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 1969; v. 59; no. 1; p. 317-330
© 1969 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 CHANDRA, U.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Exact solution for the displacement components in P1P2P1, (S1S2S1)SV, (S1S2S1)SH head waves due to an impulsive double couple source

UMESH CHANDRA

DEPARTMENT OF GEOPHYSICS AND GEOPHYSICAL ENGINEERING SAINT LOUIS UNIVERSITY, ST. LOUIS, MISSOURI

Abstract

Exact integral expressions for the displacement components as a function of azimuth, in P1P2P1, (S1S2S1)SV, and (S1S2S1)SH head waves due to an impulsive double-couple source of arbitrary orientation in two semi-infinite media separated by a plane horizontal boundary, and the effect of free surface on it, have been obtained. The time variation of the source is assumed to be represented by the Heaviside unit function. The response due to an arbitrary source excitation may, however, be obtained from this solution by superposition. Necessary formulae for the operational interpretation of integral equations occurring in the problem are given.

Illustrative examples showing the waveform in P1P2P1, (S1S2S1)SV, and (S1S2S1)SH head-wave displacement components for a particular fault and a suitably chosen earth model are given. Plots of the projection of particle trajectory for P waves in ur-uz plane, and for S waves in u{phi}-ur and u{phi}-uz planes are given for different azimuths; where ur, u{phi}, uz are the components of displacement in a cylindrical coordinate system (r, {phi}, z).







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