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 …

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 …

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

During the past five decades, numerical modeling of subduction, one of the most
challenging and captivating geodynamic processes, remained in the core of geodynamic …

We develop a 3‐D isotropic shear velocity model for the Alaska subduction zone using data
from seafloor and land‐based seismographs to investigate along‐strike variations in …

The processes occurring on the Earth are controlled by several gradients. The surface of the
Planet is featured by complex geological patterns produced by both endogenous and …

This paper briefly reviews the magmatic manifestations of volcanic arcs and aspects of how
such magmas form. Common concepts about “how subduction zones work” are reassessed …

Volcanoes represent one of the most critical geological settings for hazard modelling due to
their propensity to both unpredictably erupt and collapse, even in times of quiescence …

Subduction is a crucial part of the long‐term water and carbon cycling between Earth's
exosphere and interior. However, there is broad disagreement over how much water and …

Melt and heat transfer in the upper mantle play a crucial role in the multi-scale evolution of
the lithospheric upper mantle. However, the retention time of large amount of melt in the …