generated from top by lateral averaging of velocities.based on synthetic times for Broad Epikarst model (Sheehan, 2005a, Fig.1D Delta-t-V velocity-depth profile below each station.Smooth Inversion = 1D gradient initial model +2D WET Wavepath Eikonal Traveltime tomography Get minimum-structure 1D gradient initial model : Top : pseudo-2D Delta-t-V display Schedule 13:00 – 13:10 Overview and introductions 13:10 – 13:40 Introduction to refraction method & Rayfract® 13:40 – 14:40 Rayfract® tutorial dataset #1: Val de Travers 14:40 – 14:55 Break 14:55 – 15:45 Rayfract® tutorial dataset #2: Success Dam 15:45 – 17:00 Work on individual datasets EEGS Short CourseProcessing of Seismic Refraction Tomography Data SAGEEP 2010 Keystone, Colorado April 10, 2010
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