Three-dimensional frequency-domain full-waveform inversion with an iterative solver

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Global adjoint tomography: first-generation model (2016, background): “D wave propagation in iterative seismic inversions (Akçelik et al. 2002, 2003; Tromp et al. 2005; Fichtner et al. 2006a,b; Tromp et al. 2008; Plessix 2009; Virieux & Operto 2009; Monteiller et al. 2015; Komatitsch et al. 2016).”
A parametrization study for surface seismic full waveform inversion in an acoustic vertical transversely isotropic medium (2011, background): “D applications have also been reported (Epanomeritakis et al. 2008; Fichtner et al. 2009; Plessix 2009; Plessix & Perkins 2010; Sirgue et al. 2010; Vigh et al. 2010).”
Seismic imaging: From classical to adjoint tomography (2012, result): “Models are first inverted at a low frequency where the initial guess is sufficiently close to the true model to guarantee the linearity of the waveform function, and then successively inverted at higher frequencies using inversion results from the previous frequency as the initial model for the curr”
Fast 3D frequency-domain full-waveform inversion with a parallel block low-rank multifrontal direct solver: Application to OBC data from the North Sea (2016, methodology): “A few applications of 3D frequency-domain FWI on synthetic or real data are presented in Ben Hadj Ali et al. (2008), Plessix (2009), Petrov and Newman (2014), Operto et al. (2015).”