Carboniferous Fluvial Strata of the Inverness Formation at Finlay Point, Southwest Cape Breton Island.
A red bed unit of Westphalian C age at Finlay Point, Mabou Mines, Inverness County, Nova Scotia occurs stratigraphically near the base of the Inverness Formation and is correlated with offshore coal seams in the St. Lawrence Basin. A succession of sandstone and mudstone facies compose the measured s...
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| Format: | Report |
| Language: | unknown |
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2021
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| Online Access: | http://hdl.handle.net/10222/80392 |