Subduction erosion occurs at all convergent plate boundaries, even if they are also
accretionary margins. Frontal subduction erosion results from a combination of erosion and …

Subduction erosion, which occurs at all convergent plate boundaries associated with
magmatic arcs formed on crystalline forearc basement, is an important process for chemical …

Tectonic or subduction erosion refers to the removal of upper-plate material from the forearc
at convergent margins. Subduction erosion has been suggested to represent a major …

Subduction erosion shapes at least half of the world's convergent margins. However, its
rates, and modes as well as spatial and temporal variation are poorly understood. Based on …

Documenting the mass flux through convergent plate margins is important to the
understanding of petrogenesis in arc settings and to the origin of the continental crust, since …

Abstract Integrated Ocean Drilling Program (IODP) Expedition 334 to southern Costa Rica,
Central America, documented unprecedented subduction erosion in an area of active …

The dynamics of subduction under an active margin are analysed by using a 2D‐coupled
petrological–thermomechanical numerical model of an oceanic–continental subduction …

Arc magmatism at subduction zones (SZs) most voluminously supplies juvenile igneous
material to build rafts of continental and intra-oceanic or island arc (CIA) crust. Return or …

At ocean margins where two plates converge, the oceanic plate sinks or is subducted
beneath an upper one topped by a layer of terrestrial crust. This crust is constructed of …

Convergent plate boundaries accommodate intraplate displacement within a∼ 100–1000 m
thick shear zone. Marine geophysicists typically define this zone, the subduction channel …