Variations in particle alignment and size in sediments of the Vema Channel record Antarctic bottom-water velocity changes during the last 400 000 years.
The anisotropy of magnetic susceptibility (AMS) and mean particle size in the silt fraction has been measured in surface sediments and selected cores from the Vema Channel. Results show that a function which represents magnetic grain, long-axis alignment is highly correlated with variation in mean s...
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1982
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ftlouisianastuir:oai:digitalcommons.lsu.edu:geo_pubs-1848 2023-06-11T04:04:53+02:00 Variations in particle alignment and size in sediments of the Vema Channel record Antarctic bottom-water velocity changes during the last 400 000 years. Ledbetter, M. T. Ellwood, B. B. 1982-01-01T08:00:00Z https://digitalcommons.lsu.edu/geo_pubs/849 unknown LSU Digital Commons https://digitalcommons.lsu.edu/geo_pubs/849 Faculty Publications text 1982 ftlouisianastuir 2023-05-28T18:17:12Z The anisotropy of magnetic susceptibility (AMS) and mean particle size in the silt fraction has been measured in surface sediments and selected cores from the Vema Channel. Results show that a function which represents magnetic grain, long-axis alignment is highly correlated with variation in mean size of the carbonate-free silt fraction. An increase in alignment with increase in particle size reflects an increase in bottom-water velocity. This correlation has been used to infer fluctuation in Antarctic Bottom water (AABW) velocity during the last 400 000 years. The period of highest inferred bottom-water velocity resulted in a late Pliocene hiatus marked by a buried manganese pavement.-from Authors Text Antarc* Antarctic LSU Digital Commons (Louisiana State University) Antarctic |
institution |
Open Polar |
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LSU Digital Commons (Louisiana State University) |
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ftlouisianastuir |
language |
unknown |
description |
The anisotropy of magnetic susceptibility (AMS) and mean particle size in the silt fraction has been measured in surface sediments and selected cores from the Vema Channel. Results show that a function which represents magnetic grain, long-axis alignment is highly correlated with variation in mean size of the carbonate-free silt fraction. An increase in alignment with increase in particle size reflects an increase in bottom-water velocity. This correlation has been used to infer fluctuation in Antarctic Bottom water (AABW) velocity during the last 400 000 years. The period of highest inferred bottom-water velocity resulted in a late Pliocene hiatus marked by a buried manganese pavement.-from Authors |
format |
Text |
author |
Ledbetter, M. T. Ellwood, B. B. |
spellingShingle |
Ledbetter, M. T. Ellwood, B. B. Variations in particle alignment and size in sediments of the Vema Channel record Antarctic bottom-water velocity changes during the last 400 000 years. |
author_facet |
Ledbetter, M. T. Ellwood, B. B. |
author_sort |
Ledbetter, M. T. |
title |
Variations in particle alignment and size in sediments of the Vema Channel record Antarctic bottom-water velocity changes during the last 400 000 years. |
title_short |
Variations in particle alignment and size in sediments of the Vema Channel record Antarctic bottom-water velocity changes during the last 400 000 years. |
title_full |
Variations in particle alignment and size in sediments of the Vema Channel record Antarctic bottom-water velocity changes during the last 400 000 years. |
title_fullStr |
Variations in particle alignment and size in sediments of the Vema Channel record Antarctic bottom-water velocity changes during the last 400 000 years. |
title_full_unstemmed |
Variations in particle alignment and size in sediments of the Vema Channel record Antarctic bottom-water velocity changes during the last 400 000 years. |
title_sort |
variations in particle alignment and size in sediments of the vema channel record antarctic bottom-water velocity changes during the last 400 000 years. |
publisher |
LSU Digital Commons |
publishDate |
1982 |
url |
https://digitalcommons.lsu.edu/geo_pubs/849 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Faculty Publications |
op_relation |
https://digitalcommons.lsu.edu/geo_pubs/849 |
_version_ |
1768391489957658624 |