PSEUDO GREENS-FUNCTIONS AND WAVE-FORM TOMOGRAPHY

Retrieving source characteristics for moderate-sized earthquakes in sp arsely instrumented regions has been made possible in recent years, th rough the modeling of waveforms at regional distances. The techniques used in such studies model waveform successfully at long period, using Green's functions for simple 1D crustal models. For small earthquakes (ill < 4), however, long-period signals are usually noisy, and modeli ng short-period waveforms requires refined Green's functions such as u sed in the empirical Green's function (eGf) approach. In this article, we present a new technique that generates such Green's functions by p erturbing individual generalized ray responses calculated from a ID mo del. The model is divided into blocks, and velocities in the blocks ar e allowed to vary, which shifts the arrival time of the individual ray s similar to conventional tomography. The amplitudes of the rays are p erturbed independently to accommodate local velocity variations in the structure. For moderate-sized earthquakes with known source mechanism and time history, the velocity variation in each block and the amplif ication factor for individual rays can be optimized using a simulated annealing algorithm. The resulting modified Green's functions. pseudo Green's functions (pGfs), can be used to study the relative location a nd characteristics of neighboring events. The method is also useful in retrieving 2D structure, which is essentially waveform tomography.