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 …

This chapter reviews recycling of boron (B) and its isotopes in subduction zones. It discusses
the profound changes in B concentrations and B isotope ratios of various materials involved …

Oceanic lithosphere carries volatiles, notably water, into the mantle through subduction at
convergent plate boundaries. This subducted water exercises control on the production of …

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

Fluid-rock interaction on oceanic transform faults (OTFs) is important for both the
deformation behavior of the lithosphere and volatile cycling in the Earth. Rocks deformed …

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 …

Geodetically constrained interseismic interplate coupling has been widely used to assess
seismic potential in subduction zones. Modeling interseismic deformation is challenging, as …

Abstract The Transmexican Volcanic Belt (TMVB) is the magmatic expression of one of the
most complex convergent margins on the planet, and as such constitutes a prime location for …

The evolution of atmospheric CO 2 and the pH of the ocean can be reconstructed by the
boron isotopic composition (δ 11 B) of marine carbonates, which is influenced by the δ 11 B …

We imaged the mantle structure beneath northern Sumatra by inverting high‐quality seismic
arrival time data and using a newly developed eikonal equation‐based teleseismic …