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We demonstrated that SPL waveform data, together with associated phases, are able to constrain crustal and upper mantle seismic wave velocity structures. Forward modeling is done using a reflectivity algorithm and optimization is carried out using an algorithm called very fast simulated annealing (VFSA). The code runs efficiently on multiple processors(More)
Our goal is to jointly model surface wave dispersion, receiver functions, and characteristics of the waveform that appear in a window around the direct S arrival. Optimization is done using a three part objective function given by Error  a1 || d SPL obs d SPL syn ||p a2 || d dispersion obs d dispersion syn ||p a3 || d receiverfucntion obs d(More)
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