NissirosV1, Main, Exploration, bibRecord, 000313

Single crystal 40Ar‐39Ar dating of a Late Quaternary paroxysm on Kos, Greece: Concordance of terrestrial and marine ages

Identifieur interne : 000313 ( Main/Exploration ); précédent : 000312; suivant : 000314

Single crystal 40Ar‐39Ar dating of a Late Quaternary paroxysm on Kos, Greece: Concordance of terrestrial and marine ages

Auteurs : P. E. Smith [Canada] ; D. York [Canada] ; Y. Chen [Canada] ; N. M. Evensen [Canada]

Source :

Geophysical Research Letters [ 0094-8276 ] ; 1996-10-15.

RBID : ISTEX:00828BF71B1D548EA700C8D2FD4AD176C8EA7BF1

English descriptors

KwdEn :
- Ageof, Composite isochron, Eastern mediterranean, Hilgen, Isochron, Isotope, Keller, Kelleret, Late quaternary paroxysm, Pasteels, Pleistocene, Pumice, Quartz, Sanidine, Santorini, Sapropel, Stratigraphic, Tephra, Thekostuff, Tuff, University toronto, Xenocrystic contamination, Xenolith.
Teeft :
- Ageof, Composite isochron, Eastern mediterranean, Hilgen, Isochron, Isotope, Keller, Kelleret, Late quaternary paroxysm, Pasteels, Pleistocene, Pumice, Quartz, Sanidine, Santorini, Sapropel, Stratigraphic, Tephra, Thekostuff, Tuff, University toronto, Xenocrystic contamination, Xenolith.

Abstract

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 40Ar‐39Ar technique. This age represents a significant refinement over both conventional and highly precise (Cassignol method) K‐Ar ages, and the 40Ar‐39Ar age is shown to be in remarkably good agreement with the age of W‐3 inferred from recent astronomically calibrated oxygen isotope chronologies.

Url:

https://api.istex.fr/document/00828BF71B1D548EA700C8D2FD4AD176C8EA7BF1/fulltext/pdf

DOI: 10.1029/96GL02759

Affiliations:

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Le document en format XML

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<front><div type="abstract">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 40Ar‐39Ar technique. This age represents a significant refinement over both conventional and highly precise (Cassignol method) K‐Ar ages, and the 40Ar‐39Ar age is shown to be in remarkably good agreement with the age of W‐3 inferred from recent astronomically calibrated oxygen isotope chronologies.</div>
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<name sortKey="York, D" sort="York, D" uniqKey="York D" first="D." last="York">D. York</name>
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Single crystal 40Ar‐39Ar dating of a Late Quaternary paroxysm on Kos, Greece: Concordance of terrestrial and marine ages

Single crystal 40Ar‐39Ar dating of a Late Quaternary paroxysm on Kos, Greece: Concordance of terrestrial and marine ages

Source :

English descriptors

Abstract

Links toward previous steps (curation, corpus...)

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri