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Response of Layered Half-Space Obtained Directly in the Time Domain, Part II: SV-P and Three-Dimensional Sources

¹ Massachusetts Institute of Technology
77 Massachusetts Avenue
Cambridge, Massachusetts 02139
 (E.K.)
² Norwegian Geotechnical Institute
72 Sognsveien
NO-0855, Oslo, Norway
 (J.P.)

In Part I of this set of two companion articles we presented a new, rigorous method to obtain the seismic response of horizontally layered, viscoelastic (or elastic) half-spaces caused by antiplane (SH) sources anywhere. This method is formulated directly in the time domain, and can be applied even in the absence of attenuation. This article (Part II) generalizes the concept to SV-P line sources and to three-dimensional point sources, including seismic moments.

This article has been cited by other articles:

				J. Park and E. Kausel Response of Layered Half-Space Obtained Directly in the Time Domain, Part I: SH Sources Bulletin of the Seismological Society of America, October 1, 2006; 96(5): 1795 - 1809. [Abstract] [Full Text] [PDF]