• «Cenoman-Randschuppe»

    Rang
    écaille tectonique
    Statut
    terme incorrect (mais utilisé de manière informelle)
    En bref

    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.

    Montrer les détails
haute de page