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hammer and plate seismic source was used. Seismic reflection data were&#xD;
recorded on 24 receivers at 10 m interval and 30 m offset. Sea bed&#xD;
reflections are observed at all sites. Surface elevation measurements are&#xD;
provided to allow estimation of ice thickness when an ice base reflection is&#xD;
not visible.&#xD;
&#xD;
Funded as part of the Polar Science for Planet Earth Programme, British Antarctic Survey, Natural Environment Research Council.</gco:CharacterString>
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