Figure 4
Evolution of fast bulk sound wave Fréchet derivative Kc, the shear wave derivative  and the impedance derivative K′ρ (top, middle and bottom rows, respectively) from the initial model m00 (first column) through model m04 (fifth column) for a poroelastic inversion using direct P-wave traveltime anomalies. Note how the amplitude of the gradient decreases with each subsequent iteration. A similar number of iterations is required for acoustic, elastic and Gassmann elastic inversions.

Evolution of fast bulk sound wave Fréchet derivative Kc, the shear wave derivative graphic and the impedance derivative Kρ (top, middle and bottom rows, respectively) from the initial model m00 (first column) through model m04 (fifth column) for a poroelastic inversion using direct P-wave traveltime anomalies. Note how the amplitude of the gradient decreases with each subsequent iteration. A similar number of iterations is required for acoustic, elastic and Gassmann elastic inversions.

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