Alteration and infiltration : documenting controls on skarn formation at Mineral Hill, Sechelt, southwestern British Columbia
The Mineral Hill wollastonite deposit is hosted by a north-west trending calcareous roof pendant enclosed within Late Jurassic plutons of the southwestern Coast Plutonic Complex. The study area consists of calcite marble, other meta-sediments and skarn in contact with a dioritic component of the...
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| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/2429/11945 |