The Mohorovičić discontinuity (Moho) is a globally identifiable boundary between the crust
and the uppermost mantle (Dziewonski and Anderson, 1981). It is detected using seismic …

The continental Mohorovičić discontinuity (Moho) has been recognized worldwide from
refracted (Pn) and wide‐angle reflected (PmP) phases from earthquake and explosive …

The strong sensitivity of seismic surface waves to the Moho is evident from a mere visual
inspection of their dispersion curves or waveforms. Rayleigh and Love waves have been …

Application of regional geophysical and geological methods throughout two decades of
Canada's Lithoprobe project provides new opportunities to analyze the Mohorovičić …

The crust/mantle boundary, ie the Mohorovicic, or simply Moho, discontinuity represents the
major petrological boundary between the continental crust and upper mantle. Referring to …

Seismic tomography images of the upper mantle structures beneath the Pacific
Northwestern United States display a maze of high‐velocity anomalies, many of which …

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 …

We use observations of the Moho‐reflected phase PmP to constrain crustal thicknesses and
upper mantle velocities in southern California. We stack normalized absolute values of …

The seismic signature of the Moho from which geologic and tectonic evolution hypotheses
are derived is to a large degree a result of the seismic methodology which has been used to …

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 …