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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.
This study introduces a new 2D Discrete Element Method (2D-DEM) model for simulating grain fragmentation in fault gouge. The model accurately captures comminution and its effects on fault mechanics.
Area of Science:
- Geophysics
- Computational mechanics
- Materials science
Background:
- Understanding fault gouge behavior is crucial for seismic hazard assessment.
- Traditional models often simplify grain shapes and fracture processes.
Purpose of the Study:
- To develop and validate a 2D Discrete Element Method (2D-DEM) framework for simulating grain fragmentation in fault gouge.
- To investigate the influence of grain properties on comminution and fault zone evolution.
Main Methods:
- Implemented a 2D-DEM model with angular, breakable grains.
- Incorporated realistic fracture mechanics and grain geometries.
- Conducted numerical Brazilian, oedometric, and shear tests; compared with laboratory data.
Main Results:
- Simulations reproduced strain localization, force chain evolution, and grain rounding via chipping.
- Model successfully captured the onset and progression of fragmentation.
- Fragmentation significantly impacts fault strength and mechanical stability.
Conclusions:
- The developed 2D-DEM framework is a robust tool for studying fault gouge fragmentation.
- The model enhances understanding of microstructural evolution and its effect on fault mechanics.
- Provides a foundation for future research on grain size and material property influences.
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