Complete seismogram synthesis for transversely isotropic media
Item
Title (Dublin Core)
en-US
Complete seismogram synthesis for transversely isotropic media
Description (Dublin Core)
en-US
The response at the surface of a layered transversely isotropic medium due to a buried dislocation source can be expressed by using propagator matrices and discrete wavenumber summation. These operations produce complete seismograms for earthquake or explosion sources which include all body- and surface-vave phases for this specialized anisotropic structure. In order to test the numerical procedures, synthetic seismograms at near distances for an isotropic model are compared with those generated by other methods. The agreement is found to be satisfactory in all cases. Comparisons of synthetic seismograms for anisotropic models having a small degree of anisotropy with similar but isotropic models, show that significant differences in travel times, amplitudes and wave forms can be caused by the anisotropy.
ARK: https://n2t.net/ark:/88439/y066890
Permalink: https://geophysicsjournal.com/article/226
ARK: https://n2t.net/ark:/88439/y066890
Permalink: https://geophysicsjournal.com/article/226
Creator (Dublin Core)
Mandal, B.
Mitchell, B.J.
Subject (Dublin Core)
en-US
Anisotropy
en-US
Transverse isotropy
en-US
Propagator matrices
en-US
Wavenumber summation
en-US
Synthetic seismogram
en-US
Seismology
Publisher (Dublin Core)
en-US
Journal of Geophysics
Date (Dublin Core)
1986-02-27
Type (Dublin Core)
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US
Peer-reviewed Article
Format (Dublin Core)
application/pdf
Identifier (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/226
Source (Dublin Core)
en-US
Journal of Geophysics; Vol 59 No 1 (1986): Journal of Geophysics; 149-156
2643-2986
2643-9271
Language (Dublin Core)
eng
Relation (Dublin Core)
https://journal.geophysicsjournal.com/JofG/article/view/226/186