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  • This paper is a detailed critical review of previous studies on the subject. The main conclusion reached is that the techniques applied have been too imprecise and subjective and that a lack of relevant data of all types inhibits the development
  • In the east of the area isostatic depression was considerable and uplift was considerable, reaching up to 220 m near Oslo. Here relative sea level was subject to an almost exponential fall. On the west of the area land uplift was slower and marine