New insights into Arctic tectonics: u-pb, (u-th)/he, and hf isotopic data from the Franklinian Basin, Canadian Arctic islands

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dc.contributor.advisorLeier, Andrew
dc.contributor.authorAnfinson, Owen Anthony
dc.date.accessioned2017-12-18T22:30:41Z
dc.date.available2017-12-18T22:30:41Z
dc.date.issued2012
dc.descriptionBibliography: p. 37-46, 75-83, 97-101, 105-106, 110-113en
dc.descriptionIncludes copies of copyright permission. Original copies with original Partial Copyright Licence.en
dc.description.abstractMore than 2300 detrital zircon uranium-lead (U-Pb) ages, 32 6Hf/177Hf (£Hf) isotopic values, 37 apatite helium (AHe) ages, and 72 zircon helium (ZHe) ages rep­resent the first in-depth geochronologic and thermochronologic study of Franklinian Basin strata in the Canadian Arctic and provide new insight on >500 M.y. of geologic history along the northern Laurentian margin (modern orientation). Detrital zircon U-Pb age data demonstrate that the Franklinian Basin succession is composed of strata with three distinctly different provenance signatures. Neoproterozoic and Lower Cambri­an formations contain detrital zircon populations consistent with derivation from Archean to Paleoproterozoic gneisses and granites of the west Greenland-northeast Canadian Shield. Lower Silurian to Middle Devonian strata are primarily derived from foreland basin strata of the East Greenland Caledonides (Caledonian orogen). Middle Devonian to Upper Devonian strata also contain detrital zircon populations interpreted as being primarily northerly derived from the continental landmass responsible for the Ellesme­rian Orogen ( often referred to as Crockerland). U-Pb age data from basal turbidites of the Middle to Upper Devonian elastic succession suggest Crockerland contributed sedi­ment to the northern Laurentian margin by early-Middle Devonian time and that prior to the Ellesmerian Orogeny Crockerland had a comparable geologic history to the northern Baltica Craton. Detrital zircon U-Pb ages in Upper Devonian strata suggest Crockerland became the dominant source by the end of Franklinian Basin sedimentation. Mean £Hf values from Paleozoic detrital zircon derived from Crockerland sug­gest the zircons were primarily formed in either an island arc or continental arc built on accreted oceanic crust setting. ZHe cooling ages from Middle and Upper Devonian strata were not buried deeper than 7 km since deposition and suggest Crockerland was partially exhumed during the Caledonian Orogen. AHe cooling ages are partially reset since deposition and experienced varying burial histories depending on stratigraphic and geographic location within the basin. AHe ages from Middle Devonian strata from the western margin of the basin indicate episodes of exhumation associated with elastic in­fluxes of sediment into the Sverdrup Basin during the Late Jurassic-Early Cretaceous and Late Cretaceous.
dc.format.extentix, 169 leaves : ill. ; 30 cm.en
dc.identifier.citationAnfinson, O. A. (2012). New insights into Arctic tectonics: u-pb, (u-th)/he, and hf isotopic data from the Franklinian Basin, Canadian Arctic islands (Doctoral thesis, University of Calgary, Calgary, Canada). Retrieved from https://prism.ucalgary.ca. doi:10.11575/PRISM/4715en_US
dc.identifier.doihttp://dx.doi.org/10.11575/PRISM/4715
dc.identifier.urihttp://hdl.handle.net/1880/105716
dc.language.isoeng
dc.publisher.institutionUniversity of Calgaryen
dc.publisher.placeCalgaryen
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.titleNew insights into Arctic tectonics: u-pb, (u-th)/he, and hf isotopic data from the Franklinian Basin, Canadian Arctic islands
dc.typedoctoral thesis
thesis.degree.disciplineGeology and Geophysics
thesis.degree.grantorUniversity of Calgary
thesis.degree.nameDoctor of Philosophy (PhD)
ucalgary.item.requestcopytrue
ucalgary.thesis.accessionTheses Collection 58.002:Box 2082 627942954
ucalgary.thesis.notesUARCen
ucalgary.thesis.uarcreleaseyen
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