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 …

Reconfigurations of magmatic arcs through time have been recognized since pioneering
works, describing inland and trenchward arc migrations or magmatic shut-off lasting for …

This contribution investigates mechanisms controlling subduction development and
stabilization over time (coined as' slabitization'), from a nascent slab to a mature slab …

The thermal structure of subduction zones is fundamental to our understanding of the
physical and chemical processes that occur at active convergent plate margins. These …

Abstract Arc Basalt Simulator version 5 (ABS5) is a forward geochemical and petrological
model that can be used to examine the element mass balance in primary arc magmas …

Under the right circumstances, fluid-fluxed crustal melting occurs, as demonstrated by some
amphibolite-facies migmatites, but the relatively low temperatures involved make this mode …

Mineral grain size in the mantle affects fluid migration by controlling mantle permeability; the
smaller the grain size, the less permeable the mantle is. Mantle shear viscosity also affects …

The weak slab interface controls long-term subduction dynamics. A weak hydrous layer at
the slab interface promotes mechanical decoupling between the forearc mantle and the …

Two‐phase flow, a system where Stokes flow and Darcy flow are coupled, is of great
importance in the Earth's interior, such as in subduction zones, mid‐ocean ridges, and …

Erupted lavas and tephras remain among the best tools we have to ascertain the mantle
processes that give rise to the compositional diversity and spatial distribution of near-primary …