Southern Campbell Range Geological Map with Fold and Fault Interpretations

Government of Yukon's schematic map details fold styles and fault reactivation in southeastern Yukon. Metasomatic replacement of chert conglomerate by tremolite is documented over a 5-meter interval. The dataset was last updated on April 17, 2026.

Use Cases

• Analyze fold geometry and style based on schematic interpretations from outcrop and thin section.
• Study fault reactivation history based on descriptions of the Jules Creek fault's Permian and Jurassic motion.
• Model metasomatic processes based on documented replacement intervals and rock sequences like serpentinite to nephrite.
• Map lithological contacts and sequences based on described rock units from bottom to top across a metasomatic zone.

Strengths

• Includes specific geological interpretations, such as a 5-meter interval of tremolite replacement.
• References peer-reviewed literature (Murphy, 2004) for fault timing.
• Provides detailed rock sequences across a metasomatic contact.

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 study area in the Yukon.

Provenance

Source

Government of Yukon

Collection Method

Interpreted from fold geometry in outcrop and thin section.

Freshness

Last updated 2026-04-17 15:54:34.100005; freshness should be verified.

Geography

Southern Campbell Range (NTS 105H/3 SW), southeastern Yukon, Canada.