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 …

Serpentinization is a key phenomenon for understanding the geodynamics of subduction
zones in the 10–200 km depth range. Serpentines are a major water carrier, and their …

A model for the incorporation of alumina in FeO–MgO–Al 2 O 3–SiO 2–H 2 O (FMASH)
serpentinites has been developed by considering ideal Tschermak (Al 2 Mg− 1 Si− 1) solid …

Abstract The southwestern Tianshan (China) metamorphic belt records high-pressure (HP)
to ultrahigh-pressure (UHP) conditions corresponding to a cold oceanic subduction-zone …

Mesozoic lithological successions of the Alborán domain record two rifting events. An initial
Triassic rifting stage is characterized by thick stratigraphic successions showing typical …

Using first principle simulations we calculated the elasticity of chlorite. At a density ρ~ 2.60 g
cm− 3, the elastic constant tensor reveals significant elastic anisotropy: VP~ 27%, VS1 …

Climate is regulated by the carbonate–silicate cycle in which slab outgassing of C into deep
fluids and volcanic degassing of CO 2 into the atmosphere are an important part. However …

Double seismic zones (DSZs) are a feature of some subducting slabs, where intermediate-
depth earthquakes (~ 70–300 km) align along two separate planes. The upper seismic …

Antigorite occurs at seismogenic depth along plate boundary shear zones, particularly in
subduction and oceanic transform settings, and has been suggested to control a low …

The transition between antigorite‐serpentinite and chlorite‐harzburgite at Cerro del Almirez
(Betic Cordillera, Southern Spain) exceptionally marks in the field the front of antigorite …