Short-and long-term processes at or close to the subduction plate interface (eg, mineral
transformations, fluid release, seismicity and more generally deformation) might be more …

The discipline of seismology is based on observations of ground motion that are inherently
undersampled in space and time. Our basic understanding of earthquake processes and our …

The Andean volcanic arc includes over 200 potentially active Quaternary volcanoes, and at
least 12 giant caldera/ignimbrite systems, occurring in four separate segments referred to as …

The third edition of this widely acclaimed textbook provides a comprehensive introduction to
all aspects of global tectonics, and includes major revisions to reflect the most significant …

Subduction thrust faults generate earthquakes over a limited depth range. They are aseismic
in their seaward updip portions and landward downdip of a critical point. The seaward …

As the archetype of mountain building in subduction zones, the Central Andes has
constituted an excellent example for investigating mountain-building processes for decades …

It is well recognized that active arc volcanism at nearly all subduction zones requires
temperatures greater than 1200° C in the subarc mantle, despite the underthrusting cool …

We quantitatively analyse the spatial pattern of deformation partitioning and of temporal
accumulation of deformation in the Central Andes (15–26° S) with the aim of identifying …

Integrated magmatic, structural, and geophysical data provide a basis for modeling the
Neogene lithospheric evolution of the high Central Andean Puna-Altiplano Plateau …

Arc magmas globally are H2O-Cl-S–rich and moderately oxidized (ΔFMQ=+ 1 to+ 2) relative
to most other mantle-derived magmas (ΔFMQ≤ 0). Their relatively high oxidation state limits …