Geology and metamorphism of the Yale Creek area, B.C.
The Yale Creek area is underlain by the pelitic Settler Schist, Spuzzum hornblende quartz diorites, and minor gneiss and granodiorite. Mineral textures in the schists define three phases of folding. The structural geology is dominated by the second phase, f₂, characterized by northwest plunging isoc...
| Main Author: | |
|---|---|
| Language: | English |
| Published: |
2010
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/2429/21492 |