The seismic reflection method seeks to extract maps of the Earth's sedimentary crust from
transient near-surface recording of echoes, stimulated by explosions or other controlled …

Least‐squares inversion of seismic reflection waveform data can reconstruct remarkably
detailed models of subsurface structure and take into account essentially any physics of …

In multiparameter full-waveform inversion (FWI) and specifically one describing the
anisotropic behavior of the medium, it is essential that we have an understanding of the …

In most geologic environments, accounting for anisotropy is necessary to perform acoustic
full waveform inversion (FWI) of wide-azimuth and wide-aperture seismic data because of …

We show that the linearized reflection coefficients for arbitrary anisotropic media embedded
in an isotropic background can be derived directly from a Born formalism. Due to rapidly …

We develop a fast swee** method for static Hamilton–Jacobi equations with convex
Hamiltonians. Local solvers and fast swee** strategies apply to structured and …

Linearized inversion provides one possible sense of image amplitude correctness. An
image or bandlimited model perturbation has correct amplitudes if it is an approximate …

The retrieval of near-receiver mantle structure from scattered waves associated with
teleseismic P and S and recorded on three-component, linear seismic arrays is considered …

Common image gathers (CIGs) in the offset and surface azimuth domain are used
extensively in migration velocity analysis and amplitude variation with offset (AVO) studies. If …

Uncertainty quantification in the context of seismic imaging is important for interpreting
inverted subsurface models and updating reservoir models. The limited illumination, noisy …