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 …

We review our understanding of the exsolved volatile phase co-existing with magmas during
pre-eruptive storage at the pressures and temperatures corresponding to crustal magma …

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 …

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 …

Volcanic eruptions can be either slow outpourings of lava or explosive ejections of
fragmented rock. In his Perspective, Dingwell discusses the physical and chemical …

A new and empirical viscosity equation for anhydrous and hydrous natural silicate melts has
been developed using the following formulation: where η is the viscosity, T is the …

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 …

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

An increasing number of studies are being presented demonstrating that volcanic glasses
can be heterogeneous at the nanoscale. These nano-heterogeneities can develop both …

Eruption of the Soufrière Hills Volcano on Montserrat allowed the detailed documentation of
a Pélean dome-forming eruption. Dome growth between November 1995 and March 1998 …