Finlayson Lake District Mineralization Faults and Host Rock Characteristics

The Finlayson Lake district in southeastern Yukon hosts volcanogenic massive sulphide deposits. The dataset likely contains geological observations and interpretations regarding syn-mineralization faults and host rock characteristics near deposits like Fyre Lake and Kudz Ze Kayah. It was published by the Government of Yukon and last updated on April 17, 2026.

Use Cases

• Mapping prospective zones for massive sulphide deposits based on inferred syn-mineralization fault corridors.
• Analyzing the relationship between deposit location and changes in host rock thickness and type.
• Studying structural re-activation, such as the Money Creek thrust, as a control on mineralization.
• Correlating deposit distribution with north-northwest-striking structural trends in the district.

Strengths

• Focuses on a specific, well-defined geological district: the Finlayson Lake district in southeastern Yukon.
• Includes interpretations for multiple properties (Fyre Lake, Hat Trick, Campbell Range) and structural features (Money Creek thrust).
• Last updated date is precisely recorded: 2026-04-17 15:44:03.052212.

Limitations

• Row count and dataset size are unknown, which may limit suitability assessment.
• Column-level documentation is absent; field semantics must be inferred after download.
• Data may reflect geographic bias inherent to the specific study area.

Provenance

Source

Government of Yukon

Freshness

Last updated 2026-04-17 15:44:03.052212; freshness should be verified.

Geography

Finlayson Lake massive sulphide district, Yukon-Tanana Terrane, southeastern Yukon, Canada