The geology of part of the Shulaps ultramafite, near Jim Creek, southwestern British Columbia
The Shulaps ultramafite lies at the eastern edge of the Coast Plutonic Complex approximately 150 miles from Vancouver, B.C. It is one of the largest "alpine-type" peridotites in British Columbia, consisting primarily of harzburgite and subordinate dunite lying in an elongate zone trending...
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| Language: | English |
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2010
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| Online Access: | http://hdl.handle.net/2429/21425 |