[PDF][PDF] Effects of surface geology on ground motion: recent results and remaining issues
PY Bard - Proc. 10 European Conf. Earth. Eng., ed. Duma …, 1995 - researchgate.net
This paper reviews the recent developments concerning the methods allowing the
estimation of ground shaking site effects in a particular site, as well as the main lessons …
estimation of ground shaking site effects in a particular site, as well as the main lessons …
Large-scale simulation of seismic wave motion: A review
We review key ingredients that are needed for high-fidelity simulation of earthquake-
generated seismic waves in large regions. Specifically, we survey existing literature on wave …
generated seismic waves in large regions. Specifically, we survey existing literature on wave …
Site effect evaluation using spectral ratios with only one station
J Lermo, FJ Chávez-García - Bulletin of the …, 1993 - pubs.geoscienceworld.org
The spectral ratio technique is a common useful way to estimate empirical transfer function
to evaluates site effects in regions of moderate to high seismicity. The purpose of this paper …
to evaluates site effects in regions of moderate to high seismicity. The purpose of this paper …
An unsplit convolutional perfectly matched layer improved at grazing incidence for the seismic wave equation
D Komatitsch, R Martin - Geophysics, 2007 - library.seg.org
The perfectly matched layer (PML) absorbing boundary condition has proven to be very
efficient from a numerical point of view for the elastic wave equation to absorb both body …
efficient from a numerical point of view for the elastic wave equation to absorb both body …
2D and 3D elastic wave propagation by a pseudo-spectral domain decomposition method
A new numerical method is presented for propagating elastic waves in heterogeneous earth
media, based on spectral approximations of the wavefield combined with domain …
media, based on spectral approximations of the wavefield combined with domain …
The spectral element method for elastic wave equations—application to 2‐D and 3‐D seismic problems
D Komatitsch, JP Vilotte, R Vai… - … Journal for numerical …, 1999 - Wiley Online Library
A spectral element method for the approximate solution of linear elastodynamic equations,
set in a weak form, is shown to provide an efficient tool for simulating elastic wave …
set in a weak form, is shown to provide an efficient tool for simulating elastic wave …
Retrieval of the Green's function from cross correlation: the canonical elastic problem
FJ Sánchez-Sesma, M Campillo - Bulletin of the …, 2006 - pubs.geoscienceworld.org
In realistic materials, multiple scattering takes place and average field intensities or energy
densities follow diffusive processes. Multiple P to S energy conversions by the random …
densities follow diffusive processes. Multiple P to S energy conversions by the random …
Dynamic stability analysis of jointed rock slopes using the DDA method: King Herod's Palace, Masada, Israel
YH Hatzor, AA Arzi, Y Zaslavsky, A Shapira - International Journal of Rock …, 2004 - Elsevier
A dynamic, two-dimensional, stability analysis of a highly discontinuous rock slope is
demonstrated in this paper. The studied rock slope is the upper terrace of King Herod's …
demonstrated in this paper. The studied rock slope is the upper terrace of King Herod's …
[PDF][PDF] The spectral-element method in seismology
We present the main properties of the spectral-element method, which is well suited for
numerical calculations of synthetic seismograms for three-dimensional Earth models. The …
numerical calculations of synthetic seismograms for three-dimensional Earth models. The …
Seismic response of three-dimensional alluvial valleys for incident P, S, and Rayleigh waves
FJ Sanchez-Sesma, F Luzon - Bulletin of the …, 1995 - pubs.geoscienceworld.org
A simplified indirect boundary-element method (BEM) is presented. It is used to compute the
seismic response of three-dimensional alluvial valleys under incident P, S, and Rayleigh …
seismic response of three-dimensional alluvial valleys under incident P, S, and Rayleigh …