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We present a method for inverting for laterally heterogeneous earth structure with respect to a laterally heterogeneous starting model. Our method makes it possible to perform iterative linearized inversion of seismic waveform data; in contrast, previous methods have been limited to a single iteration in which the entire laterally heterogeneous part of the model is treated as a perturbation. We demonstrate the feasibility of our approach by inverting for low angular order (s = 1 to s = 4) laterally heterogeneous upper mantle structure with respect to a laterally heterogeneous starting model, using data from the IDA network.
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Hara et al. (2007) studied this question.
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