The integral equation method is used to model the propagation of surface waves in 3-D structures. The wavefield is represented by the Fredholm integral equation, and the scattered surface waves are calculated by solving the integral equation numerically. The integration of the Green's function elements is given analytically by treating the singularity of the Hankel function at R = 0, based on the proper expression of the Green's function and the addition theorem of the Hankel function. No far-field and Born approximation is made. We investigate the scattering of surface waves propagating in layered reference models imbedding a heterogeneity with different density, as well as Laméconstant contrasts, both in frequency and time domains, for incident plane waves and point sources. © 2008 The Authors Journal compilation © 2008 RAS.
CITATION STYLE
Lu, L., Maupin, V., Zeng, R., & Ding, Z. (2008). Scattering of surface waves modelled by the integral equation method. Geophysical Journal International, 174(3), 857–872. https://doi.org/10.1111/j.1365-246X.2008.03787.x
Mendeley helps you to discover research relevant for your work.