The emerging concept of a magma reservoir is one in which regions containing melt extend
from the source of magma generation to the surface. The reservoir may contain regions of …

We extracted all volcanic arc rock analyses calculated to be in equilibrium with mantle
olivine from the global georoc database. This results in 938 primitive melt compositions from …

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 …

Melt extraction from the partially molten mantle is among the fundamental processes
sha** the solid Earth today and over geological time. A diversity of properties and …

Continental arcs in Cordilleran orogenic systems display episodic changes in magma
production rate, alternating between flare ups (70–90 km 3 km− 1 Myr− 1) and lulls (< 20 km …

Quantification of fluid generation during contact metamorphism of shale is important for the
understanding of metamorphic processes, fluid flow in sedimentary basins and perturbations …

A better understanding of the subduction zone fluid cycle and its chemical–mechanical
feedback requires in-depth knowledge about how fluids flow within and out of descending …

Many unresolved questions in geodynamics revolve around the physical behaviour of the
two-phase system of a silicate melt percolating through and interacting with a tectonically …

The modification of magma through mixing or through assimilation of country rocks is
commonly inferred from various chemical and isotopic features of magmatic rock suites and …

Melt extraction from the Earth's mantle requires some form of channelized flow to produce
the observed disequilibrium between the crust-forming lavas and their mantle sources. In …