Add to ORKGWe present a scheme for generating synthetic point-source seismograms for shear dislocation sources using line source (two-dimensional) theory. It is based on expanding the complete three-dimensional solution of the wave equation expressed in cylindrical coordinates in an asymptotic form which provides for the separation of the motions into SH and P-SV systems. We evaluate the equations of motion with the aid of the Cagniard-de Hoop technique and derive close-formed expressions appropriate for finite-difference source excitation
The Parkfield, California, earthquake of 1966 produced the first recording of ground motion in the i...
Twelve three-component strong-motion displacement records are modeled for the 1979 Imperial Valley e...
Given the scarcity of near-source recordings for large earthquakes, numerical simulations play an im...
We present a scheme for generating synthetic point-source seismograms for shear dislocation sources ...
Generalized ray expansions of the P, SH, and SV displacement potentials resulting from a point-sourc...
The exact Cagniard-de Hoop solutions for a point dislocation in half-space are used to construct mod...
Although the earth is 3-dimensional (3-D), numerical simulations of wave propagation through lateral...
The accuracy of the finite-difference method for generating synthetic seismograms of SH wave propaga...
Paper presents the generation and implementation of various types of earthquake sources in a 2D fini...
The strong motion displacement records available during an earthquake can be treated as the response...
The data from five strong-motion accelerograph stations centered above and surrounding the fault are...
Three-dimensional models of a finite fault located in a half-space are constructed to study the gro...
In this work solutions are developed for the motions generated in an elastic half space or a half s...
Two analytical approaches based on the methods of self-similar potentials and rotational superpositi...
The focus on the present study is on the point-source approximation of a seismic source. First, we c...
The Parkfield, California, earthquake of 1966 produced the first recording of ground motion in the i...
Twelve three-component strong-motion displacement records are modeled for the 1979 Imperial Valley e...
Given the scarcity of near-source recordings for large earthquakes, numerical simulations play an im...
We present a scheme for generating synthetic point-source seismograms for shear dislocation sources ...
Generalized ray expansions of the P, SH, and SV displacement potentials resulting from a point-sourc...
The exact Cagniard-de Hoop solutions for a point dislocation in half-space are used to construct mod...
Although the earth is 3-dimensional (3-D), numerical simulations of wave propagation through lateral...
The accuracy of the finite-difference method for generating synthetic seismograms of SH wave propaga...
Paper presents the generation and implementation of various types of earthquake sources in a 2D fini...
The strong motion displacement records available during an earthquake can be treated as the response...
The data from five strong-motion accelerograph stations centered above and surrounding the fault are...
Three-dimensional models of a finite fault located in a half-space are constructed to study the gro...
In this work solutions are developed for the motions generated in an elastic half space or a half s...
Two analytical approaches based on the methods of self-similar potentials and rotational superpositi...
The focus on the present study is on the point-source approximation of a seismic source. First, we c...
The Parkfield, California, earthquake of 1966 produced the first recording of ground motion in the i...
Twelve three-component strong-motion displacement records are modeled for the 1979 Imperial Valley e...
Given the scarcity of near-source recordings for large earthquakes, numerical simulations play an im...