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 …

Deep-seated slow slip and tremor (SST), including slow slip events, episodic tremor and
slip, and low-frequency earthquakes, occur downdip of the seismogenic zone of numerous …

The Alps are amongst the best subduction archives in the world, with abundant blueschists
and eclogites preserving fragments of mantle, gabbros, thinned continental margin and …

Assessing the size of a former ocean of which only remnants are found in mountain belts is
challenging but crucial to understanding subduction and exhumation processes. Here we …

The thermal evolution of subducting slabs controls a range of subduction processes, yet we
lack a robust understanding of how thermal structure develops over a subduction zone's …

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 thermal structure of subduction zones is fundamental to our understanding of the
physical and chemical processes that occur at active convergent plate margins. These …

Abstract The Indo-Burma Ranges form an enigmatic mountain belt, with fragments of
evidence for an early accretionary history (Jurassic Jade belt HP-LT metamorphism; Early …

Abstract Models of orogens identify subduction of oceanic crust as the key mechanism
leading to continental collision. Such models, based inter alia on thermobarometric and …

Fragments of subducted slow-spreading oceanic lithosphere are exposed continuously in
the Liguro-Piemont domain of the Western Alps. By combining new and literature …