Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Bulletin of the Seismological Society of America Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Bulletin of the Seismological Society of America; February 1974; v. 64; no. 1; p. 99-101
© 1974 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
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
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by BRADNER, H.
Right arrow Articles by BRUNE, J. N.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The use of sonobuoys in determining hypocenters of aftershocks of the February 21, 1973 Pt. Mugu earthquake

HUGH BRADNER and JAMES N. BRUNE

INSTITUTE OF GEOPHYSICS AND PLANETARY PHYSICS SCRIPPS INSTITUTION OF OCEANOGRAPHY, LA JOLLA, CALIFORNIA 92037

Abstract

A five-station sonobuoy array was deployed in the ocean near the epicenter of the February 21, 1973 Pt. Mugu earthquake to supplement California Institute of Technology land stations for aftershock hypocenter locations. The sonobuoy data tend to force epicenters north, compared with locations from land stations alone. The study illustrates the value of sonobuoys for epicenter locations in or near the oceans.







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Seismological Society of America