GEOACOUSTIC MODELS OF THE SEA FLOOR. I. SHALLOW BERING SEA; 2. MOHOLE (GUADALUPE SITE)
The information and technology necessary to derive a valid geological-geophysical-acoustic model of the sea floor are presented. Two contrasting models are detailed and discussed: one in the Bering Sea which has a shallow-water, high-velocity, hard-sand bottom; and the Mohole (Guadalupe Site) model...
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Format: | Text |
Language: | English |
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1965
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Online Access: | http://www.dtic.mil/docs/citations/AD0466064 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0466064 |
Summary: | The information and technology necessary to derive a valid geological-geophysical-acoustic model of the sea floor are presented. Two contrasting models are detailed and discussed: one in the Bering Sea which has a shallow-water, high-velocity, hard-sand bottom; and the Mohole (Guadalupe Site) model which has a deep-water, low-velocity, soft-clay bottom. Other models are to be reported in a continuing series. (Author) |
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