Underplating was originally proposed as the process of magma ponding at the base of the
crust and was inferred from petrologic considerations. This process not only may add high …

We present a new digital crustal model for Moho depth and crustal structure in Europe,
Greenland, Iceland, Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W …

Prior to participating in Rodinia, the East European Craton (Baltica) had undergone a
complex process of development. Many of the structures, which were important during the …

Summary The European Plate has a 4.5 Gy long and complex tectonic history. This is
reflected in the present-day large-scale crustal structures. A new digital Moho depth map is …

Publisher Summary The wealth of new data from the Fennoscandian Shield allows an
attempt of a new comprehensive tectonic model for the Paleoproterozoic evolution of the …

The Transscandinavian Igneous Belt (TIB) comprises a giant elongated array of batholiths
extending c. 1400 km across the Scandinavian Peninsula from southeasternmost Sweden to …

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 …

A priori knowledge on large-scale sub-surface conductivity structure is required in many
applications investigating electrical properties of the lithosphere. A map on crustal …

We present a digital model SibCrust of the crustal structure of the Siberian craton (SC) and
the West Siberian basin (WSB), based on all seismic profiles published since 1960 and …

Magmatism has occurred throughout Earth's history. From the early Earth to the modern
plate-tectonic Earth, the amount of magmatism has varied, but it has always occurred on …