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Skarn from
Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada


Locality type:Pluton
Classification
Type:Skarn
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Skarn data
Locality Data:Click here to view Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada
Data Identifiers
Mindat Occurrence Record ID:1620845
Long-form Identifier:1:3:1620845:4
GUID (UUID V4):0
Localities for Skarn in this Region
Bartnik deposit, Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada
Bril deposit, Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada
Cliff deposit, Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada
Glacier deposit, Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada
Nearest other occurrences of Skarn
2.3km (1.4 miles) ⓘGlacier deposit, Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada
2.5km (1.6 miles) ⓘCliff deposit, Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada
3.0km (1.9 miles) ⓘBartnik deposit, Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada
3.3km (2.0 miles) ⓘBril deposit, Zippa Mountain pluton, Liard Mining Division, British Columbia, Canada
16.5km (10.3 miles) ⓘBronson Skarn, Iskut River, Liard Mining Division, British Columbia, Canada
28.8km (17.9 miles) ⓘBurgundy prospect, Newmont Lake district, Liard Mining Division, British Columbia, Canada
53.2km (33.0 miles) ⓘMax (Maxwell Smart; Granduc Iron), Stewart, Skeena Mining Division, British Columbia, Canada
53.3km (33.1 miles) ⓘGalore Creek Cu-Au-Ag deposit, Galore Creek, Liard Mining Division, British Columbia, Canada
68.0km (42.2 miles) ⓘMitchell Cu-Au deposit, KSM project, Sulphurets District, Iskut River, Skeena Mining Division, British Columbia, Canada
References
Coulson, I. M., Westphal, M., Anderson, R. G., Kyser, T. K. (2007) Concomitant skarn and syenitic magma evolution at the margins of the Zippa Mountain pluton. Mineralogy and Petrology, 90 (3) 199-221 doi:10.1007/s00710-006-0178-9
 
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