The direct dynamical problem of seismics for horizontally stratified media.
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Displaying 1 – 5 of 5
The weak boundary effect in a field as a source approaches the boundary.
Krauklis, P.V., Krauklis, A.P. (2004)
Journal of Mathematical Sciences (New York)
Theoretical aspects of a multiscale analysis of the eigenoscillations of the Earth.
Volker Michel (2003)
Revista Matemática Complutense
The elastic behaviour of the Earth, including its eigenoscillations, is usually described by the Cauchy-Navier equation. Using a standard approach in seismology we apply the Helmholtz decomposition theorem to transform the Fourier transformed Cauchy-Navier equation into two non-coupled Helmholtz equations and then derive sequences of fundamental solutions for this pair of equations using the Mie representation. Those solutions are denoted by the Hansen vectors Ln,j, Mn,j, and Nn,j in geophysics....
Time series modelling of the Kobe-Osaka earthquake recordings.
Singh, N., Tampubolon, D., Yadavalli, V. S. S. (2002)
International Journal of Mathematics and Mathematical Sciences
Time-frequency representations of earthquake motion records.
Demetriu, Sorin, Trandafir, Romică (2003)
Analele Ştiinţifice ale Universităţii “Ovidius" Constanţa. Seria: Matematică
Currently displaying 1 – 5 of 5
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