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Massimo Coltorti Massimo Coltorti. Lorenzo Milani Lorenzo Milani. Leonardo Salvini Leonardo Salvini. Franca Siena Franca Siena. Renzo Tassinari Renzo Tassinari. Slab disruption, mantle circulation, and the opening of the Tyrrhenian basins Author s. Claudio Faccenna Claudio Faccenna. Francesca Funiciello Francesca Funiciello.


Lucia Civetta Lucia Civetta. Monica Moroni Monica Moroni. Claudia Piromallo Claudia Piromallo. Chemical and isotopic composition Os, Pb, Nd, and Sr of Neogene to Quaternary calc-alkalic, shoshonitic, and ultrapotassic mafic rocks from the Italian peninsula: Inferences on the nature of their mantle sources Author s. Sandro Conticelli Sandro Conticelli. Richard W. Carlson Richard W. Elisabeth Widom Elisabeth Widom. Giancarlo Serri Giancarlo Serri. Components and processes in the magma genesis of the Phlegrean Volcanic District, southern Italy Author s.

Cenozoic Volcanism in the Tyrrhenian Sea Region (Advances in Volcanology) | KSA | Souq

Ilenia Arienzo Ilenia Arienzo. Geochemical features and geodynamic significance of the southern Tyrrhenian backarc basin Author s. Teresa Trua Teresa Trua. Michael P. Marani Michael P. A west-east geochemical and isotopic traverse along the volcanism of the Aeolian Island arc, southern Tyrrhenian Sea, Italy: Inferences on mantle source processes Author s. Lorella Francalanci Lorella Francalanci. Riccardo Avanzinelli Riccardo Avanzinelli.

Simone Tommasini Simone Tommasini. Arnd Heuman Arnd Heuman.

Cenozoic Volcanism in the Tyrrhenian Sea Region (E-Book, PDF)

Mount Etna pyroxene as tracer of petrogenetic processes and dynamics of the feeding system Author s. Pietro Armienti Pietro Armienti. Michele Lustrino Michele Lustrino.

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Leone Melluso Leone Melluso. Vincenzo Morra Vincenzo Morra. Cenozoic evolution of the Alboran Domain: A review of the tectonomagmatic models Author s.

  1. Sicily Channel (Sicilian Channel; Strait of Sicily), Italy?
  2. otykunocodax.ml: cenozoic volcanism in the tyrrhenian sea region 2nd edition by angelo peccerillo.
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  4. Miguel Doblas Miguel Doblas. Cenozoic alkaline volcanism of the Atakor massif, Hoggar, Algeria Author s. Bernard Bonin Bernard Bonin. Amel Benhallou Amel Benhallou. Rachid Yahiaoui Rachid Yahiaoui. View Full GeoRef Record. Citing Books via Google Scholar. Close Modal. Silicic rocks are either of crustal anatectic origin or, in most cases, represent mixtures between crustal magmas and various amounts and types of mantle-derived melts.

    Mafic rocks range from calc-alkaline and shoshonitic to potassic and ultrapotassic.

    Plio-Quaternary Volcanism in Italy: Petrology, Geochemistry, Geodynamics

    The Intra-Apennine Province This province comprises a number of small ultrapotassic monogenetic centres e. San Venanzo and Cupaello scattered through the internal zones of Apennines. The best known volcanic rocks consist of ultrapotassic kalsilite-pyroxene and olivine melilitites kamafugites. Incompatible element ratios and isotopic signatures are similar to the Roman Province.

    Intra-Apennine volcanic also include some carbonate-rich pyroclastic rocks, which have been suggested represent carbonatitic magmas. The Roman Province or Latium Province This is part of the belt of potassic and ultrapotassic rocks running from northern Latium to the Neapolitan area, which was defined as the Roman Comagmatic Region by Washington Potassic rocks KS basically consist of trachybasalts, latites and trachytes; ultrapotassic rocks HKS are represented by leucite-tephrites, leucitites to leucite-phonolites.

    Evolved rocks largely prevail over mafic ones, and mainly occur as large ignimbritic sheets and fallout deposits. Isotope compositions are still close to crustal values, but are less extreme than in Tuscany.

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    Incompatible element ratios define distinct trends than those observed for mafic potassic and ultrapotassic rocks of Tuscany. Some low potassium mafic rocks falling in the calc-alkaline compositional field have been also found. On the contrary, ultrapotassic rocks resemble the Colle Albani and other Roman volcanoes. Therefore, the Ernici-Roccamonfina zone is characterised by the coexistence of Roman-type and Campanian-type rocks. The composition of volcanic rocks is variable, from potassic to ultrapotassic; calc-alkaline rocks are also found by borehole drillings and among lithic ejecta.

    The mafic rocks with different enrichment in potassium have comparable concentrations for several incompatible elements and exhibit less extreme isotopic compositions than the equivalent rocks of the Roman Province. Overall, trace element ratios and isotopes basically coincide with the rocks from Stromboli in the eastern Aeolian arc, a volcano consisting of calcalkaline, shoshonitic and potassic rocks. This has led to the conclusion that Vesuvio and adjoining volcanoes do not represent the southern end of the Roman Province but rather the northern extension of the eastern Aeolian arc Peccerillo The Pontine Islands are here considered as part of the Campania Province, although they contain, in addition to Quaternary potassic volcanics, older rocks about 4 Ma-old rhyolites at Ponza which are calc-alkaline in composition and probably related to a Pliocene volcanic arc along the tyrrhenian Sea floor.

    Vulture is petrologically and geochemically different from any other Italian volcano. Such a diversity was early recognised by Washington who established a separate magmatic province for this volcano Apulian Region. The latest activity at Vulture is characterised by explosive eruptions emitting carbonate-rich material Stoppa and Woolley The Aeolian arc Province This is divided into a western, a central and an eastern sector.

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    The western Aeolian arc Alicudi, Filicudi, Salina consists of calc-alkaline rocks with typical island arc signatures. Mafic and intermediate rocks dominate the volcanic sequence, with minor silicic volcanics. The central islands Vulcano and Lipari are dominated by calc-alkaline to shoshonitic mafic to silicic rocks; mafic rocks from this sector show isotopic compositions and incompatible trace element ratios similar to the western islands.

    The eastern arc Panarea and Stromboli consists of calc-alkaline to potassic alkaline rocks. Stromboli shows geochemical and isotopic signatures akin to the Neapolitan volcanoes. The Island of Panarea, located between Stromboli and Lipari, has intermediate characteristics between these two volcanoes.