Seismic full-waveform inversion (FWI) for imaging Earth's interior was introduced in the late
1970s. Its ultimate goal is to use all of the information in a seismogram to understand the …

Seismic tomography is a powerful tool for illuminating Earth structure across a range of
scales, but the usefulness of any image that is generated by this method is dependent on …

Building on global adjoint tomography model GLAD-M15, we present transversely isotropic
global model GLAD-M25, which is the result of 10 quasi-Newton tomographic iterations with …

Full waveform inversion using the conventional L 2 distance to measure the misfit between
seismograms is known to suffer from cycle skip**. An alternative strategy is proposed in …

We recognized that the envelope fluctuation and decay of seismic records carries ultra low-
frequency (ULF, ie, the frequency below the lowest frequency in the source spectrum) …

Recent progress in numerical methods and computer science allows us today to simulate
the propagation of seismic waves through realistically heterogeneous Earth models with …

We present the first-generation global tomographic model constructed based on adjoint
tomography, an iterative full-waveform inversion technique. Synthetic seismograms were …

Wave equation based inversions, such as full-waveform inversion and reverse-time
migration, are challenging because of their computational costs, memory requirements and …

Low-frequency seismic data are crucial for convergence of full-waveform inversion (FWI) to
reliable subsurface properties. However, it is challenging to acquire field data with an …