Government of Yukon data describes the geology of the Carpenter Creek and McKay Hill areas, straddling the Paleozoic basin-platform transition coincident with the Dawson thrust. The description details Proterozoic and Paleozoic rock groups, unconformities, and structural features. Ag-Pb-Zn ± Au and Au-Ag-Cu-Pb mineralization is noted near Grey Copper Hill and McKay Hill, spatially associated with geological structures.
Use Cases
- Mapping geological structures based on descriptions of thrust faults, unconformities, and folds.
- Identifying potential mineral exploration targets based on described Ag-Pb-Zn ± Au and Au-Ag-Cu-Pb mineralization.
- Studying stratigraphic relationships based on described Proterozoic and Paleozoic rock groups and their separations.
- Analyzing the spatial association of mineralization with specific geological features like strike-slip faults.
Strengths
- Data is provided by the authoritative Government of Yukon.
- Description provides specific geological context including named formations (e.g., Gillespie Lake Group, Bouvette Formation) and structural features.
- Mineralization types (Ag-Pb-Zn ± Au, Au-Ag-Cu-Pb) and their spatial associations are explicitly mentioned.
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 the specific mapped area in Yukon.
Provenance
- Source
- Government of Yukon
- Freshness
- Last updated 2026-04-17 15:57:47.873972; freshness should be verified.
- Geography
- Carpenter Creek and McKay Hill areas (NTS 106D/6, 11), central Yukon