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Journal ArticleDOI

Solubility of H2O- and CO2-bearing fluids in tholeiitic basalts at pressures up to 500 MPa

TLDR
In this paper, the solubility of H2O and CO2-bearing fluids in tholeiitic basalts has been investigated experimentally at temperature of 1250 °C and pressures of 50, 100, 200, 300, 400 and 500 MPa.
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This article is published in Chemical Geology.The article was published on 2010-10-01. It has received 181 citations till now. The article focuses on the topics: Melt inclusions & Solubility.

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Sulfur K-edge XANES analysis of natural and synthetic basaltic glasses: Implications for S speciation and S content as function of oxygen fugacity

TL;DR: XANES analyses at the sulfur K-edge were used to determine the oxidation state of S species in natural and synthetic basaltic glasses and to constrain the fO2 conditions for the transition from sulfide (S 2� ) to sulfate (S 6+ ) in silicate melts as mentioned in this paper.
Journal ArticleDOI

An H 2 O–CO 2 mixed fluid saturation model compatible with rhyolite-MELTS

TL;DR: A thermodynamic model for estimating the saturation conditions of H2O-CO2 mixed fluids in multicomponent silicate liquids is described in this paper, where the model is restricted to natural composition liquids over the pressure range 0.3 GPa.
Journal ArticleDOI

New experimental data and semi-empirical parameterization of H2O–CO2 solubility in mafic melts

TL;DR: In this article, a semi-empirical H2O-CO2 solubility model for mafic melts, which employs simplified concepts of gas-melt thermodynamics coupled with a parameterization of both chemical composition and structure of the silicate melt, is presented.
Journal ArticleDOI

Reconstructing the deep CO2 degassing behaviour of large basaltic fissure eruptions

TL;DR: In this article, the mass of volatiles degassed from volcanic eruptions is estimated by comparing the volatile concentrations in undegassed glassy melt inclusions with the volatile concentration in the degassed matrix glass.
Journal ArticleDOI

Experimental Simulation of Closed-System Degassing in the System Basalt–H2O–CO2–S–Cl

TL;DR: In this article, an alternative experimental approach aimed at directly simulating decompression-driven, closed-system degassing of basaltic magma in equilibrium with an H^C^O^S^Cl fluid under oxidized conditions (fO2 of 1·0^2· 4l og units above the Ni^NiO buffer).
References
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Journal ArticleDOI

VOLATILECALC: a silicate melt-H 2 O-CO 2 solution model written in Visual Basic for excel

TL;DR: The VOLATILECALC solution models for the rhyolite-H2O-CO2 and basalt-H 2 O-CO 2 systems at magmatic temperatures and pressures below ∼ 5000 bar are presented in this paper.

Volatiles in subduction zone magmas : concentration and fluxes based on melt inclusion and volcanic gas data

P. J. Wallace
TL;DR: In this paper, the fluxes of volatiles subducted back into the mantle along subduction zones and returned from the mantle to the surface reservoir via magmatism suggests that there is an approximate balance for structurally bound H2O and Cl.
Journal ArticleDOI

Volatiles in subduction zone magmas: concentrations and fluxes based on melt inclusion and volcanic gas data

TL;DR: In this paper, the fluxes of volatiles subducted back into the mantle along subduction zones and returned from the mantle to the surface reservoir via magmatism suggests that there is an approximate balance for structurally bound H2O and Cl.
Journal ArticleDOI

An Experimental Study of Water and Carbon Dioxide Solubilities in Mid-Ocean Ridge Basaltic Liquids. Part I: Calibration and Solubility Models

TL;DR: In this paper, the authors used IR spectroscopy to determine the solubilities of H2O and CO_2 and the nature of their mixing behavior in basaltic liquid at pressures and temperature relevant to seqfloor eruption.
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