Abstract Earth Crustal Model 1 (ECM1) is a 1° x 1° global crustal model that describes the
thickness of the crust, including the overlying sediments, and the corresponding seismic …

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 …

We have addressed the geophysical problem of obtaining an elastic model of the
subsurface from recorded normal-incidence seismic data using convolutional neural …

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

Frequency-domain wavefield solutions corresponding to the anisotropic acoustic wave
equation can be used to describe the anisotropic nature of the Earth. To solve a frequency …

Exploration seismology uses reflected and refracted seismic waves, emitted from a
controlled (active) source into the ground, and recorded by an array of seismic sensors …

Summary The European Plate has a 4.5 Gy long and complex tectonic history. This is
reflected in the present-day large-scale crustal structures. A new digital Moho depth map is …

We test a fully non-linear method to solve Bayesian seismic tomographic problems using
data consisting of observed traveltimes of first-arriving waves. Rather than using Monte …

We develop and apply a full waveform inversion method that incorporates seismic data on a
wide range of spatio-temporal scales, thereby constraining the details of both crustal and …

Active source seismology provides a critical constraint on the global crustal structure.
However, the heterogeneous data coverage means that interpolation is necessary to fill the …