Metamorphic fluids, faults, and shear zones are carriers of carbon from the deep Earth to
shallower reservoirs. Some of these fluids are reduced and transport energy sources, like …

Abstract Deep Slow Slip and Tremors (SSTs) are a combination of transient clusters of
tectonic tremors and slow slip associated with extremely elevated fluid pressures. SSTs are …

Volcanoes represent one of the most critical geological settings for hazard modelling due to
their propensity to both unpredictably erupt and collapse, even in times of quiescence …

Despite the fact that rock textures depend on the 3D spatial distribution of minerals, our
tectono-metamorphic reconstructions are mostly based on a 2D visualisation (ie thin …

Deep tectonic tremor downdip of the seismogenic zone in warm subduction zones is thought
to occur in the region of high fluid pressures. However, the deformation and fluid processes …

Abstract The Yangsan Fault, a long-lived intracontinental fault in SE Korea, exhibits various
slip behaviors, including coseismic slip and aseismic creep. However, there is insufficient …

Fluid overpressure from the water released by subducted sediments and oceanic crust is an
important mechanism for generating earthquakes via brittle failure and frictional instability. If …

Synkinematic phyllosilicates play a key role in controlling the rheology and the style of shear
zones. At the same time, aqueous fluids released by metamorphic dehydration reactions …

Fold-and-thrust belts and accretionary prisms exhibit considerable variability in slip
behaviors along active faults. While numerous studies have investigated fault mechanics …

Maximum shear stress along an active deformation zone marking the subduction plate
interface is important for understanding earthquake phenomena and is an important input …