ZusammenfassungEine Neuuntersuchung der Tektonik in den Vilser Alpen und im Hochvogelgebiet, wo die Frage seit langer Zeit diskutiert wird, ob dort die Allgfiu-und Lechtal-Decke getrennte Einheiten bilden, oder stratigraphisch untrennbar zusammenh~ingen, erbrachte eine eindeutige Entscheidung fiir den Deckenbau. Der Verlauf der Deckengrenze konnte zwischen Hochvogel und Hohenschwangauer Alpen prfizisiert werden. Der interne Falten-und Schuppenbau der Lechtal-Decke hat nirgends zur Bildung yon tektonisch tieferen Teildekken geffihrt, die internen Verschuppungen besitzen nur ein geringes Ausmafl. AbstractA new investigation of the tectonics in the Vilser Alps and in the Mt. Hochvogel area where since a long time a discussion was going on if the thrust sheets of All#iu-and Lechtal-Decke are separate units or connected by stratigraphic sequences, a definite decision could be made in favour of the nappe structure in this part of the Northern Calcareous Alps. The internal structure of the Lechtal-Decke thrust sheet is characterized by local imbricate structure which originate from sheared folds.
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