An outcrop of limestones with rich associations of Senonian planctonic foraminifers is reported and described. The limestones was deposited unconformably with the Upper Norian (?)-Raethian Dachstein Limestone. It is interpreted as a neptunian dike originated by the eoalpine tectonic phase that involved the eastern part of Southern Alps.
Tettonica estensionale del Senoniano nel Gruppo del Montasio (Alpi Meridionali orientali)
PONTON, MAURIZIO
2006-01-01
Abstract
An outcrop of limestones with rich associations of Senonian planctonic foraminifers is reported and described. The limestones was deposited unconformably with the Upper Norian (?)-Raethian Dachstein Limestone. It is interpreted as a neptunian dike originated by the eoalpine tectonic phase that involved the eastern part of Southern Alps.File in questo prodotto:
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