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Identification and dispersion of the campanian ash layer (Y-5) in the sediments of the Eastern Mediterranean

Identifieur interne : 000444 ( Main/Exploration ); précédent : 000443; suivant : 000445

Identification and dispersion of the campanian ash layer (Y-5) in the sediments of the Eastern Mediterranean

Auteurs : Adrian Cramp [Royaume-Uni] ; Charles J. Vitaliano [États-Unis] ; Michael B. Collins [Royaume-Uni]

Source :

RBID : ISTEX:8EFEF34AE0800F6001746477BB903AE7F06E5081

English descriptors

Abstract

Abstract: Sedimentological, mineralogical, optical, and geochemical analyses were used to identify pyroclastic material contained within gravity and piston cores recovered from the northwestern Aegean and Gulf of Corinth areas of the eastern Mediterranean Sea. The lithological, optical, and elemental signatures of the tephra suggest that the material originated from the Campanian Province of Italy, and is known as the Campanian Ash Layer or Y-5. The identification of the Y-5 layer in these two previously unreported areas extend the distribution of this stratigraphic marker and increases the quantitative estimates of pyroclastic material volume. In addition, our knowledge of sedimentary processes active within these two areas is extended.

Url:
DOI: 10.1007/BF02262814


Affiliations:


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


Le document en format XML

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<term>Continental slope</term>
<term>Core sites</term>
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<term>Sedimentary processes</term>
<term>Sedimentation processes</term>
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<div type="abstract" xml:lang="en">Abstract: Sedimentological, mineralogical, optical, and geochemical analyses were used to identify pyroclastic material contained within gravity and piston cores recovered from the northwestern Aegean and Gulf of Corinth areas of the eastern Mediterranean Sea. The lithological, optical, and elemental signatures of the tephra suggest that the material originated from the Campanian Province of Italy, and is known as the Campanian Ash Layer or Y-5. The identification of the Y-5 layer in these two previously unreported areas extend the distribution of this stratigraphic marker and increases the quantitative estimates of pyroclastic material volume. In addition, our knowledge of sedimentary processes active within these two areas is extended.</div>
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