Sedimentology, stratigraphy and depositional history of the Falher F conglomerate trend, Alberta, Canada
Detailed sequence stratigraphic analyses indicate that the lower Cretaceous Falher F unit is made up of 4 sandy/pebbly prograding parasequences labeled F1, F2, F3, and F4. Of the parasequences only F3 has a significant (>2m) thickness of conglomerate. Vertical lithological successions through...
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| Format: | Others |
| Language: | en |
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McGill University
2004
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| Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=81368 |