Mesothermal Gold-Quartz Vein Fluid Inclusion and Isotope Study in Yukon Klondike Schists

A geological study analyzes fluid inclusions and stable isotopes in mesothermal gold-quartz veins within the Klondike Schists of Yukon Territory. The research describes and examines the geology of these gold-bearing quartz veins.

Use Cases

• Analyze fluid inclusion data to model hydrothermal conditions during gold-quartz vein formation.
• Use stable isotope measurements to trace fluid sources and mineralization processes.
• Correlate geological descriptions of quartz veins with regional gold ore distribution patterns.

Strengths

• Study focuses on a specific, economically significant geological setting in the Yukon Klondike Schists.
• Data includes specialized geochemical analysis from fluid inclusions and stable isotopes.
• Provided by the Government of Yukon, indicating an authoritative source for regional geology.

Limitations

• Data format is HTML, which is not structured for direct quantitative analysis without extraction.
• Sample data and column definitions are unavailable, limiting immediate analytical use.
• The dataset scope is a single study, not a time-series or multi-location compilation.

Provenance

Source

Government of Yukon

Collection Method

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Time Range

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Freshness

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Geography

Klondike Schists, Yukon Territory, Canada