Mineral-hosted melt inclusions have become an important source of information on
magmatic processes. As the number of melt inclusion studies increases, so does the need to …

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

Experiment and observation have established the centrality of oxygen fugacity (f O 2) to
determining the course of igneous differentiation, and so the development and application of …

We have re-evaluated mantle potential temperature estimates for the North Atlantic Igneous
Province (NAIP). Temperature estimates involving olivine addition to pillow-lava glasses are …

Deep carbon cycle is crucial for mantle dynamics and maintaining Earth's habitability.
Recycled carbonates are a strong oxidant in mantle carbon-iron redox reactions, leading to …

The behavior of C, H, and S in the solid Earth depends on their oxidation states, which are
related to oxygen fugacity (f O2). Volcanic degassing is a source of these elements to Earth's …

The concentration of carbon in primary mid‐ocean ridge basalts (MORBs), and the
associated fluxes of CO2 outgassed at ocean ridges, is examined through new data …

Volcanic emissions link the oxidation state of the Earth's mantle to the composition of the
atmosphere. Whether the oxidation state of an ascending magma follows a redox buffer …

The oxidation state of a basaltic liquid may be obtained from the average valence state of Fe
in its quenched glass. Suitable glasses are widely available from the basalts erupted at Mid …

From oxic atmosphere to metallic core, the Earth's components are broadly stratified with
respect to oxygen fugacity. A simple picture of reducing oxygen fugacity with depth may be …