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This document presents a new method for directly inverting seismic refraction data in dipping planar structures. It uses slant stacking of common-shot profiles to obtain a delay time-slowness (tau-p) wavefield. The tau-p curves from two shotpoints describing critical arrivals are automatically picked and jointly used to iteratively calculate velocity and dip of isovelocity lines, obtaining a 2D velocity model. This method was successfully applied to synthetic and field data from central California, indicati

Author

Daod Daospi

Language

EN