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Two types of microseisms

Gutenberg, B. (1958) Two types of microseisms. Journal of Geophysical Research, 63 (3). pp. 595-597. ISSN 0148-0227. https://resolver.caltech.edu/CaltechAUTHORS:20140807-150207193

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Abstract

In general, microseisms are a nuisance. It is now quite widely agreed that microseisms are channel waves, similar in nature to the Lg and Rg waves. It is not at all unusual to observe microseisms which have traveled over distances of continental proportions. In order to determine the direction from which the microseisms come and to investigate in more detail the characteristics of microseismic disturbances, we established a tri-partite system on Mount Palomar.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1029/JZ063i003p00595DOIArticle
http://onlinelibrary.wiley.com/doi/10.1029/JZ063i003p00595/abstractPublisherArticle
Additional Information:Copyright 1958 by the American Geophysical Union.
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological Sciences881
Issue or Number:3
Record Number:CaltechAUTHORS:20140807-150207193
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20140807-150207193
Official Citation:Gutenberg, B. (1958), Two types of microseisms, J. Geophys. Res., 63(3), 595–597, doi:10.1029/JZ063i003p00595
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:48201
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:07 Aug 2014 22:07
Last Modified:03 Oct 2019 07:01

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