Palynologic zonation and correlation of the Peace River coalfield, northeastern British Columbia
The strata of the Peace River coalfield, in the Foothills of northeasten British Columbia, formed in a tectonically active region near the western margin of the craton. The complex pattern of intertonguing marine and non-marine strata which resulted was subsequently deformed by folding and thrusting...
| Main Author: | |
|---|---|
| Language: | English |
| Published: |
University of British Columbia
2010
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/2429/26173 |