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Updated: Sep 19, 2025

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The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults
Published on: November 6, 2021
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Stick-slip from heterogeneous Coulomb friction.
Maryam Alghannam1, Jan M Nordbotten2, Ruben Juanes1
1Massachusetts Institute of Technology, Department of Civil and Environmental Engineering, Cambridge, Massachusetts, USA.
Physical Review. E
|June 19, 2025
Summary
Irregular fault surfaces create position-dependent friction, explaining diverse seismic events like fault creep and earthquakes. This friction heterogeneity alone can model complex fault slip behaviors.
Area of Science:
- Geophysics
- Earth Sciences
- Seismology
Background:
- Stick-slip fault behavior is traditionally explained by velocity-dependent and time-dependent friction.
- Existing models inadequately address position-dependent friction, crucial for complex natural fault zones.
Purpose of the Study:
- To investigate the role of position-dependent friction in fault slip dynamics.
- To demonstrate how surface irregularities lead to heterogeneous friction along faults.
Main Methods:
- Simulated dynamic interactions between irregular surfaces to model Coulomb friction heterogeneity.
- Employed a spring-slider model for dynamic simulations of fault slip.
Main Results:
- Demonstrated that surface irregularities generate heterogeneous Coulomb friction.
- Showed that friction heterogeneity alone can reproduce various stick-slip phenomena.
Conclusions:
- Position-dependent friction is a key factor in understanding complex fault behaviors.
- Heterogeneous Coulomb friction can explain phenomena ranging from fault creep to different earthquake types and slow slip events.
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