Paleotectonic setting of Takla Group volcano-sedimentary rocks Quesnellia, North Central British Columbia
Upper Triassic Takla Group rocks occur in Quesnellia and Stikinia, two allochthonous terranes of the Canadian Cordillera. The terranes are separated by the major, north-northwest trending, dextral transcurrent Findlay fault. The stratigraphy of the study area, east of the fault in Quesnellia, is com...
| Main Author: | |
|---|---|
| Format: | Others |
| Language: | en |
| Published: |
McGill University
1989
|
| Subjects: | |
| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59412 |