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TitleU-Pb zircon ages of volcanic ashes integrated with ammonite biostratigraphy, Fernie Formation (Jurassic), western Canada, with implications for Cordilleran-Foreland Basin connections and comments on the Jurassic time scale
 
AuthorPana, D I; Poulton, T P; Heaman, L M
SourceBulletin of Canadian Petroleum Geology vol. 66, no. 3, 2018 p. 595-622
Image
Year2018
Alt SeriesEarth Sciences Sector, Contribution Series 20160212
PublisherNRC Research Press
Documentserial
Lang.English
Mediapaper; on-line; digital
RelatedThis publication is accompanied by U-Pb zircon ages of volcanic ashes integrated with ammonite biostratigraphy, Fernie Formation (Jurassic), Western Canada: supplementary data files
File formatpdf (Adobe® Reader®); html
ProgramGeoscience for New Energy Supply (GNES) Shale Reservoir Characterization
Released2018 09 01
AbstractThe Jurassic system of the Western Canada Sedimentary Basin records the transition in its tectonic setting from a 'passive' back-arc platformal basin to a foreland basin at the western margin of ancient North America. We report new U-Pb zircon ages from bentonite layers and from probable volcanic ash components of clastic detritus in other strata of the Fernie Formation, which encompasses most of the Jurassic in the western portions of the basin and which is now deformed in the Rocky Mountain fold-and-thrust belt. The bentonite ages come from the lower Nordegg Member (Pliensbachian) and an equivalent ash layer in the Lower Fernie phosphatic shale. Detrital zircon spectra from the Bathonian Gryphaea Bed silty limestone and the zircon ages from the mainly Oxfordian Green Beds glauconitic sandstone also are likely indicative of contemporaneous ash-falls. In addition, we review previously published U-Pb bentonite ages from the Fernie Formation and comment on the Jurassic time scale as represented on the International Chronostratigraphic Chart. We have compiled an updated local stratigraphic correlation chart against a time scale that incorporates ages for some of the Middle and Upper Jurassic stage boundaries, from the literature, that differ from those on the current standard charts. The presence of multiple volcanic ashes throughout the Jurassic system in the Western Canada Sedimentary Basin supports tectonostratigraphic models with relatively nearby western magmatic activity. The southeastern Omineca crystalline belt and Quesnellia terrane contain magmatic rocks with ages that could account for all of the Fernie ashes, and are closest to the depositional basin, but source terranes farther afield cannot be ruled out.
Summary(Plain Language Summary, not published)
Volcanic ash layers, deposited everywhere at the same time in stratigraphic sequences, are tools for the correlation of those sequences. They also indicate proximity to volcanic sources, within several thousands of km. Further, the radioactive decay of their uranium content (U-Pb dating) contributes to our knowledge of the geological time scale which currently is very poorly controlled within the Jurassic period. These ages also permit correlation with volcanic events in the western Cordillera, and permit speculation regarding the paleogeographic location of the ancient volcanic systems, and the tectonic plate motions that are implied since they were active. All of these data allow for a better understanding of the Western Canada Sedimentary Basin, and the conditions pertaining to the formation of its natural resources. The Jurassic in Alberta is particularly noted as a major source, and a moderate reservoir of oil and gas.
GEOSCAN ID299314

 
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