Cataclastic and crystal-plastic deformation in shallow mantle-wedge serpentinite controlled by cyclic changes in pore fluid pressures

Episodic tremor and slip (ETS) events in the forearc mantle wedge of a warm subduction zone may reflect mixed brittle-ductile deformation of serpentinite in association with high pore fluid pressures. To understand deformation mechanisms and processes occurring in the hydrated mantle wedge, we examined in the Sanbagawa metamorphic belt, SW Japan, an antigorite serpentinite shear zone derived from mantle wedge that was formed under pressure and temperature conditions that correspond to the ETS regions. The serpentinite underwent multiple extensional (mode I) and extensional-shear (mode I-II) failure events at supralithostatic pore fluid pressures (P-f). Such failure events led to drops in P-f (several MPa) and formation of a distributed 'fault-fracture mesh'. Antigorite precipitation in the fracture openings contributed to an increase in P-f until the failure condition was reached again, and thereby antigorite kinetics controlled the recurrence interval of seismic events. We also suggest that under the low-P-f conditions that facilitate intracrystalline plasticity rather than cataclasis, the newly precipitated antigorite aggregates (localized along shear bands) deform by dislocation creep at a high strain rate and high shear stress, resulting in the transient, accelerated viscous creep that may characterize slow slip transients. (C) 2021 Elsevier B.V. All rights reserved.

Automated summary

Episodic tremor and slip events in the forearc mantle wedge of warm subduction zones may be caused by mixed brittle-ductile deformation of serpentinite and high pore fluid pressures. In a study conducted in the Sanbagawa metamorphic belt in SW Japan, it was found that serpentinite experienced multiple extensional and extensional-shear failure events at supralithostatic pore fluid pressures, leading to drops in fluid pressure and formation of a distributed fault-fracture mesh. The presence of antigorite precipitation in fracture openings contributed to an increase in fluid pressure until the failure condition was reached again, controlling the recurrence interval of seismic events.