2014
DOI: 10.1016/j.quascirev.2014.04.010
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Major explosive activity in the Monti Sabatini Volcanic District (central Italy) over the 800–390 ka interval: geochronological–geochemical overview and tephrostratigraphic implications

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Cited by 72 publications
(110 citation statements)
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“…7b). The latter ones, according to what were discussed in Marra et al (2014) about the Monti Sabatini products, display longer distance from the origin of the axis, which is consistent with the more differentiated character of their magma Smith et al, 2011). These include the products of Agnano, Astroni, Archiaverno, Pigna San Nicola, Capo Miseno, Baia and Fondi di Baia eruptive centers, which are all located near Pozzuoli (Fig.…”
Section: Ports Of Claudius and Anxursupporting
confidence: 73%
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“…7b). The latter ones, according to what were discussed in Marra et al (2014) about the Monti Sabatini products, display longer distance from the origin of the axis, which is consistent with the more differentiated character of their magma Smith et al, 2011). These include the products of Agnano, Astroni, Archiaverno, Pigna San Nicola, Capo Miseno, Baia and Fondi di Baia eruptive centers, which are all located near Pozzuoli (Fig.…”
Section: Ports Of Claudius and Anxursupporting
confidence: 73%
“…6 we have plotted the Zr/TiO 2 vs Nb/TiO 2 compositions of the products whose pyroclastic-flow deposits are characterized by the presence of black vesicular scoriae within a loose ash matrix. These include the Sutri (Vico's Tufo Rosso a Scorie Nere), Ronciglione and Carbognano formations from Vico volcano (Perini et al, 2004), and the unlithified facies of the Tufo Roso a Scorie Nere from Monti Sabatini (Marra et al, 2014). Comparison of sample SU ANF composition with those of the different volcanic deposits suggests correlation with the Carbognano and Ronciglione Formations.…”
Section: Sutrimentioning
confidence: 94%
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“…The LTGVT is a massive light grey to pale yellow ignimbrite with abundant white lapilli-sized pumice fragments and accretionary lapilli (Karner et al 2001;Masotta et al 2010). Recently Marra et al (2014) determined an age of 546±5 ka for the Tufo Giallo della Via Tiberina eruptive cycle. The cycle encompasses both UTGVT and LTGVT, for which these authors suggest a co-eruptive origin.…”
Section: Geo-volcanological Settingmentioning
confidence: 99%