The continental Mohorovicic discontinuity is most often interpreted as a step‐function
velocity boundary. However, on deep crustal seismic reflection profiles, reflections, at depths …

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 …

The available experimental data and steady‐state calculations make it difficult to explain the
M discontinuity beneath both oceans and continents on the basis of the same phase …

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

The Nature of the Mohorovicic Discontinuity ADS Classic is now deprecated. It will be completely
retired in October 2019. This page will automatically redirect to the new ADS interface at that …

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

Comparisons of deep seismic reflection profiles from a variety of tectonic regions that span a
large fraction of the Earth's history lead to a threefold categorization of reflection patterns …

The concept that the Mohorovicic Discontinuity (Moho) does not necessarily coincide with
the base of the continental crust as defined by rock-type compositions was introduced in the …

Seismic reflection profiles in USA and West Germany over thirty years ago showed strong
reflections from the lower crust but technical advances through the 1970s were needed for …

Since 1978, several seismic reflection transects have been run across the Appalachian and
Ouachita orogens; several special topical reflection lines in the craton have shown the …