Origins of replacement dolomites, Upper Devonian Leduc, Nisku and Wabamun formations, southeastern Alberta western Canada sedimentary basin
The Upper Devonian Leduc, Nisku and Wabamun/Stettler formations (Frasnian and Famennian) were deposited on extensive carbonate platforms, and form three unconformity bounded megasequences, characterized by stacked shallowing upward meter to tens of meter-scale paracycles. Carbonates interbedded with...
| Main Author: | |
|---|---|
| Other Authors: | |
| Format: | Others |
| Language: | en |
| Published: |
McGill University
1998
|
| Subjects: | |
| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=35634 |