Identification and correlation of distal tephra layers in deep-sea sediment cores, Scotia Sea, Antarctica
Moreton, S.G.; Smellie, J.L.. 1998 Identification and correlation of distal tephra layers in deep-sea sediment cores, Scotia Sea, Antarctica. Annals of Glaciology, 27. 285-289. 10.3189/1998AoG27-1-285-289
Full text not available from this repository. (Request a copy)Abstract/Summary
Quaternary deposits in six sediment cores from the Scotia Sea, Antarctica, were examined for the presence of volcanic ash layers. The cores were recovered from water depths of 3369-4025 m. Altogether, 23 ash layers were found, 18 of which have been investigated by electron-probe microanalysis. Deception Island is identified as the source of all the ash layers analyzed. The upper ash layer in each core can be correlated across all six cores, over a distance of 400 km, on the basis of its unusual bimodal composition, major oxide geochemistry and strati graphic position. Two other ash layers can also be correlated between several of the cores.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.3189/1998AoG27-1-285-289 |
Programmes: | BAS Programmes > Pre 2000 programme |
ISSN: | 0260-3055 |
Date made live: | 10 Dec 2013 11:31 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/504203 |
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