The earthquake activity of Norway and nearby offshore areas is low to intermediate, with few
events above magnitude 5. Recent significant improvements in instrumental coverage in …

In 1989–1990 the SeaMARC II side-looking sonar and swath bathymetric system imaged
more than 80 000 km 2 of the seafloor in the Norwegian-Greenland Sea and southern Arctic …

A comprehensive compilation of 112 earthquake focal mechanism solutions in Norway and
adjacent areas has been completed, including 7 previously unpublished solutions for recent …

The analysis of heat flow, seismic, and topographic data collected in the northern Norwegian‐
Greenland Sea reveals an asymmetric evolution of the Eurasian and North American plates …

This chapter is essentially a continuation of the preceding chapter, and the introduction of
that chapter serves also as an introduction to this chapter. As was stated there, the main …

Dynamic glacier activity is increasingly observed through passive seismic monitoring. We
analysed near-regional-scale seismicity on the Arctic archipelago of Svalbard to identify …

Геолого-геофизическая уникальность Северного Ледовитого океана стала очевидной
еще в XX веке после выполнения региональных исследований. Больше нигде на Земле …

The Svalbard Archipelago is situated in the northwestern part of the Barents shelf, in close
proximity to the passive continental margin. This intraplate region is characterized by some …

Recent major improvements in our knowledge about the seismicity (historical and
contemporary) in the continental margin areas of Norway has now made it possible to obtain …

Integrated interpretation of multi-beam bathymetric, sediment-penetrating acoustic
(PARASOUND) and seismic data show a multiple slope failure on the northern European …