Blar i Rapporter på forfatter "Olsen, L."

Viser treff 1-4 av 4

    • Age and location of late Bølling - early Allerød ice-marginal substages in Mid-Norway - Outer Coast and Tingvoll, based on mapping and a compilation of 14C dates 

      Olsen, L.; Høgaas, F.; Sveian, L. (NGU-Rapport (2020.010), Report, 2020)
      The Outer Coast (OC)-Tingvoll ice margins in Mid Norway do not show continuous lines of ice marginal deposits (moraines, ice contact deltas, etc.) (Fig. 1), they appear rather as discontinuous lines of correlated deposits ...

    • Neotectonics in Nordland - Implications for petroleum exploration (NEONOR2) 

      Ottesen, D.; Olsen, L.; Rise, L.; Rodenay, S.; Lauknes,T.R.; Storheim, B.M.; Strømme, M.L.; Tjåland, A.; Drottning, A.; Riis, F.; Olesen,O.; Janutyte,I.; Michálek, J.; Keiding, M.; Lindholm, C.; Kierulf, H.P.; Ottemöller, L.; Gradmann, S.; Maystrenko,Y.P., Rouyet, L.; Dehls, J..; Ask, M.; Ask, D. (NGU-Rapport (2018.010), Report, 2018)
      The individual papers and reports from the NEONOR2 project (Neotectonics in Nordland - implications for petroleum exploration) are compiled in the present report. The results are also summarized and compared to the results ...

    • Neotectonics in Norway, Final Report 

      Blikra, L. H.; Fjeldskaar, W.; Olsen, L.; Roberts, D.; Rise, L.; Brekke, H.; Olesen, O.; Bockmann, L.; Faleide, J. I.; Dehls, J.; Bungum, H.; Riis, F.; Hicks, E.; Braathen, A.; Longva, O.; Lindholm, C. (NGU-Rapport (2000.002), Report, 2000)
      Geodynamic modelling of the present crustal uplift indicates that the uplift of western Norway and northern Norway is partly due to other mechanisms that the glacioisostatic rebound. We have also deduced a new model based ...

    • “Shaken not stirred”: Mosaic sand – a semi-liquefaction phenomenon originating from strong earthquakes 

      Olsen, L.; Høgaas, F. (NGU-Rapport (2020.020), Report, 2020)
      The formation of mosaic sand, here as exemplified from a 0.23 km2 sand field at the coast of Nordland County in Northern Norway, is thought to be related to earthquake induced shaking, re-mobilization and partial (semi-) ...