Marine seismic studies near Newport, Oregon
In July 1964 three seismic refraction profiles were recorded over Stonewall Bank (44°32'N, 124°24'W) to determine gross sub-bottom geological structure to depths of thousands of feet. In August 1964 a continuous seismic reflection profiler was used to document shallow geological structure...
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| Language: | en_US |
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2012
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| Online Access: | http://hdl.handle.net/1957/29369 |