Age and origin of the Turnagain Alaskan-type intrusion and associated Ni-sulphide mineralization, north-central British Columbia, Canada
The Turnagain Alaskan-type intrusion in north-central British Columbia consists of ultramafic to dioritic rocks and contains significant magmatic sulphide mineralization. The age of the intrusion is constrained by U-Pb and Ar-Ar geochronology to be 190±1 Ma and the minimum depositional age of the yo...
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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/2429/32512 |