The Flysch di Solignano was deposited in a basin plain below the CCD close to the western margin of the Ligurian Tethys. The siliciclastic supply was mainly delivered by a crystalline basement of Sardinian-Corsican affinity. The carbonate supply, made up of pelagic ooze, derived by oceanic intrabasinal structural highs represented by transform prisms uplifted within the compressive field affecting the Ligurian domain during Late Cretaceous. Resedimentation processes were likely triggered by tsunami waves
Il Flysch di Solignano nel quadro dei Flysch a Elmintoidi (Maastrichtiano inferiore, Appennino settentrionale)
Tateo;
1990
Abstract
The Flysch di Solignano was deposited in a basin plain below the CCD close to the western margin of the Ligurian Tethys. The siliciclastic supply was mainly delivered by a crystalline basement of Sardinian-Corsican affinity. The carbonate supply, made up of pelagic ooze, derived by oceanic intrabasinal structural highs represented by transform prisms uplifted within the compressive field affecting the Ligurian domain during Late Cretaceous. Resedimentation processes were likely triggered by tsunami wavesFile in questo prodotto:
Non ci sono file associati a questo prodotto.
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
