Identification and dispersion of the campanian ash layer (Y-5) in the sediments of the Eastern Mediterranean
Identification and dispersion of the campanian ash layer (Y-5) in the sediments of the Eastern Mediterranean
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.
19-25
Cramp, Adrian
9d81da27-979d-4ec8-88eb-236924f8a8a2
Vitaliano, Charles J.
17ed7e2a-47f3-4134-8aba-ef3637542f05
Collins, Michael B.
3b70278b-0004-45e0-b3c9-0debdf0a9351
1989
Cramp, Adrian
9d81da27-979d-4ec8-88eb-236924f8a8a2
Vitaliano, Charles J.
17ed7e2a-47f3-4134-8aba-ef3637542f05
Collins, Michael B.
3b70278b-0004-45e0-b3c9-0debdf0a9351
Cramp, Adrian, Vitaliano, Charles J. and Collins, Michael B.
(1989)
Identification and dispersion of the campanian ash layer (Y-5) in the sediments of the Eastern Mediterranean.
Geo-Marine Letters, 9 (1), .
(doi:10.1007/BF02262814).
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.
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Published date: 1989
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Local EPrints ID: 192519
URI: http://eprints.soton.ac.uk/id/eprint/192519
ISSN: 0276-0460
PURE UUID: 78dc00c2-d522-4193-bfb0-0c085082409b
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Date deposited: 05 Jul 2011 10:36
Last modified: 14 Mar 2024 03:50
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Author:
Adrian Cramp
Author:
Charles J. Vitaliano
Author:
Michael B. Collins
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