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 …

A quantitative understanding of crystallization and solidification is central to appreciating a
variety of phenomena at the interface between volcanology and petrology. Interpretation of …

A thermodynamic model for estimating the saturation conditions of H 2 O–CO 2 mixed fluids
in multicomponent silicate liquids is described. The model extends the capabilities of rhyolite …

Pressure is one of the key variables that controls magmatic phase equilibria. However,
estimating magma storage pressures from erupted products can be challenging. Various …

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 …

The volatile saturation surface in H2O–CO2–silicate melt systems is modeled by applying
thermodynamic equilibrium between gaseous and liquid volatile components. The whole …

We present crystallization experiments on silicate melt compositions related to the lunar
magma ocean (LMO) and its evolution with cooling. Our approach aims at constraining the …

The origin of iron oxide-apatite deposits is controversial. Silicate liquid immiscibility and
separation of an iron-rich melt has been invoked, but Fe–Ca–P-rich and Si-poor melts …

Crystallization experiments were performed at 200 MPa in the temperature range 1150–
950° C at oxygen fugacities corresponding to the quartz–fayalite–magnetite (QFM) and MnO …

We performed hydrous partial melting experiments at shallow pressures (0.2 GPa) under
slightly oxidizing conditions (NNO oxygen buffer) on oceanic cumulate gabbros drilled by …