Sirgue, Laurent, 2003. Inversion de la forme d'onde dans le ...

List of Tables
2.1 Condition of existence of G −1 in equation 2.5 (p. 48 of (Scales et al., 2001)). . 16
2.2 Review of possible cases. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20
2.3 Possible model parameterisations. . . . . . . . . . . . . . . . . . . . . . . . . 48
3.1 Frequency discretisation sequences for the near and far offset surveys. The
last frequency 8 Hz is chosen arbitrarily so that both experiments use identical
frequency ranges within the spectrum of the source signature. . . . . . . . . . . 70
4.1 Number of nonzero singular values with frequency and offset range. . . . . . . 95
4.3 Strategy of preconditioning for the waveform inversion for the 2-D extended
Marmousi experiment. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 129
5.1 Synthetic data characteristics. . . . . . . . . . . . . . . . . . . . . . . . . . . . 139
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