During the Cenozoic widespread anorogenic magmatism, unrelated to recent supra-
subduction zone modification of its mantle source, developed within the Mediterranean and …

It is widely recognized that hydrous minerals are involved in a number of geochemical
processes in the Earth's mantle (Michael 1988; Thompson 1992; Schmidt and Poli 1998) …

We present a geodynamic reconstruction of the Central–Western Mediterranean and
neighboring areas during the last 50Myr, including magmatological and tectonic …

Subducted crust refertilizes the subarc mantle wedge as well as the deep convecting mantle.
In the subarc region, mass transfer occurs mainly through fluids, melts, or supercritical …

We have experimentally investigated the fluid-absent melting of a phlogopite peridotite at
1.0 GPa (1000–1300° C) to understand the source of K 2 O-and SiO 2-rich magmas that …

Melting experiments have been performed at 3 GPa, between 1150 and 1450° C, on a
phlogopite-peridotite source in the garnet stability field. We succeeded to extract and …

Melting experiments on ultramafic rocks rich in the hydrous minerals phlogopite or
phlogopite+ K-richterite, some including 5% of accessory phases, have been conducted at …

Primitive, high-K minettes and basanites erupted during the Pleistocene from cinder cones
on the flanks of the Colima Volcanic Complex in the western Trans-Mexican Volcanic Belt …

This paper presents field, geochemical and isotopic (Sr, Nd, Pb) results on basalts from the
Antipodes, Campbell and Chatham Islands, New Zealand. New 40Ar/39Ar age …

Abstract Upper Cretaceous–Miocene alkaline SiO2-undersaturated volcanic rocks in the
southern Central European Volcanic Province (CEVP) comprise two distinct rock series:(i) …