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 Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Bulletin of the Seismological Society of America; February 1970; v. 60; no. 1; p. 167-191
© 1970 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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by DUNKIN, J. W.
Right arrow Articles by CORBIN, D. G.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Deformation of a layered, elastic, half-space by uniformly moving line loads

J. W. DUNKIN and D. G. CORBIN

ESSO PRODUCTION RESEARCH COMPANY, HOUSTON, TEXAS

Abstract

When a layered half-space is subjected to loads which move uniformly along its surface, the deformation of the half-space depends on the manner in which the load couples into the surface-wave modes. The uniform speed of the load selects those parts of the modal spectra that have phase velocities equal to the load speed. The restriction that the phase velocity be real leads to novel dispersion relations for the leaky modes, but the trapped mode dispersion relations are the usual ones. In this paper general expressions are derived for the solution for uniformly moving line loads on an elastic half-space containing an arbitrary number of layers. In addition to the modal contributions, the solution contains contributions from source singularities and a line integral that reduce to the static solution as the load speed tends to zero. The details are worked out for the special case of a single low-speed layer lying on a high-speed half-space. For the modes, real and imaginary parts of frequency and velocity amplitudes at various depths are presented as functions of frequency. Total velocity waveforms are shown for selected load speeds and depths.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
J. Pujol, P. Rydelek, and T. Bohlen
Determination of the Trajectory of a Fireball Using Seismic Network Data
Bulletin of the Seismological Society of America, August 1, 2005; 95(4): 1495 - 1509.
[Abstract] [Full Text] [PDF]




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