The Campi Flegrei Blind Test: Evaluating the Imaging Capability of Local Earthquake Tomography in a Volcanic Area
Figure 26
Mean deviation of the inverted velocity models and ratio from the true ones as a function of depth. Deviation is calculated for each method as the weighted rms difference between the true and inverted models along horizontal planes, using the resolution matrix as a weight. Note that a logarithmic scale is used to represent the quite large dynamics of the values adequately.
