Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; July 1958; v. 48; no. 3; p. 253-268
© 1958 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by HUDSON, D. E.
Right arrow Articles by HOUSNER, G. W.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

An analysis of strong-motion accelerometer data from the San Francisco earthquake of March 22, 1957

D. E. HUDSON and G. W. HOUSNER

EARTHQUAKE ENGINEERING RESEARCH LABORATORY, DIVISION OF ENGINEERING CALIFORNIA INSTITUTE OF TECHNOLOGY,, PASADENA, CALIFORNIA

Abstract

The San Francisco earthquake of March 22, 1957, was recorded simultaneously by accelerometers at five United States Coast and Geodetic Survey stations in the San Francisco area. Response spectrum curves were computed from the acceleration-time records, and from these response spectrum curves the spectrum intensities have been determined. From these spectrum intensities certain conclusions are drawn as to: (1) the effects of local geology on the recorded ground motions; (2) the calculation of total energy released by the earthquake from strong-motion accelerometer records; (3) possible influence of structural dynamic behavior on the accelerations recorded in building basements, and the relationship between basement accelerations and ground accelerations; and (4) the applicability of a simplified type of strong-motion earthquake instrument for investigations of local distribution effects. A general comparison is made between the present earthquake and typical Pacific Coast earthquakes.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
R. D. BORCHERDT and G. GLASSMOYER
On the characteristics of local geology and their influence on ground motions generated by the Loma Prieta earthquake in the San Francisco Bay region, California
Bulletin of the Seismological Society of America, April 1, 1992; 82(2): 603 - 641.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
R. DOBRY, I. M. IDRISS, and E. NG
A reply
Bulletin of the Seismological Society of America, December 1, 1979; 69(6): 2127 - 2128.
[PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
E. FACCIOLI
A stochastic approach to soil amplification
Bulletin of the Seismological Society of America, August 1, 1976; 66(4): 1277 - 1291.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
R. D. BORCHERDT
Effects of local geology on ground motion near San Francisco Bay
Bulletin of the Seismological Society of America, February 1, 1970; 60(1): 29 - 61.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
I. M. IDRISS and H. B. SEED
An analysis of ground motions during the 1957 San Francisco earthquake
Bulletin of the Seismological Society of America, December 1, 1968; 58(6): 2013 - 2032.
[Abstract] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1958 by the Seismological Society of America.