2015
DOI: 10.1007/s00015-015-0177-0
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The succession of the Val Marecchia Nappe (Northern Apennines, Italy) in the light of new field and biostratigraphic data

Abstract: This paper challenges the classical idea that the Val Marecchia Nappe, the highest of the north-eastern Apennines, is a nappe that originated from the External Ligurian Domain and consisting of Upper Cretaceous-Middle Eocene rocks, accreted to the Palaeo-Apenninic Chain in the Middle-Late Eocene due to the Ligurian tectonic phase. Its succession comprises a Middle-Late Jurassic ophiolitic substratum and its sedimentary cover of Late Jurassic to Early Miocene age. This succession is quite similar to those of th… Show more

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Cited by 12 publications
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“…and the Pliocene deposits (Argille Azzurre Fm., Figure 3). The Ligurian Unit formations span in age from Early Cretaceous to Middle Eocene for the Marecchia Valley area (part of these units are ascribed to a more external domain by Perrone, De Capoa, & Cesarini, 1998and by De Capoa et al, 2015.…”
Section: Geological Settingmentioning
confidence: 99%
“…and the Pliocene deposits (Argille Azzurre Fm., Figure 3). The Ligurian Unit formations span in age from Early Cretaceous to Middle Eocene for the Marecchia Valley area (part of these units are ascribed to a more external domain by Perrone, De Capoa, & Cesarini, 1998and by De Capoa et al, 2015.…”
Section: Geological Settingmentioning
confidence: 99%