The Mt Freikofel at the Austria-Italy border is constituted of one of the best, and most complete Devonian sequence of the Carnic Alps (Fig. 1). It was not disrupted by the Variscan and Alpine tectonics, and it is quite easy to follow on the field due to the special morphology of the mount. The sequence is made by seven calcareous formations representing different depositional settings within the lower Palaeozoic Carnic basin. These lithostratigraphic units yield more or less rich conodont faunas that allowed to set a date in terms of conodont biostratigraphy to the whole sequence.

The Devonian sequence at the Mt Freikofel (Carnic Alps, Austria-Italy)

Spalletta C.
Writing – Original Draft Preparation
;
Corradini C.
Membro del Collaboration Group
;
Perri M. C.
Membro del Collaboration Group
;
2023

Abstract

The Mt Freikofel at the Austria-Italy border is constituted of one of the best, and most complete Devonian sequence of the Carnic Alps (Fig. 1). It was not disrupted by the Variscan and Alpine tectonics, and it is quite easy to follow on the field due to the special morphology of the mount. The sequence is made by seven calcareous formations representing different depositional settings within the lower Palaeozoic Carnic basin. These lithostratigraphic units yield more or less rich conodont faunas that allowed to set a date in terms of conodont biostratigraphy to the whole sequence.
2023
Workshop Geology and Paleontology of Friuli and adjacent areas in memory of Luca Simonetto - Museo Friulano di Storia Naturale Udine, 16-17 June 2023
57
60
Spalletta C., Corradini C., Simonetto L., Corriga M.G., Perri M.C., Pondrelli, M.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11585/943077
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