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Автор Smith, P. E.
Автор York, D.
Автор Chen, Y.
Автор Evensen, N. M.
Дата выпуска 1996
dc.description The late Quaternary plinian eruption forming the Kos Plateau Tuff on the island of Kos, Greece, was one of the largest in the Mediterranean. A precise date for this eruption would significantly improve the chronology of the deep‐sea tephra layer W‐3, because reliable correlation of W‐3 with the KOS Plateau Tuff has been previously established. We have dated sanidine from the eruption at 161.3±1.1 ka using the laser‐fusion single crystal <sup>40</sup>Ar‐<sup>39</sup>Ar technique. This age represents a significant refinement over both conventional and highly precise (Cassignol method) K‐Ar ages, and the <sup>40</sup>Ar‐<sup>39</sup>Ar age is shown to be in remarkably good agreement with the age of W‐3 inferred from recent astronomically calibrated oxygen isotope chronologies.
Формат application.pdf
Копирайт Copyright 1996 by the American Geophysical Union.
Тема Volcanology
Тема Volcanology: Ash deposits
Тема Geographic Location
Тема Information Related to Geographic Region: Europe
Тема Information Related to Geologic Time
Тема Information Related to Geologic Time: Cenozoic
Название Single crystal <sup>40</sup>Ar‐<sup>39</sup>Ar dating of a Late Quaternary paroxysm on Kos, Greece: Concordance of terrestrial and marine ages
Тип article
DOI 10.1029/96GL02759
Electronic ISSN 1944-8007
Print ISSN 0094-8276
Журнал Geophysical Research Letters
Том 23
Первая страница 3047
Последняя страница 3050
Аффилиация Smith, P. E.; Department of Physics, University of Toronto, Toronto, Ontario
Аффилиация York, D.; Department of Physics, University of Toronto, Toronto, Ontario
Аффилиация Chen, Y.; Department of Physics, University of Toronto, Toronto, Ontario
Аффилиация Evensen, N. M.; Department of Physics, University of Toronto, Toronto, Ontario
Выпуск 21
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