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Low-speed layer in water-covered areas

Press, Frank and Ewing, Maurice (1948) Low-speed layer in water-covered areas. Geophysics, 13 (3). pp. 404-420. ISSN 0016-8033. https://resolver.caltech.edu/CaltechAUTHORS:20141015-143656311

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Abstract

In many water-covered areas it has been reported that the speed of sound in the topmost layers of the bottom is less than that in water. Several methods of investigating such layers are discussed. The normal-mode theory offers the best method of detecting and investigating a low-speed layer covered by water.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/ 10.1190/1.1437410DOIArticle
http://library.seg.org/doi/abs/10.1190/1.1437410PublisherArticle
http://geophysics.geoscienceworld.org/content/13/3/404PublisherArticle
Additional Information:© 1948 Society of Exploration Geophysicists. This work represents results of research carried out for the Bureau of Ships of the Navy Department under contract with Columbia University. Manuscript received by the Editor March 15, 1948.
Issue or Number:3
Record Number:CaltechAUTHORS:20141015-143656311
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20141015-143656311
Official Citation:Frank Press and William Maurice Ewing Low-speed layer in water-covered areas Geophysics, July 1948, v. 13, p. 404-420, doi:10.1190/1.1437410
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:50420
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:15 Oct 2014 22:09
Last Modified:03 Oct 2019 07:23

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