Seismic Evidence of a Wet Zone Under the West Antarctic Ice Sheet
Abstract It appears to be possible to identify certain conditions of thermal regime at the base of a glacier through the seismic reflection method. In some cases layers of water or wet rock debris may be identifiable. The procedure is based upon the reversal of phase of reflected dilatational waves...
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Cambridge University Press (CUP)
1976
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Online Access: | http://dx.doi.org/10.1017/s0022143000031439 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031439 |
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crcambridgeupr:10.1017/s0022143000031439 2024-03-03T08:37:54+00:00 Seismic Evidence of a Wet Zone Under the West Antarctic Ice Sheet Dewart, Gilbert 1976 http://dx.doi.org/10.1017/s0022143000031439 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031439 en eng Cambridge University Press (CUP) Journal of Glaciology volume 16, issue 74, page 73-88 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1976 crcambridgeupr https://doi.org/10.1017/s0022143000031439 2024-02-08T08:36:15Z Abstract It appears to be possible to identify certain conditions of thermal regime at the base of a glacier through the seismic reflection method. In some cases layers of water or wet rock debris may be identifiable. The procedure is based upon the reversal of phase of reflected dilatational waves at the interface between ice and a substratum of lower acoustic impedance. Illustrations of the method are given from the west Antarctic ice sheet, and suggestions are made for the improvement of the technique. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Journal of Glaciology Cambridge University Press Antarctic West Antarctic Ice Sheet Journal of Glaciology 16 74 73 88 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Dewart, Gilbert Seismic Evidence of a Wet Zone Under the West Antarctic Ice Sheet |
topic_facet |
Earth-Surface Processes |
description |
Abstract It appears to be possible to identify certain conditions of thermal regime at the base of a glacier through the seismic reflection method. In some cases layers of water or wet rock debris may be identifiable. The procedure is based upon the reversal of phase of reflected dilatational waves at the interface between ice and a substratum of lower acoustic impedance. Illustrations of the method are given from the west Antarctic ice sheet, and suggestions are made for the improvement of the technique. |
format |
Article in Journal/Newspaper |
author |
Dewart, Gilbert |
author_facet |
Dewart, Gilbert |
author_sort |
Dewart, Gilbert |
title |
Seismic Evidence of a Wet Zone Under the West Antarctic Ice Sheet |
title_short |
Seismic Evidence of a Wet Zone Under the West Antarctic Ice Sheet |
title_full |
Seismic Evidence of a Wet Zone Under the West Antarctic Ice Sheet |
title_fullStr |
Seismic Evidence of a Wet Zone Under the West Antarctic Ice Sheet |
title_full_unstemmed |
Seismic Evidence of a Wet Zone Under the West Antarctic Ice Sheet |
title_sort |
seismic evidence of a wet zone under the west antarctic ice sheet |
publisher |
Cambridge University Press (CUP) |
publishDate |
1976 |
url |
http://dx.doi.org/10.1017/s0022143000031439 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031439 |
geographic |
Antarctic West Antarctic Ice Sheet |
geographic_facet |
Antarctic West Antarctic Ice Sheet |
genre |
Antarc* Antarctic Ice Sheet Journal of Glaciology |
genre_facet |
Antarc* Antarctic Ice Sheet Journal of Glaciology |
op_source |
Journal of Glaciology volume 16, issue 74, page 73-88 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000031439 |
container_title |
Journal of Glaciology |
container_volume |
16 |
container_issue |
74 |
container_start_page |
73 |
op_container_end_page |
88 |
_version_ |
1792502655630704640 |