Provenance of the Paleocene-Eocene Oyster Bay Formation, British Columbia

dc.contributor.authorMahoney, J. Brian
dc.contributor.authorWilliams, Jane B.
dc.date.accessioned2018-02-23T16:07:16Z
dc.date.available2018-02-23T16:07:16Z
dc.date.issued2018-02-23T16:07:16Z
dc.descriptionColor poster with text, images, and maps.en
dc.description.abstractThe Oyster Bay Formation is a recessive, thin-bedded, fine-grained succession that disconformably overlies the Upper Cretaceous Nanaimo Group in isolated exposures along the eastern coast of Vancouver Island, British Columbia. The Formation consists of thin-bedded siltstone and sandy siltstone intercalated with lesser intervals, and contain permineralized fossil plants, gastropods, decapods, corals, echinoderms, bivalves, and foraminifera. Those fossils, coupled with fossilized crab burrows, suggest a shallow marine depositional setting. Paleontology and palynology suggest a Palocene to Eocene age.en
dc.description.sponsorshipUniversity of Wisconsin--Eau Claire Office of Research and Sponsored Programsen
dc.identifier.urihttp://digital.library.wisc.edu/1793/78054
dc.language.isoen_USen
dc.relation.ispartofseriesUSGZE AS589;
dc.subjectFeldsparen
dc.subjectSandstoneen
dc.subjectBritish Columbiaen
dc.subjectVancouver Islanden
dc.subjectOyster Bay Formationen
dc.subjectPostersen
dc.titleProvenance of the Paleocene-Eocene Oyster Bay Formation, British Columbiaen
dc.typePresentationen

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