This paper presents a new model of the shear velocity structure of the crust and uppermost
mantle beneath the contiguous US The model is based on more than a decade of USArray …

The lateral expansion of the southeastern Tibetan Plateau causes devastating earthquakes,
but is poorly understood. In particular, the links between regional variations in surface …

We present a novel method for joint inversion of receiver functions and surface wave
dispersion data, using a transdimensional Bayesian formulation. This class of algorithm …

A non-linear Bayesian Monte-Carlo method is presented to estimate a Vsv model beneath
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …

The detection of a seismic boundary, the “Moho”, between the outermost shell of the Earth,
the Earth's crust, and the Earth's mantle by A. Mohorovičić was the consequence of …

Rayleigh wave phase velocity maps from ambient noise and earthquake data are inverted
jointly with receiver functions observed at 828 stations from the USArray Transportable Array …

Seismology is among the intrinsic sciences that strictly affect human lives. Many research
efforts are presented in the literature aiming at achieving risk mitigation and disaster …

Studying the structures, properties and origins of the Earth's internal discontinuities is an
important part in the efforts to understand the physical and chemical properties of the …

Receiver functions are a powerful tool to isolate and interpret receiver-side structure effects
in teleseismic seismic records. They are easily constructed by deconvolving one component …

Cross correlation of seismic-background motions (;) is applied to observations from the
Korean Meteorological Administration seismic network to estimate the short-period Rayleigh …