# Insight into the microphysics of antigorite deformation from spherical nanoindentation

## TL;DR

This study uses spherical nanoindentation to investigate the deformation mechanisms of antigorite, revealing that high-pressure deformation is dominated by shear crack sliding rather than dislocation activity, with implications for subduction zone mechanics.

## Contribution

It provides the first detailed nanoindentation analysis of antigorite's microphysical deformation behavior, proposing a crack sliding model for high-pressure ductile deformation.

## Key findings

- Deformation involves elastic loading, yield, and strain hardening.
- Yield stress varies with crystal orientation, lower parallel to basal plane.
- Deformation is dominated by shear crack sliding, not dislocation activity.

## Abstract

The mechanical behavior of antigorite strongly influences the strength and deformation of the subduction interface. Although there is microstructural evidence elucidating the nature of brittle deformation at low pressures, there is often conflicting evidence regarding the potential for plastic deformation in the ductile regime at higher pressures. Here, we present a series of spherical nanoindentation experiments on aggregates of natural antigorite. These experiments effectively investigate the single-crystal mechanical behavior because the volume of deformed material is significantly smaller than the grain size. Individual indents reveal elastic loading followed by yield and strain hardening. The magnitude of the yield stress is a function of crystal orientation, with lower values associated with indents parallel to the basal plane. Unloading paths reveal more strain recovery than expected for purely elastic unloading. The magnitude of inelastic strain recovery is highest for indents parallel to the basal plane. We also imposed indents with cyclical loading paths, and observed strain energy dissipation during unloading-loading cycles conducted up to a fixed maximum indentation load and depth. The magnitude of this dissipated strain energy was highest for indents parallel to the basal plane. Subsequent scanning electron microscopy revealed surface impressions accommodated by shear cracks and a general lack of lattice misorientation around indents, indicating the absence of dislocations. Based on these observations, we suggest that antigorite deformation at high pressures is dominated by sliding on shear cracks. We develop a microphysical model that is able to quantitatively explain the Young's modulus and dissipated strain energy data during cyclic loading experiments, based on either frictional or cohesive sliding of an array of cracks contained in the basal plane.