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 Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Bulletin of the Seismological Society of America; February 1967; v. 57; no. 1; p. 1-8
© 1967 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
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
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by CRAMPIN, S.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Shear-coupled higher mode seismic surface waves

STUART CRAMPIN

SEISMOLOGICAL INSTITUTE UPPSALA UNIVERSITY, UPPSALA, Sweden

Abstract

Some higher mode wave trains with irregular dispersion, and some anomalies in the S-wave motion at epicentral distances less than 30°, are shown to be shear-coupled higher modes. The group velocities along the higher mode portions of the paths agree well with observations of direct higher mode dispersion in Scandinavia.

Footnotes

Now at: SEISMOLOGY UNIT 6 SOUTH OSWALD ROAD EDINBURGH 9, SCOTLAND




This article has been cited by other articles:


Home page
 Bulletin of the Seismological Society of AmericaHome page
J. A. BROOKS
Rayleigh waves in southern New Guinea: I. Higher mode group velocities
Bulletin of the Seismological Society of America, April 1, 1969; 59(2): 945 - 958.
[Abstract] [PDF]


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