• «Cenoman-Randschuppe»

    Rang
    tektonische Schuppe
    Status
    inkorrekter Begriff (jedoch informell gebraucht)
    Kurzbeschreibung

    The Cenoman-Randschuppe consists of an imbricate zone of slivers formed at the active margin between the Adriatic continental plate and the Piemonte-Liguria Ocean. It lies at the northern rim of the Upper Austroalpine (Northern Calcareous Alps) and consists of flysch-like coarse-grained deposits.

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