Geology of the Casino Copper-Molybdenum Deposit in Yukon
Updated 3mo ago
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Description
Yukon's Casino porphyry copper-molybdenum deposit in the Dawson Range is described with detailed geological features. The report details a concentrically zoned alteration pattern around a breccia pipe measuring approximately 2,000 by 1,200 feet at the surface. It was published by the Government of Yukon and discusses genesis models related to the Canadian Cordillera.
Use Cases
Analyze the spatial relationship between the breccia pipe dimensions and the concentric alteration zones for deposit modeling.
Study the distribution of chalcopyrite and molybdenite within the phyllic alteration zone for mineral exploration targeting.
Model supergene enrichment processes using described factors like original hypogene copper grade and pyrite presence.
Correlate potassic alteration facies core dimensions with underlying magmatic and tectonic models described in the report.
Strengths
Provides specific geological measurements, such as a breccia pipe surface area of 2,000 ft. by 1,200 ft.
Describes a detailed, concentric zonation of alteration facies with defined diameters, like a 1,500 ft. potassic core.
Includes a quantified factor for supergene enrichment, noting an average increase in copper grade by a factor of 1.7.
Limitations
Data is presented as a descriptive geological report in HTML format, not as a structured, queryable table.
Lacks numerical tabular data (rows/columns) for direct statistical or machine learning analysis.
The technical description is highly specialized, requiring expert domain knowledge in economic geology for interpretation.
Provenance
Source
Government of Yukon
Collection Method
null
Time Range
Discusses Mid-Cretaceous to Tertiary geological processes.