Fennoscandia is the key area for glacial isostatic adjustment (GIA) research. Owing to its
long settlement and excellent infrastructure, ongoing land uplift in the north as well as …

Geological and geodynamic models of the mantle often rely on joint interpretations of
published seismic tomography images and petrological/geochemical data. This approach …

We present the official land uplift model NKG2016LU of the Nordic Commission of Geodesy
(NKG) for northern Europe. The model was released in 2016 and covers an area from 49° to …

Abstract In Fennoscandia, tectonics, Glacial Isostatic Adjustment (GIA), and climatic changes
cause ongoing crustal deformation of some millimetres per year, both vertically and …

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 …

The Central European Basin System (CEBS) is composed of a series of subbasins, the
largest of which are (1) the Norwegian–Danish Basin (2), the North German Basin extending …

Sedimentary basins host, among others, most of our energy and fresh-water resources: they
can be regarded as large geo-reactors in which many physical and chemical processes …

A series of steps in the lithospheric thickness of eastern Australia are revealed by the latest
seismic surface wave tomographic model and calculations of the horizontal gradient of …

Abstract Subsequent to the Variscan Orogeny, the lithosphere of Central Europe was
subjected to a series of tectonic events in the Latest Palaeozoic and Mesozoic which were …

We present a uniform updated model of the European lithosphere–asthenosphere boundary
(LAB) recalculated from data collected during our regional studies of seismic anisotropy and …