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

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

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 …

Results of deep seismic soundings from various areas of the world are presented. Much
weight is put on recent European investigations. Seismic refraction surveys are found to …

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

In October 1909 an earthquake near Pokupsko, about 40 km to the southeast of Zagreb in
Croatia, sparked the interest of the meteorologist and seismologist Andrija Mohorovičić. He …

Since the late 1970s studies of the oceanic crust using airgun sources and towed
hydrophone arrays have been conducted in a wide range of ocean basin settings including …