Magma genesis along an arc-transform transition zone
The Wrangell volcanic belt lies in a transpressional zone that results from the oblique convergence between the NE Pacific and North American plates. Transitional lavas predominate in the SE transform regime, whereas a calc-alkaline arc lies to the NW. The geochemical evolution of the St. Clare Cree...
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| Format: | Others |
| Language: | en |
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McGill University
1990
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| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=74677 |