Lithofacies of the Lower Paleozoic Carbonate Shelf to Basin Facies Transition, West-Central Ellesmere Island, Canadian Arctic
The Upper Ordovician (Ashgillian) to Middle Silurian (Wenlockian) graptolitic carbonates and cherts of the Cape Phillips Formation accumulated in the deep water basinal environment of the Hazen Trough. The coeval platform carbonates of the Allen Bay Formation to the east in a shelf environment. Nine...
| Main Author: | |
|---|---|
| Format: | Report |
| Language: | unknown |
| Published: |
2021
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/10222/81030 |