Geology and Asbestos Mineralization of the Clinton Creek Deposit

A geological thesis details the Clinton Creek asbestos deposit in Yukon, analyzing its formation within the Yukon Metamorphic Complex. The study delineates three phases of deformation and links chrysotile-fibre mineralization to late Cretaceous intrusive activity. The author is unknown, and the data is presented in an HTML document.

Use Cases

• Analyze the relationship between chrysotile-fibre occurrence and the contact of argillite and other geological units.
• Study the three prominent phases of deformation, including the Permian phase associated with initial Tintina fault movement.
• Model the proposed formation of chrysotile-fibre as fracture filling linked to late Cretaceous acid intrusive rocks.
• Examine the structural trends of folds and their changes in direction relative to the Tintina Trench.

Strengths

• Provides a detailed geological analysis of a specific asbestos deposit, including formation hypotheses.
• Identifies three distinct phases of deformation with associated structural characteristics.
• Links mineralization events to specific geological time periods, such as the Permian and late Cretaceous.

Limitations

• Data is presented as a descriptive thesis without structured tabular data or quantified measurements.
• Sample data, row counts, and column definitions are unavailable for computational analysis.
• The focus is on a single deposit, limiting broader regional comparative analysis.

Provenance

Source

Government of Yukon

Collection Method

Geological thesis research

Time Range

Covers geological events from Ordovician-Devonian to Cretaceous-Tertiary periods.

Freshness

null

Geography

Clinton Creek asbestos deposit, 77 km northwest of Dawson City, Yukon Territory, Canada.