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Dinoflagellate biostratigraphy, Dawson Canyon Formation, Hibernia area, offshore Eastern Canada

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dc.contributor.advisorHills, Leonard V.
dc.contributor.authorHyslop, Kevin D.
dc.coverage.spatial2000003371en
dc.date.accessioned2005-07-21T19:48:38Z
dc.date.available2005-07-21T19:48:38Z
dc.date.issued1986
dc.descriptionBibliography: p. 96-110.en
dc.format.extentxi, 110 leaves : ill., maps ; 30 cm.en
dc.identifier.citationHyslop, K. D. (1986). Dinoflagellate biostratigraphy, Dawson Canyon Formation, Hibernia area, offshore Eastern Canada (Master's thesis, University of Calgary, Calgary, Canada). Retrieved from https://ucalgary.scholaris.ca. doi:10.11575/PRISM/24409
dc.identifier.doihttp://dx.doi.org/10.11575/PRISM/24409
dc.identifier.isbn0315327537
dc.identifier.lccQE 688 H47 1987en
dc.identifier.urihttp://hdl.handle.net/1880/21971
dc.language.isoeng
dc.publisher.institutionUniversity of Calgaryen
dc.publisher.placeCalgaryen
dc.relationAdditional Copy: QE 688 H47 1986en
dc.rightsUniversity of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.
dc.subject.lccQE 688 H47 1987en
dc.subject.lcshGeology, Stratigraphic - Cretaceous
dc.subject.lcshGeology, Stratigraphic - Tertiary
dc.subject.lcshGeology - Newfoundland - Dawson Canyon Formation
dc.subject.lcshDawson Canyon Formation (Nfld.)
dc.subject.lcshDinoflagellata, Fossil
dc.titleDinoflagellate biostratigraphy, Dawson Canyon Formation, Hibernia area, offshore Eastern Canada
dc.typemaster thesis
thesis.degree.disciplineGeology and Geophysics
thesis.degree.grantorUniversity of Calgary
thesis.degree.nameMaster of Science (MSc)
ucalgary.thesis.accessionTheses Collection 58.002:Box 586 215772189
ucalgary.thesis.additionalcopyQE 688 H47 1986
ucalgary.thesis.notesoffsite
ucalgary.thesis.uarcreleasey

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