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Wave velocities at depths between 50 and 600 kilometers

Gutenberg, B. (1953) Wave velocities at depths between 50 and 600 kilometers. Bulletin of the Seismological Society of America, 43 (3). pp. 223-232. ISSN 0037-1106. http://resolver.caltech.edu/CaltechAUTHORS:20140806-123113965

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Abstract

Wave velocities in the interior of the earth are usually calculated by means of the Wiechert-Herglotz method. Incorrect interpretation of the form of the travel time curve for a certain distance interval then leads to errors not only in results concerning the corresponding depth interval but (in decreasing amounts) also for all greater depths. A new method is described and applied to that portion of the earth's mantle in which earthquake foci exist. Values obtained with this method for velocities at various depths are independent of each other.


Item Type:Article
Related URLs:
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http://bssa.geoscienceworld.org/content/43/3/223.abstractPublisherArticle
Additional Information:Copyright © 1953, by the Seismological Society of America. Manuscript received for publication July 7, 1952.
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Caltech Division of Geological Sciences601
Record Number:CaltechAUTHORS:20140806-123113965
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20140806-123113965
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:48094
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:06 Aug 2014 20:12
Last Modified:13 Feb 2019 18:02

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