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 recognition of slow earthquakes in geodetic and seismological data has transformed the
understanding of how plate motions are accommodated at major plate boundaries. Slow …

We present observations from an exhumed subduction complex that resembles the
environment of modern deep episodic tremor and slow slip (ETS). We focus on the Cycladic …

Slab retreat, slab tearing and interactions of slabs are first-order drivers of the deformation of
the overriding lithosphere. An independent description of the tectonic evolution of the back …

We use structural and microstructural observations from exhumed subduction-related rocks
exposed on Syros Island (Cyclades, Greece) to provide constraints on the length scales and …

High‐P rocks such as eclogite and blueschist are metamorphic markers of palaeo‐
subduction zones, and their formation at high‐P and low‐T (HP–LT) conditions is relatively …

Subduction is a key component of Earth's long‐term sulfur cycle; however, the mechanisms
that drive sulfur from subducting slabs remain elusive. Isotopes are a sensitive indicator of …

Abstract The 40 Ar/39 Ar geochronological technique has significantly contributed to the
study of crustal deformation. However, the frequent occurrence of extraneous argon in high …

Constraining conditions and mechanisms of the early stages of exhumation from within
subduction zones is challenging. Although pressure, temperature, and age can be inferred …