Post-collisional strongly peraluminous granites

PJ Sylvester - lithos, 1998 - Elsevier
Strongly peraluminous (SP) granites have formed as a result of post-collisional processes in
various orogens. Inhigh-pressure'collisions such as the European Alps and Himalayas, post …

Magmatism, mantle evolution and geodynamics at the converging plate margins of Italy

A Peccerillo, ML Frezzotti - Journal of the Geological Society, 2015 - lyellcollection.org
The Plio-Quaternary magmatism in the Tyrrhenian Sea area exhibits wide compositional
variations, which cover almost entirely those observed for volcanic rocks worldwide. Some …

The geochemistry of volcanic rocks from Pantelleria Island, Sicily Channel: petrogenesis and characteristics of the mantle source region

L Civetta, MD 'Antonio, G Orsi, GR Tilton - Journal of Petrology, 1998 - academic.oup.com
Major and trace element, Sr–Nd–Pb isotope and mineral chemical data are presented for
mafic and felsic volcanic rocks from the island of Pantelleria. The mafic rocks, mostly basalts …

Source contamination and mantle heterogeneity in the genesis of Italian potassic and ultrapotassic volcanic rocks: Sr–Nd–Pb isotope data from Roman Province and …

S Conticelli, M D'Antonio, L Pinarelli, L Civetta - Mineralogy and Petrology, 2002 - Springer
The Tyrrhenian border of the Italian peninsula has been the site of intense magmatism from
Pliocene to recent times. Although calc-alkaline, potassic and ultrapotassic volcanism …

Volcanological and petrological evolution of Vulcano island (Aeolian Arc, southern Tyrrhenian Sea)

G De Astis, L La Volpe, A Peccerillo… - Journal of Geophysical …, 1997 - Wiley Online Library
Petrological and geochemical data are reported for volcanic rocks from Vulcano island. The
subaerial volcanism (120 ka to present) built up a NW‐SE elongated composite structure …

Geology, volcanic history and petrology of Vulcano (central Aeolian archipelago)

G De Astis, F Lucchi, P Dellino, L La Volpe, CA Tranne… - 2013 - pubs.geoscienceworld.org
Vulcano is an active NW–SE-elongated composite volcano located in the central Aeolian
archipelago. Based on available radiometric ages and tephrochronology, the exposed …

U–Pb zircon and monazite geochronology of Variscan magmatism related to syn-convergence extension in Central Northern Portugal

BV Aguado, MR Azevedo, U Schaltegger, JRM Catalán… - Lithos, 2005 - Elsevier
The Viseu area is located in the Central Iberian Zone of the Iberian Variscan Belt and hosts
numerous post-thickening, collision-related granitoids intruded into upper and middle crustal …

Geochemical and isotopic (Nd–Pb–Sr–O) variations bearing on the genesis of volcanic rocks from Vesuvius, Italy

RA Ayuso, B De Vivo, G Rolandi, RR Seal II… - Journal of volcanology …, 1998 - Elsevier
Alkaline volcanism produced by Monte Somma–Vesuvius volcano includes explosive
plinian and subplinian activity in addition to effusive lava flows. Pumice, scoria, and lava …

[PDF][PDF] The Calabria-Peloritani Orogen, a composite terrane in Central Mediterranean; its overall architecture and geodynamic significance for a pre-Alpine scenario …

R Cirrincione, E Fazio, P Fiannacca… - Periodico di …, 2015 - researchgate.net
Abstract The Calabria-Peloritani Orogen is an arcuate segment of the peri-Mediterranean
orogenic Alpine nappe system that comprises the whole Calabria and the north-eastern …

Petrology and geochemistry of volcanic rocks from the island of Panarea: implications for mantle evolution beneath the Aeolian island arc (southern Tyrrhenian sea)

N Calanchi, A Peccerillo, CA Tranne, F Lucchini… - Journal of Volcanology …, 2002 - Elsevier
Major, trace element and radiogenic isotope (Sr, Nd, Pb) data are reported for a suite of
rocks from the Panarea volcano, a large structure that is largely hidden below sea level and …