Ultrasonic Velocity Investigations of Crystal Anisotropy in Deep Ice Cores from Antarctica
Ice cores from Byrd Station and Little America V have been used to test an ultrasonic technique for evaluating crystal anisotropy in the Antarctic Ice Sheet. P-wave velocities measured parallel and perpendicular to the vertical axes of cores from the 2164-m-thick ice sheet at Byrd Station have yield...
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Format: | Text |
Language: | English |
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1979
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Online Access: | http://www.dtic.mil/docs/citations/ADA071451 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA071451 |