Water-fluxed melting, also known as fluid-or water-present melting, is a fundamental process
in the differentiation of continents but its importance has been underestimated in the past 20 …

The origin of granites was once a question solely for petrologists and geochemists. But in
recent years a consensus has emerged that recognizes the essential role of deformation in …

At low temperatures (< 750 C at moderate to high crustal pressures), the production of
sufficient melt to reach the melt connectivity transition (∼ 7 vol%), enabling melt drainage …

Vanguard efforts in forecasting volcanic eruptions are turning to physics-based models,
which require quantitative estimates of magma conditions during pre-eruptive storage …

Abstract A 200,000-yr interval of extreme global warming marked the start of the Eocene
epoch about 55 million years ago. Negative carbon-and oxygen-isotope excursions in …

The third edition of Bubbles, Drops, and Particles in Non-Newtonian Fluids provides
comprehensive coverage of the scientific foundations and the latest advances in particle …

In the absence of global plate tectonics, mantle convection and plume–lithosphere
interaction are the main drivers of surface deformation on Venus. Among documented …

Most plutons have widespread magmatic fabrics, the interpretation of which remains
controversial. We propose a method to constrain likely causes of fabric patterns, the …

The relatively low rates of magma production in island arcs and continental extensional
settings require that the volume of silicic magma involved in large catastrophic caldera …

Significant volume of wet melting requires an influx of H2O-rich volatile phase. In hydrate-
breakdown melting, initial melt accumulation is diffusion-controlled and melt accumulates …