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«Cenoman-Randschuppe»
- Rango
- scaglia tettonica
- Statuto
- termine scorretto (informale)
- In breve
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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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