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Multiarrival wavefront tracking and its applications
2008
Geochemistry Geophysics Geosystems
1] Multivalued traveltimes have traditionally not been used in seismic imaging, with only a handful of notable exceptions in the field of exploration geophysics. For studies at local and regional scales (e.g., local earthquake/teleseismic tomography), the focus has largely been on first arrivals, with numerous ray-and grid-based schemes developed for their calculation. However, later arrivals often contribute to the length and shape of a recorded wave train, particularly in regions of complex
doi:10.1029/2008gc002069
fatcat:a5m4bdgjprhaloo2s5kam3ln74