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   <subfield code="a">The Early Miocene &quot;Bisciaro volcaniclastic event” (northern Apennines, Italy): a key study for the geodynamic evolution of the central-western Mediterranean</subfield>
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   <subfield code="c">[Francesco Guerrera, Manuel Martín-Martín, Giuliana Raffaelli, Mario Tramontana]</subfield>
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   <subfield code="a">The Early Miocene Bisciaro Fm., a marly limestone succession cropping out widely in the Umbria-Romagna-Marche Apennines, is characterized by a high amount of volcaniclastic content, characterizing this unit as a peculiar event of the Adria Plate margin. Because of this volcaniclastic event, also recognizable in different sectors of the central-western Mediterranean chains, this formation is proposed as a &quot;marker” for the geodynamic evolution of the area. In the Bisciaro Fm., the volcaniclastic supply starts with the &quot;Raffaello” bed (Earliest Aquitanian) that marks the base of the formation and ends in the lower portion of the Schlier Fm. (Late Burdigalian-Langhian p.p.). Forty-one studied successions allowed the recognition of three main petrofacies: (1) Pyroclastic Deposits (volcanic materials more than 90%) including the sub-petrofacies 1A, Vitroclastic/crystallo-vitroclastic tuffs; 1B, Bentonitic deposits; and 1C, Ocraceous and blackish layers; (2) Resedimented Syn-Eruptive Volcanogenic Deposits (volcanic material 30-90%) including the sub-petrofacies 2A, High-density volcanogenic turbidites; 2B, Low-density volcanogenic turbidites; 2C, Crystal-rich volcanogenic deposits; and 2D, Glauconitic-rich volcaniclastites; (3) Mixing of Volcaniclastic Sediments with Marine Deposits (volcanic material 5-30%, mixed with marine sediments: marls, calcareous marls, and marly limestones). Coeval volcaniclastic deposits recognizable in different tectonic units of the Apennines, Maghrebian, and Betic Chains show petrofacies and chemical-geochemical features related to a similar calc-alkaline magmatism. The characterization of this event led to the hypothesis of a co-genetic relationship between volcanic activity centres (primary volcanic systems) and depositional basins (depositional processes) in the Early Miocene palaeogeographic and palaeotectonic evolution of the central-western Mediterranean region. The results support the proposal of a geodynamic model of this area that considers previously proposed interpretations.</subfield>
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   <subfield code="a">Springer-Verlag Berlin Heidelberg, 2015</subfield>
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   <subfield code="a">Stratigraphy</subfield>
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   <subfield code="a">Guerrera</subfield>
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   <subfield code="u">Dipartimento di Scienze della Terra, della Vita e dell'Ambiente, (DiSTeVA), Università degli Studi di Urbino &quot;Carlo Bo”, Campus Scientifico &quot;Enrico Mattei'', 61029, Urbino, Italy</subfield>
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   <subfield code="a">Martín-Martín</subfield>
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