Correctly interpreting phase events thanks to data processing techniques based on
correlation or deconvolution has been the focus of numerous studies in the field of high …

Time-shift estimation between arrivals in two seismic traces before and after a velocity
perturbation is a crucial step in many seismic methods. The accuracy of the estimated …

We present a three‐dimensional (3‐D) hybrid method that interfaces the spectral‐element
method (SEM) with the frequency‐wave number (FK) technique to model the propagation of …

Conversions of shear waves (S) to compressional waves (P), often analysed as Sp receiver
functions, are useful for studying upper-mantle layering, and have been used to map upper …

The information obtained from seismic monitoring at injection sites is often limited to seismic
event properties (eg, location, origin time, moment tensor), the accuracy of which greatly …

A method for scattered wave imaging in 3‐D with both teleseismic P and S wave receiver
function data is introduced. The approach relies on body‐wave scattering kernels that are …

Topside reverberations off mantle discontinuities are commonly observed at long periods,
but their interpretation is complicated because they include both near‐source and near …

Full-waveform inversion (FWI) is not yet a mature imaging technology for lithospheric
imaging from teleseismic data. Therefore, its promise and pitfalls need to be assessed more …

Receiver function analysis is widely used to image sharp structures in the Earth, such as the
Moho or transition zone discontinuities. Standard procedures either rely on the assumption …

We demonstrate with synthetic and field data that with sufficiently dense sampling wave-
equation-based methods such as reverse time migration (RTM), implicitly forming array …