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Causse, C., Vincent, J. -S. (1989) Th–U disequilibrium dating of Middle and Late Pleistocene wood and shells from Banks and Victoria islands, Arctic Canada. Canadian Journal of Earth Sciences, 26 (12) 2718-2723 doi:10.1139/e89-231

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Reference TypeJournal (article/letter/editorial)
TitleTh–U disequilibrium dating of Middle and Late Pleistocene wood and shells from Banks and Victoria islands, Arctic Canada
JournalCanadian Journal of Earth Sciences
AuthorsCausse, C.Author
Vincent, J. -S.Author
Year1989 (December 1)Volume26
Issue12
PublisherCanadian Science Publishing
DOIdoi:10.1139/e89-231Search in ResearchGate
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Mindat Ref. ID480334Long-form Identifiermindat:1:5:480334:2
GUID0
Full ReferenceCausse, C., Vincent, J. -S. (1989) Th–U disequilibrium dating of Middle and Late Pleistocene wood and shells from Banks and Victoria islands, Arctic Canada. Canadian Journal of Earth Sciences, 26 (12) 2718-2723 doi:10.1139/e89-231
Plain TextCausse, C., Vincent, J. -S. (1989) Th–U disequilibrium dating of Middle and Late Pleistocene wood and shells from Banks and Victoria islands, Arctic Canada. Canadian Journal of Earth Sciences, 26 (12) 2718-2723 doi:10.1139/e89-231
In(1989, December) Canadian Journal of Earth Sciences Vol. 26 (12) Canadian Science Publishing
Abstract/Notes An attempt has been made at dating Middle and Late Pleistocene deposits from Banks and Victoria islands using the Th–U disequilibrium method. Geological correlations are difficult to establish because of the discontinuous nature of the terrestrial units and the relative absence of datable fossil wood and shells. The Th–U geochemical system likely remained closed for extended periods because of the presence of permafrost, which implies very limited or absent water circulation. The Th–U age determinations obtained confirmed the previously established stratigraphic framework and provide chronological information in that samples of Sangamonian age are differentiated from those that are younger (Wisconsinan and Holocene) or older (Middle Pleistocene). The Th–U disequilibrium method carefully used in areas where water circulation is limited can thus provide chronological control for sediments older than those that can be dated by the radiocarbon method.


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