Fluid saturation and volatile partitioning between melts and hydrous fluids in crustal magmatic systems: The contribution of experimental measurements and solubility …

DR Baker, M Alletti - Earth-Science Reviews, 2012 - Elsevier
This work reviews the experimental constraints on the concentrations of volatiles that can be
expected in melts found in the crust and the saturation of such melts with a separate fluid …

The distribution of volatile elements during rocky planet formation

TA Suer, C Jackson, DS Grewal, C Dalou… - Frontiers in Earth …, 2023 - frontiersin.org
Core segregation and atmosphere formation are two of the major processes that redistribute
the volatile elements—hydrogen (H), carbon (C), nitrogen (N), and sulfur (S)—in and around …

A theoretical framework for volcanic degassing chemistry in a comparative planetology perspective and implications for planetary atmospheres

F Gaillard, B Scaillet - Earth and Planetary Science Letters, 2014 - Elsevier
Magmatic degassing is ubiquitous and enduring, yet its impact on both planetary surficial
chemistry and how it may have varied among planetary systems remains imprecise. A large …

Evidence for multiple magma ocean outgassing and atmospheric loss episodes from mantle noble gases

JM Tucker, S Mukhopadhyay - Earth and Planetary Science Letters, 2014 - Elsevier
The energy associated with giant impacts is large enough to generate global magma
oceans during Earth's accretion. However, geochemical evidence requiring a terrestrial …

New insights into the recent magma dynamics under Campi Flegrei caldera (Italy) from petrological and geochemical evidence

G Buono, A Paonita, L Pappalardo… - Journal of …, 2022 - Wiley Online Library
Abstract The Campi Flegrei caldera is considered the most dangerous volcano in Europe
and is currently in a new phase of unrest (started in 2000 and still ongoing) that has …

[HTML][HTML] Nitrogen, helium, and argon reveal the magmatic signature of fumarole gases and episodes of outgassing from upper-crustal magma reservoirs: The case of …

G Bini, G Chiodini, S Caliro, F Tassi, O Vaselli… - … et Cosmochimica Acta, 2022 - Elsevier
The chemical composition of gases emitted by active volcanoes reflects both magma
degassing and shallower processes, such as fluid-rock hydrothermal interaction and mixing …

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 …

Raman spectroscopy study of COHN speciation in reduced basaltic glasses: Implications for reduced planetary mantles

C Dalou, MM Hirschmann, SD Jacobsen… - … et Cosmochimica Acta, 2019 - Elsevier
To better understand the solution of volatile species in a reduced magma ocean, we identify
via Raman spectroscopy the nature of COHN volatile species dissolved in a series of …

Extensive CO2 degassing in the upper mantle beneath oceanic basaltic volcanoes: First insights from Piton de la Fournaise volcano (La Réunion Island)

G Boudoire, AL Rizzo, A Di Muro, F Grassa… - … et Cosmochimica Acta, 2018 - Elsevier
In spite of its major role on the atmospheric volatile budget, climate, and tracking magmatic
transfers, mantle (CO 2) degassing below volcanoes is still poorly understood. Most of the …

Thermodynamics of multi-component gas–melt equilibrium in magmas: theory, models, and applications

P Papale, R Moretti, A Paonita - Reviews in Mineralogy …, 2022 - pubs.geoscienceworld.org
Volatiles are the fuel and fundamental control for major processes involving magmas and
volcanoes, including magma ascent, magma convection and mixing, magma differentiation …