An integrated PT-H2O-lattice strain model to quantify the role of clinopyroxene fractionation on REE+ Y and HFSE patterns of mafic alkaline magmas: Application to …

S Mollo, J Blundy, P Scarlato, SP De Cristofaro… - Earth-Science …, 2018 - Elsevier
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 …

Strongly SiO2-undersaturated, CaO-rich kamafugitic Pleistocene magmatism in Central Italy (San Venanzo volcanic complex) and the role of shallow depth limestone …

M Lustrino, S Ronca, A Caracausi, CV Bordenca… - Earth-Science …, 2020 - Elsevier
Abstract The Pleistocene (~ 460–265 ka) San Venanzo volcanic complex belongs to the IAP
(Intra-Apennine Province) in central Italy, which comprises at least four small Pleistocene …

The analysis and interpretation of noble gases in modern hydrothermal systems

Y Sano, TP Fischer - The noble gases as geochemical tracers, 2013 - Springer
This chapter describes the practice in the analysis and interpretation of noble gases in
modern hydrothermal systems, including sample collection and analytical methods …

New mafic magma refilling a quiescent volcano: Evidence from He‐Ne‐Ar isotopes during the 2011–2012 unrest at Santorini, Greece

AL Rizzo, F Barberi, ML Carapezza… - Geochemistry …, 2015 - Wiley Online Library
Abstract In 2011–2012, Santorini was characterized by seismic‐geodetic‐geochemical
unrest, which was unprecedented since the most‐recent eruption occurred in 1950 and led …

Upper mantle scale enrichment of Cenozoic intraplate magmatism in Northeast Asia: He-Sr-Nd-Pb-O isotope geochemistry of the basalts around the Korean peninsula

D Kim, H Lee, MJ Lee, C Park, AL Rizzo - Gondwana Research, 2025 - Elsevier
The Earth's mantle is considered to be geochemically heterogeneous, which is reflected by
the diverse compositions of oceanic island basalts (OIB). The mantle enrichment resulting in …

Geochemical evidence for mixing between fluids exsolved at different depths in the magmatic system of Mt Etna (Italy)

A Paonita, A Caracausi, G Iacono-Marziano… - … et Cosmochimica Acta, 2012 - Elsevier
A 4-year geochemical survey of some fumaroles at the Voragine summit crater of Mt Etna
was performed in combination with synchronous monitoring of peripheral gas emissions at …

Geochemical evidence for a lithospheric origin of the Comoros Archipelago (Indian Ocean) as revealed by ultramafic mantle xenoliths from La Grille volcano

CV Bordenca, B Faccini, A Caracausi, M Coltorti… - Lithos, 2023 - Elsevier
Petrology and fluid inclusions (FI) geochemistry are increasingly used in tandem to constrain
the compositional features and evolution of the lithospheric mantle. In this study, we …

The composition of fluids stored in the central Mexican lithospheric mantle: Inferences from noble gases and CO2 in mantle xenoliths

A Sandoval-Velasquez, AL Rizzo, ML Frezzotti… - Chemical …, 2021 - Elsevier
We present the first isotopic (noble gases and CO 2) characterization of fluid inclusions
coupled to Raman microspectroscopy analyses in mantle xenoliths from Central Mexico, a …

Geochemistry of the mantle source and magma feeding system beneath Turrialba volcano, Costa Rica

A Di Piazza, AL Rizzo, F Barberi, ML Carapezza… - Lithos, 2015 - Elsevier
Turrialba volcano lies in the southern sector of the Central American Volcanic Front (CAVF)
in Costa Rica. The geochemistry of major and trace elements, and Sr and Nd isotopes of a …

Noble gas isotopic systematics of Fe–Ti–V oxide ore-related mafic–ultramafic layered intrusions in the Panxi area, China: The role of recycled oceanic crust in their …

T Hou, Z Zhang, X Ye, J Encarnacion… - … et Cosmochimica Acta, 2011 - Elsevier
Olivine and clinopyroxene grains have been separated from four large Fe–Ti–V oxide ore-
bearing intrusions (Panzhihua, Hongge, Baima and Taihe) in the Panxi area, Emeishan …