We explore the validity of the linear relation between cross-correlation delay times and velocity model perturbations that is required for linearized finite-frequency tomography. We estimate delay times from a large number of 'ground truth' seismograms computed with the spectral element method in 3-D models. We find that the observed cross-correlation delays remain sufficiently linear, depending on frequency, for sharp velocity contrasts of up to 10 per cent in a checkerboard model. This significantly extends the domain of linearity beyond that of inversions based on direct waveform differences. A small deviation from linearity can be attributed to the Wielandt effect (i.e. the asymmetry in the effect of positive and negative anomalies on the traveltime). Smoother Gaussian covariance models can have velocity variations twice as large and cross-correlation delay times still remain sufficiently linear for tomographic interpretations.
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Univ Calif Santa Cruz, Inst Geophys & Planetary Phys, Santa Cruz, CA 95060 USAUniv Calif Santa Cruz, Inst Geophys & Planetary Phys, Santa Cruz, CA 95060 USA
Geng, Yu
Xie, Xiao-Bi
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Univ Calif Santa Cruz, Inst Geophys & Planetary Phys, Santa Cruz, CA 95060 USAUniv Calif Santa Cruz, Inst Geophys & Planetary Phys, Santa Cruz, CA 95060 USA
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Univ Notre Dame, Dept Elect Engn, Notre Dame, IN 46556 USA
Raytheon SAS, Ft Wayne, IN 46808 USAUniv Notre Dame, Dept Elect Engn, Notre Dame, IN 46556 USA
Kleber, Nikolaus
Dietlein, Charles R.
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CCDC ARL, Adelphi, MD 20783 USAUniv Notre Dame, Dept Elect Engn, Notre Dame, IN 46556 USA
Dietlein, Charles R.
Chisum, Jonathan D.
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Univ Notre Dame, Dept Elect Engn, Notre Dame, IN 46556 USAUniv Notre Dame, Dept Elect Engn, Notre Dame, IN 46556 USA