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We review historical earthquake research in Northern Europe. 'Historical' is defined as being identical with seismic events occurring in the pre-instrumental and early instrumental periods between 107...
The sensitivity of global navigation satellite system (GNSS) measurements in Fennoscandia to nearby viscosity variations in the upper mantle is investigated using a 3-D finite element model of glacial...
An international LAPNET array (2007–2009, http://www.oulu.fi/sgo-oty/lapnet) of the POLENET/LAPNET sub-project of the POLENET-IPY consortium, related to seismic and geodetic studies in the Arctic regi...
A compilation of fission track data is presented here to show from where fission track data are available in Fennoscandia and to highlight potential targets for future research. Because of the relativ...
The Archaean to Palaeoproterozoic West Troms Basement Complex comprises various tonalitic gneisses, felsic and mafic intrusive rocks and intervening narrow NW-SE-trending belts with partly mylonitised...
On the Land Uplift in Fennoscandia.
Phase Velocities of Rayleigh Waves in Southern Fennoscandia.
Gaussian Curvature of Postglacial Rebound and the Discovery of Caves Created by Major Earthquakes in Fennoscandia.
The crustal structure in Fennoscandia has been intensively studied by seismic methods over the last one and half decade. The features and differences of the crustal structure are discussed by reviewi...

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