Variation in slip behaviour along megathrusts controlled by multiple physical properties
Megathrusts, faults at the plate interface in subduction zones, exhibit substantial spatiotemporal variability in their slip behaviour. Many previo…
Category: Structural geology
Fault–fracture mesh development produces tectonic tremor in fluid-overpressured serpentinized mantle wedge
Deep tectonic tremor occurs repeatedly at the base of a forearc mantle wedge corner, where a highly fluid-pressurized serpentinite shear zone is th…