Geology of the Deer Horn prospect, Omineca M.D., British Columbia
The Deer Horn property lies astride the contact of the Coast Range batholith and a group of siliceous and shaly sediments of Jurassic or Lower Cretaceous age. The contact strikes westerly and dips about 50° to the South. The southern three fifths of the property are underlain by granitic rocks, the...
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| Language: | English |
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University of British Columbia
2012
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| Online Access: | http://hdl.handle.net/2429/40236 |