• A study of large-scale basins and comparison to the Eastern Barents Sea basins 

      Braitenberg, Carla; Ebbing, Jörg (NGU-Rapport (2006.081), Report, 2006)
      Detailed study of the gravity field and the isostatic state of the Barents Sea Region shows that the Eastern Barents Sea basins are not typical rift basins. They show distinctive features as large wavelengths, high ...
    • Gravity and magnetic interpretation of the regional deep structure of the Vøring Basin 

      Ebbing, Jörg (NGU-Rapport (2003.081), Report, 2004)
      The crustal structrue in the outer Vøring Basin is investigated by forward modelling of gravity data and interpretation of the magnetic field and the isostatic state. In addition all available magentic and gravity data for ...
    • Lithospheric structure and tectonic setting of the greater Barents Sea Region 

      Ebbing, J.; Skilbrei, J. R.; Marello, L.; Barrère, C.; Wienecke, S.; Buiter, S.; Braitenberg, C. (NGU-Rapport (2008.012), Report, 2008)
      The Barents Sea is characterised by deep basins in the western and eastern Barent Sea, and large-scale differences in the lithospheric structure, which reflect the different tectonic history and basin forming processes. ...
    • Neotectonics in Norway. Annual Technical Report 1997 

      Olesen, Odleiv et.al.; Dehls, John (NGU-Rapport (98.016), Report, 1998)
      Neotectonic crustal deformations have been reported at a large number of locations in Norway (both on local and regional scales). The NEONOR Project represents a national effort by several national research and mapping ...
    • New insigths into the West Siberian Basin from the satellite mission GRACE 

      Ebbing, Jörg; Braitenberg, Carla (NGU-Rapport (2007.056), Report, 2007)
      The West Siberian Basin covers an area of ~3.2 x10(6) sq.km and is among the most extended basins in the world. Recent investigations have revealed that the basin contrains and extensive layer of flood basalts of late ...