The Palaeoproterozoic crust and upper mantle in the region between the Ukrainian and
Baltic shields of the East European Craton were built up finally during collision of the …

Despite the relatively long-standing availability of numerical approaches for estimating
palaeogeotherms using peridotite xenolith Pressure–Temperature (P–T) data, the practise of …

A new multichannel seismic reflection profile collected across the Sichuan Basin in southern
China by SINOPROBE images prominent reflectors that originate within the lower crust and …

The upper mantle of North America has been well studied using various seismic methods.
Here we investigate the density structure of the North American (NA) upper mantle based on …

The “frozen-in” information in the crust plays an important role in improving our
understanding of cratonic formation and evolution and plate tectonics in the Precambrian …

The collision of the Yakutat block in the corner of the Gulf of Alaska has resulted in large
deformation in the adjacent Chugach–Saint Elias Mountains. This collision is inferred to …

Geophysically detectible mid-lithospheric discontinuities (MLD) and lithosphere-
asthenosphere boundaries (LAB) beneath cratons have received much attention over recent …

Abstract Analysis of the Lithoprobe Deep Probe and Southern Alberta Refraction Experiment
data sets, focusing on the region between Deep Probe shots 43 and 55, has resulted in a …

The Slave craton in northwestern Canada, a relatively small Archean craton (600× 400 km),
is ideal as a natural laboratory for investigating the formation and evolution of Mesoarchean …

We present a summary of geophysical models of the subcrustal lithosphere of Europe. This
includes the results from seismic (reflection and refraction profiles, P-and S-wave …