Magma reservoirs play a key role in controlling numerous processes in planetary evolution,
including igneous differentiation and degassing, crustal construction, and volcanism. For …

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 …

This contribution presents a semiempirical model describing the effective relative viscosity of
crystal‐bearing magmas as function of crystal fraction and strain rate. The model was …

This paper presents a model for the genesis of migmatites and granites during orogenic
evolution based on the analysis of several Phanerozoic crustal segments and a review of …

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 …

Our ability to forecast volcanic hazards at active volcanoes stems from our knowledge of
parameters affecting eruption dynamics. Persistent activity displayed by basaltic volcanic …

Heterogeneities in crustal magma chambers are generated by incomplete mixing of different
batches of magmas, precipitation or remelting of solids~ 10–20% denser than surrounding …

Whether a magma body is able to produce eruptions and at what frequency remains a
challenging problem in volcanology as it involves the nonlinear interplay of different …

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

Partially molten rocks, often called a mush, are examples of a hydrogranular mixture where
the dynamics are controlled by both fluid and crystal‐crystal interactions. An obstacle to …