Inclusions of basaltic melt trapped inside of olivine phenocrysts during igneous
crystallization provide a rich, crystal-scale record of magmatic processes ranging from …

The timing of delivery and the types of body that contributed volatiles to the terrestrial planets
remain highly debated,. For example, it is unknown if differentiated bodies, such as that …

The amount of water dissolved in magmas at depth beneath volcanoes is fundamental to a
wide range of magmatic and eruptive processes due to water's dominant control on magma …

Despite the strong theoretical basis for the importance of magma decompression rate in
modulating the dynamics of explosive basaltic eruptions, few measurements exist. Here, we …

The fate of highly volatile elements (H, C, F, Cl and S) during planetary accretion and
differentiation is debated. Recent analyses of water in non-carbonaceous chondrites (RC …

Processes of magma generation and transportation in global mid‐ocean ridges are key to
understanding lithospheric architecture at divergent plate boundaries. These magma …

The rate at which H+ moves into, through, and out of olivine is of great interest for
understanding the deep water cycle, assessing the fidelity of olivine-hosted melt inclusions …

Despite its increasing application to estimate magma decompression rates for explosive
eruptions, the embayment speedometer has long awaited critical experimental evaluation …

Glasses quenched from relatively undegassed ocean island magmas erupted from
volcanoes at Iceland, Hawaii, the Canary Islands, and Erebus have elevated Fe 3+/∑ Fe …

Volatile measurements in mineral-hosted sealed melt inclusions, and open-ended
embayments, have previously been used to study magma ascent dynamics in large rhyolitic …