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Advanced filters: Author: S. ten Hietbrink Clear advanced filters

  • The retreat of the Fennoscandian Ice Sheet during the last deglaciation led to the infiltration of seawater into a submarine groundwater system on the Norwegian continental shelf, according to an analysis of groundwater geochemistry on the Norwegian shelf.

    • S. ten Hietbrink
    • H. Patton
    • W.-L. Hong
    ResearchOpen Access
    Nature Geoscience
    Volume: 18, P: 779-786