Laboratory measurements of seismic velocities in ocean sediments
- 18 March 1954
- journal article
- Published by The Royal Society in Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences
- Vol. 222 (1150) , 336-341
- https://doi.org/10.1098/rspa.1954.0076
Abstract
Laboratory measurements have been made of the compressional wave velocities in samples of deep-sea sediments using ultrasonic methods. The variation of velocity with compaction pressure has been determined. From the results it has been concluded that a vertical gradient of velocity exists in the sedimentary layer of the ocean.Keywords
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