Seismicity of the Nordland
area, Norway
Jan Michalek, Lars Ottemoeller, Berit Marie Storheim, Marte Louise Strømme
University of Bergen, Norway
The Nordland
area (65-70N; 8-18E) is tectonically active part of Norway. Enhanced seismicity may
reflect on off-shore subsidence combined with the uplift of landmasses usually attributed to glacial
isostatic adjustment (related
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