Diagenesis of middle devonian presqu'ile dolomite pine point NWT and adjacent subsurface
Four types of dolomites occur in the Middle Devonian Presqu'ile barrier: fine-crystalline, medium-crystalline, coarse-crystalline, and saddle. Fine-crystalline dolomite formed penecontemporaneously by Middle Devonian seawater, because it is interbedded with Muskeg anhydrite in the back-barrier...
| Main Author: | |
|---|---|
| Format: | Others |
| Language: | en |
| Published: |
McGill University
1991
|
| Subjects: | |
| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=70187 |