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Study on the limitations of traveltime inversion in the presence of extreme velocity anomalies

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Academic year: 2017

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Table 1. Velocities and densities used in the synthetic model. Physical properties were taken from Carmichael (1982)
Table 2. Parameters used to generate synthetic data.
Table 3. Allowed variation to generate modified models for velocity, velocity gradient and thick- thick-ness for every layer in models 1 and 2.
Table 4. Picking uncertainty in ms for every layer considered in metropolis algorithm.
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