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King, R. H., Kingston, M. S., Barnett, R. L. (1982) A numerical approach toward the classification of magnetites from tephra in southern Alberta. Canadian Journal of Earth Sciences, 19 (10) 2012-2019 doi:10.1139/e82-178

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Reference TypeJournal (article/letter/editorial)
TitleA numerical approach toward the classification of magnetites from tephra in southern Alberta
JournalCanadian Journal of Earth Sciences
AuthorsKing, R. H.Author
Kingston, M. S.Author
Barnett, R. L.Author
Year1982 (October 1)Volume19
Issue10
PublisherCanadian Science Publishing
DOIdoi:10.1139/e82-178Search in ResearchGate
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Mindat Ref. ID477286Long-form Identifiermindat:1:5:477286:0
GUID0
Full ReferenceKing, R. H., Kingston, M. S., Barnett, R. L. (1982) A numerical approach toward the classification of magnetites from tephra in southern Alberta. Canadian Journal of Earth Sciences, 19 (10) 2012-2019 doi:10.1139/e82-178
Plain TextKing, R. H., Kingston, M. S., Barnett, R. L. (1982) A numerical approach toward the classification of magnetites from tephra in southern Alberta. Canadian Journal of Earth Sciences, 19 (10) 2012-2019 doi:10.1139/e82-178
In(1982, October) Canadian Journal of Earth Sciences Vol. 19 (10) Canadian Science Publishing
Abstract/Notes High-titanium glass-encased magnetites associated with intermixed tephras in upper subalpine soils in Banff National Park are shown to be characteristic of Mazama tephra and of regional significance. Similar magnetites occur in a Mazama layer above a paleosol at Fish Creek, Alberta and within a sample of Mazama ash (UA 396) from Windy Point, Alberta. Detailed sampling and analysis of the Fish Creek tephra indicate that the magnetites do not represent a separate eruptive event or an older ashfall. Cluster analysis of glass-encased magnetites from reference samples of Mazama, St. Helens Y, and Bridge River ashes revealed composite grouping of Mazama and Bridge River magnetites and separate and strong groupings of high-TiO2 magnetites. Discriminant analysis identifies MgO, TiO2, and Al2O3 as the most significant chemical discriminants between the various ashes. Discriminant function analysis identifies the high-titanium magnetites as Mazama in type and successfully classifies 96% of the tephra-derived magnetites in two soils developed from intermixed ashes. Numerical analysis confirms the utility of compositional variations in tephra-derived magnetites in providing a time-stratigraphic framework in the analysis of volcanic ash soils in western Canada.


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