A correct description and quantification of the geochemical behaviour of REE+ Y (rare earth
elements and Y) and HFSE (high field strength elements) is a key requirement for modeling …

The peninsular and insular Italy are punctuated by Quaternary volcanoes and their rocks
constitute an important aliquot of the Italian Quaternary sedimentary successions. Also away …

Magmatic systems are the engines driving volcanic eruptions and the source of fluids
responsible for the formation of porphyry-type ore deposits. Sudden variations of pressure …

Nolans-type ore deposits contain REE and Th mineralization hosted in fluorapatite veins.
These veins intrude granulite facies rocks and are surrounded by a diopside selvage …

Genetic models for iron oxide–apatite deposits are controversial and span a spectrum from
orthomagmatic to hydrothermal endmembers. This lack of consensus is rooted in …

Large Ca isotope variations recorded in mantle xenoliths and mantle-derived igneous rocks
have been widely used to decode the origin of mantle heterogeneity, especially to trace …

Carbonate melts produced by partial melting of the carbonated mantle or by liquid
immiscibility from mantle-derived silicate melts provide insights into the deep carbon cycle …

Merapi volcano, Indonesia, is a highly active arc volcano built upon a crustal succession that
includes thick carbonate sequences. Calc-silicate (skarn) xenoliths are frequently found in …

Magma–carbonate interaction is an increasingly recognized process occurring at active
volcanoes worldwide, with implications for the magmatic evolution of the host volcanic …

Abstract Between January 2011 and April 2012, Santorini volcano (Greece) experienced a
period of unrest characterised by the onset of detectable seismicity and caldera-wide uplift …