The geology of the Fraser Valley between Hope and Emory Creek, British Columbia
The Fraser Valley from Hope to Emory Creek is underlain by mainly regionally metamorphosed Palaeozoic and (?) Mesozoic sedimentary and volcanic rocks. The Chilliwack group consists of iron- and magnesium-rich pelitic schists and minor basic schists of the staurolite-quartz subfacies and to a lesser...
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| Language: | English |
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University of British Columbia
2011
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| Online Access: | http://hdl.handle.net/2429/39566 |