.804908; freshness should be verified.
- Geography
- Plata-Inca property, Yukon, northern Cordilleran miogeocline