Transient Slow Slip Characteristics of Frictional‐Viscous Subduction Megathrust Shear Zones

Transient Slow Slip Characteristics of Frictional‐Viscous Subduction Megathrust Shear Zones

Abstract The deep roots of subduction megathrusts exhibit aseismic slow slip events, commonly accompanied by tectonic tremor. Observations from exhumed rocks suggest this region of the subduction interface is a shear zone with frictional lenses embedded in a viscous matrix. Here, we use numerical mo...

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Bibliographic Details
Main Authors:	Whitney M. Behr, Taras V. Gerya, Claudio Cannizzaro, Robert Blass
Format:	Article
Language:	English
Published:	Wiley 2021-09-01
Series:	AGU Advances
Subjects:	subduction megathrust frictional‐viscous transition episodic tremor and slow slip slow slip events heterogeneous melange subduction interface
Online Access:	https://doi.org/10.1029/2021AV000416

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