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Updated: Jan 14, 2026

The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults
Published on: November 6, 2021
Angular grain fragmentation with DEM modeling: application to fault gouge shearing
Nathalie Casas1, Guilhem Mollon2, Marco Maria Scuderi1
1Dipartimento di Scienze della Terra, La Sapienza Università di Roma, Rome, Italy.
Abstract:
Understanding grain fragmentation in fault gouge is essential for capturing the mechanical behavior and evolution of fault zones under shear. In this study, we present a 2D Discrete Element Method (2D-DEM) framework that simulates comminution using angular, breakable grains, overcoming limitations of traditional models based on spherical particles. Our approach incorporates realistic fracture mechanics and grain geometries to better represent microstructural evolution during shearing. A series of numerical experiments, including Brazilian, oedometric, and shear tests, were conducted to calibrate the model and examine the roles of grain strength, friction, and Young's modulus. The simulations reproduce key numerical observations such as strain localization, force chain evolution, and grain rounding through chipping mechanisms. Results show that the model captures the onset and progression of fragmentation, as well as its impact on fault strength and mechanical stability. A comparison with a dedicated laboratory experiment is provided. This work provides a robust numerical tool for studying fault gouge behavior and lays the foundation for future studies exploring the influence of initial grain size and material properties on fault mechanics.
Graphical Abstract:
A robust numerical tool with fragmentation for studying fault gouge behavior.
Supplementary Information:
The online version contains supplementary material available at 10.1007/s10035-025-01578-9.
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