Extremely voluminous magmatic systems known as large igneous provinces (LIPs)
punctuate Earth's history, and the gases they release plausibly link large-scale geodynamic …

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 …

Convergent plate boundaries are key sites for continental crustal formation and recycling.
Quantifying the evolution of crustal thickness and paleoelevation along ancient convergent …

The Neogene history of the Central Andes records one of Earth's most productive periods of
high-flux silicic magmatism. Subduction of an aseismic ridge, the Juan Fernández Ridge …

Two distinct igneous differentiation trends–the tholeiitic and calc-alkaline–give rise to Earth's
oceanic and continental crust, respectively. Mantle melting at mid-ocean ridges produces …

Abstract Arclogites, or clinopyroxene-, garnet-, amphibole-, and Fesingle bond Ti oxide-
bearing cumulates and restites (collectively representing residues) to andesitic continental …

Arclogites are eclogite-like rocks formed magmatically as ultramafic residues and cumulates
in the roots of thick arcs (Ducea et al., 2021 companion paper). They are inferred to be …

Shortening of the continental lithosphere is generally accommodated by the growth of
crustal wedges building above megathrusts in the mantle lithosphere. We show that the …

Abstract The Central Andes is a key global location to study the enigmatic relation between
volcanism and plutonism because it has been the site of large ignimbrite-forming eruptions …

Dehydration of the oceanic subducting slab promotes the formation of magmatic arcs, intra-
slab intermediate-depth seismicity, and hydration of the overlying mantle wedge. However …