Prominent reflectors are observed at about 30 and 50 km depths throughout much of
northern Scotland. The deeper reflector results from impedance contrasts here attributed to …

Layering at the Moho as determined from seismic reflection data is a commonly observed
phenomenon in the Basin and Range for which we propose a porous‐flow melt model …

Manzhouli-Suifenhe geoscience transect (MS) is one of the eleven transects in China
territory determined by global geoscience transect project. Data acquisition, data processing …

Although the year 2009 marked one century since the discovery of the Moho, or crust-mantle
boundary, the exact nature of that boundary and the manner in which it formed remain major …

A seismic survey in the Archean Minnesota gneiss terrane (3.6-3.8 Ga) imaged a seismically
variable, discontinuous Moho at both vertical incidence and wide angles. The wide-angle …

A wide‐angle stack using all onshore‐offshore, and onshore seismic data from the SIGHT'96
experiment provides a direct three‐dimensional (3‐D) image of the Moho below the …

A study to map the variations in the thickness and velocity contrast of the Mantle-Crust
Transition (MCT) beneath North America is conducted using seismic receiver functions …

The Moho discontinuity is one of the fundamental boundaries on Earth, separating the crust
from the upper mantle. Arrival times of seismic reflection and refraction data are used to …

The geology of Scotland documents a protracted geological history from Precambrian
basement formation through the Caledonian Orogeny and to the Tertiary opening of the …

Based on the full-waveform theoretical seismograms of different Moho velocity models, the
receiver functions of different frequencies are calculated, and the performances of different …