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; December 1987; v. 77; no. 6; p. 2181-2191
© 1987 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 VARADAN, V. K.
Right arrow Articles by LANGSTON, C. A.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Radiation characteristics of elastodynamic line sources buried in layered media with periodic interfaces. I. SH- wave analysis

VIJAY K. VARADAN, AKHLESH LAKHTAKIA, VASUNDARA V. VARADAN and CHARLES A. LANGSTON

LABORATORY OF ELECTROMAGNETIC AND ACOUSTIC RESEARCHDEPARTMENT OF ENGINEERING SCIENCE AND MECHANICSTHE PENNSYLVANIA STATE UNIVERSITY, UNIVERSITY PARK, PENNSYLVANIA 16802
DEPARTMENT OF GEOSCIENCES THE PENNSYLVANIA STATE UNIVERSITY, UNIVERSITY PARK, PENNSYLVANIA 16802

Abstract

Using the T matrix method, or the extended boundary condition, the solution for a class of problems involving an SH line source in an elastic wave guide is determined. The boundaries of the wave guide may be periodically corrugated and the wave guide may be embedded between elastic media. Numerical results are given for a seismically interesting case of wave propagation in a one-layer crustal model over a mantle half-space with a corrugated free surface representing the Basin and Range topography in the Western United States. Analysis of the scattered fields at the surface, and of the fields radiated into the half-space, shows complicated field behavior, even with sinusoidal free surface corrugation. These results are directly applicable to regional wave propagation and scattering.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
X. Chen
Seismogram synthesis for multi-layered media with irregular interfaces by global generalized reflection/transmission matrices method. II. Applications for 2D SH case
Bulletin of the Seismological Society of America, August 1, 1995; 85(4): 1094 - 1106.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
X.-F. CHEN
Seismogram synthesis for multi-layered media with irregular interfaces by global generalized reflection/transmission matrices method. I. Theory of two-dimensional SH case
Bulletin of the Seismological Society of America, December 1, 1990; 80(6A): 1696 - 1724.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
H. D. AXILROD and J. F. FERGUSON
SH-wave scattering from a sinusoidal grating: An evaluation of four discrete wavenumber methods
Bulletin of the Seismological Society of America, June 1, 1990; 80(3): 643 - 655.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
V. K. VARADAN, A. LAKHTAKIA, V. V. VARADAN, and C. A. LANGSTON
Radiation characteristics of elastodynamic line sources buried in layered media with periodic interfaces. II. P- and SV-wave analysis
Bulletin of the Seismological Society of America, December 1, 1987; 77(6): 2192 - 2211.
[Abstract] [PDF]




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