Theory and observations point to the occurrence of magma ponds or oceans in the early
evolution of terrestrial planets and in many early-accreting planetesimals. The apparent …

We consider the current state of our understanding of the rheology of two-phase magmas,
that is suspensions of either bubbles or crystals in a viscous silicate melt. The discussion is …

The largest accumulations of rhyolitic melt in the upper crust occur in voluminous silicic
crystal mushes, which sometimes erupt as unzoned, crystal-rich ignimbrites, but are most …

The Moon is thought to have originated with a magma ocean that produced a plagioclase
flotation crust as solidification proceeded. Ages of anorthositic crust range over at least …

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 …

A comprehensive examination of rheometry theory and its practical applications This
publication enables readers to understand and characterize the flow properties of complex …

The style and evolution of volcanic eruptions are dictated by the fluid mechanics governing
magma ascent. Decompression during ascent causes dissolved volatile species, such as …

Over the past 25 years, our understanding of the physical processes that drive volcanic
eruptions has increased enormously thanks to major advances in computational and …

When considering the rheology of a suspension the fundamental physical aspect to be
quantified is the redistribution of strain between the deformable matrix fraction of the …

The eruptive dynamics of volcanic systems are largely controlled by the viscosity of
deforming magma. Here we report the results of a series of high-temperature, high-pressure …