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Il Flysch di Solignano nel quadro dei Flysch a Elmintoidi (Maastrichtiano inferiore, Appennino settentrionale)

1990
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 ...
Fontana D   +5 more
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Der Flysch

1991
K. J. Hsü, U. Briegel
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Paesaggi dei flysch appenninici

2004
I Flysch sono successioni di arenarie, calcari e peliti di origine torbiditica. I paesaggi dei Flysch, sono in funzione della litologia che li costituisce (alternanza di litotipi) e, soprattutto, dell’assetto strutturale. Nell'articolo vengono descritti, con l'ausilio di carte dell'IGM, alcuni esempi di paesaggi dei Flysch nell'Appennino Settentrionale.
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FLYSCH SEDIMENTATION

Geological Society of America Bulletin, 1957
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Sedimentology of Istrian flysch Megabeds

2019
The Istrian Foreland basin was formed during the Eocene period in collisional processes between the Adria microplate and the Eurasian plate as a foredeep depozone in front of the migrating Dinaridic wedge (KORBAR, 2009). Its sedimentary fill consists of Foraminiferal limestones, Transitional beds (Globigerina marls) and Istrian flysch which represent ...
Bergant, Stanislav, Petrinjak, Krešimir
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Il Flysch di Solignano nel quadro dei Flysch a Helmintoid (Maastrichtiano inferiore, Appennino settentrionale)

1990
The Flysch di Solignano was deposited in a basin plain below the CCD close to the western margin of the Ligurian Tethys during Early Maastrichtian.The siliciclastic supply was mainly delivered by a crystalline basement of Sardinian-Corsican affinity.
FONTANA, Daniela   +3 more
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