Lacustrine sedimentation and tectonics: An example from the Weichselian at Lønstrup Klint, Denmark

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    Resumé

    Sedimentological analysis of the Weichselian deposits exposed in the coastal cliff section at Lønstrup Klint, northern Jutland, Denmark, demonstrates the presence of four sedimentary units comprising fine-grained lacustrine and fluvial deposits of the latest Middle Wcichselian. The Lønstrup Klint section also shows an interplay between glaciotectonics and sedimentation. The two lower sedimentary units are separated by an erosional unconformity of pretectonic origin, whereas the upper two units are syntectonic. The glaciotectonic processes reflect the Late Weichselian expansion of the Scandinavian ice cap into northern Jutland. The sedimentary structures indicate high rates of deposition. The area underwent dramatic palaeogeographic changes from deep lake to proglacial fluvial plain in a time-span of a few thousand years.
    OriginalsprogEngelsk
    Sider (fra-til)113-126
    Antal sider14
    TidsskriftBoreas
    Vol/bind26
    Udgave nummer2
    DOI
    StatusUdgivet - jun. 1997

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    • Programområde 3: Energiressourcer

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