Research paperPetrology of final-stage Latera lavas (Vulsini Mts.): Mineralogical, geochemical and Sr-isotopic data and their bearing on the genesis of some potassic magmas in central Italy
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The multi-component mantle source of Roman province ultrapotassic magmas revealed by melt inclusions
2023, Geochimica et Cosmochimica ActaGeothermal fluid circulation in a caldera setting: The Torre Alfina medium enthalpy system (Italy)
2021, GeothermicsCitation Excerpt :The activity of the Vulsini Volcanic District, at the southern margin of the study area, developed in several phases between 0.8 and 0.1 My ago (Fornaseri, 1985; Palladino et al., 2010; Varekamp, 1979) and produced a thick sequence of pyroclastic deposits and lava flows from the five eruptive centers of Paleo-Bolsena, South Vulsini, Bolsena, Latera and Montefiascone (Palladino et al., 2010) covering a wide area between the Radicofani and Tevere-Paglia grabens. The last stages of volcanic activity involved consistent ignimbritic eruptions (Conticelli et al., 1986, 1991) forming calderas whose collapse was controlled by regional fault systems and led to the development the Latera and Bolsena depressions (Acocella et al., 2012). The latter is a complex structure consisting of an inner ring fault, buried within the lake and accommodating a subsidence of about 1000 m (Barberi et al., 1994).
Multiple subduction imprints in the mantle below Italy detected in a single lava flow
2016, Earth and Planetary Science LettersCitation Excerpt :Erupted products of Latera comprise SHO as well as HKS rock types (Conticelli et al., 1991). We focus on samples from various locations across a ca. 12 km long shoshonitic flow (Selva del Lamone, SdL) and from a representative HKS lava from nearby Monte Starnina (Conticelli et al., 1991). The SdL samples (4.8–5.8 wt.
TIMS analysis of Sr and Nd isotopes in melt inclusions from Italian potassium-rich lavas using prototype 10<sup>13</sup>Ω amplifiers
2015, Chemical GeologyCitation Excerpt :The small range in Sr isotope compositions for bulk Latera lavas suggests that the magma became homogenised prior to eruption. These explanations for the isotopic relationships are consistent with earlier petrological evidence for contributions of multiple mantle derived melts to the late-stage effusive and strombolian products of the Latera complex, admixture of a distinct lamproitic component to the shoshonitic magma and for the role of crustal assimilation and the presence of potential assimilants with high 87Sr/86Sr in the subsurface (Ferrara et al., 1986; Varekamp and Kalamarides, 1989; Conticelli et al., 1991). The four melt inclusions in two HKS lava samples from Vulsini and Sabatini volcanic complexes have 87Sr/86Sr ratios that overlap with the data range for bulk lavas reported in the literature (Fig. 8b).