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 …

High-pressure low-temperature (HP–LT) metamorphic rocks provide invaluable constraints
on the evolution of convergent zones. Based on a worldwide compilation of key information …

This hands-on introduction to numerical geodynamic modelling provides a solid grounding
in the necessary mathematical theory and techniques, including continuum mechanics and …

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

In order to understand how orogens “work,” a quantitative approach demonstrating proof of
concept is essential. Our goal is to reconcile the diverse array of tectonic features observed …

During the last four decades, subduction remained one of the most challenging and
captivating geodynamic processes investigated with numerical techniques. While significant …

Ultrahigh-pressure (UHP) metamorphism refers to mineralogical modifications of continental
and oceanic crustal protoliths±associated mafic-ultramafic rocks initially formed or emplaced …

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

The question of lateral and/or vertical continuity of subducted slabs in active orogens is a hot
topic partly due to poorly resolved tomographic data. The complex slab structure beneath …

The idea that prominent geological phenomena observed in the crust and at the surface may
be caused by the detachment of subducting dense lithosphere has been anticipated by …