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Water in the Earth's interior: distribution and origin
AH Peslier, M Schönbächler, H Busemann… - Space Science …, 2017 - Springer
The concentration and distribution of water in the Earth has influenced its evolution
throughout its history. Even at the trace levels contained in the planet's deep interior (mantle …
throughout its history. Even at the trace levels contained in the planet's deep interior (mantle …
Exsolved volatiles in magma reservoirs
We review our understanding of the exsolved volatile phase co-existing with magmas during
pre-eruptive storage at the pressures and temperatures corresponding to crustal magma …
pre-eruptive storage at the pressures and temperatures corresponding to crustal magma …
The magmatic web beneath Hawai 'i
The deep magmatic architecture of the Hawaiian volcanic system is central to understanding
the transport of magma from the upper mantle to the individual volcanoes. We leverage …
the transport of magma from the upper mantle to the individual volcanoes. We leverage …
The influence of water on melting of mantle peridotite
This experimental study examines the effects of variable concentrations of dissolved H 2 O
on the compositions of silicate melts and their coexisting mineral assemblage of olivine+ …
on the compositions of silicate melts and their coexisting mineral assemblage of olivine+ …
An experimental study of water and carbon dioxide solubilities in mid-ocean ridge basaltic liquids. Part I: calibration and solubility models
JE Dixon, EM Stolper, JR Holloway - Journal of Petrology, 1995 - academic.oup.com
Experiments were conducted to determine the solubilities of H2O and CO2 and the nature of
their mixing behavior in basaltic liquid at pressures and temperature relevant to seqfloor …
their mixing behavior in basaltic liquid at pressures and temperature relevant to seqfloor …
Chemical composition of volcanic gases
R Scarpa, RI Tilling, WF Giggenbach - Monitoring and mitigation of …, 1996 - Springer
The composition of gases released from volcanoes is a function of deep processes, such as
vapor-melt separation during the generation and rise of the magmas, and shallow …
vapor-melt separation during the generation and rise of the magmas, and shallow …
Non-chondritic sulphur isotope composition of the terrestrial mantle
Core–mantle differentiation is the largest event experienced by a growing planet during its
early history. Terrestrial core segregation imprinted the residual mantle composition by …
early history. Terrestrial core segregation imprinted the residual mantle composition by …
Volatile abundances in basaltic magmas and their degassing paths tracked by melt inclusions
N Metrich, PJ Wallace - Reviews in mineralogy and …, 2008 - pubs.geoscienceworld.org
The abundances of CO2, H2O, S and halogens dissolved in basaltic magmas are strongly
variable because their solubilities and ability to be fractionated in the vapor phase depend …
variable because their solubilities and ability to be fractionated in the vapor phase depend …
Sulfur in basaltic magmas
P Wallace, ISE Carmichael - Geochimica et Cosmochimica Acta, 1992 - Elsevier
The concentration of S in basaltic magmas at 1 atm pressure is strongly dependent on
temperature, the fugacities of oxygen (ƒ O 2) and sulfur (ƒ S 2), and bulk composition …
temperature, the fugacities of oxygen (ƒ O 2) and sulfur (ƒ S 2), and bulk composition …
The sulfur budget in magmas: evidence from melt inclusions, submarine glasses, and volcanic gas emissions
The major magmatic volatile components—H 2 O, CO 2, S, Cl, and F—play an important role
in the formation, evolution, and eruption of magma. Knowledge of magmatic concentrations …
in the formation, evolution, and eruption of magma. Knowledge of magmatic concentrations …