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; February 1969; v. 59; no. 1; p. 317-330
© 1969 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
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 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).







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1969 by the Seismological Society of America.