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Updated: Feb 2, 2026

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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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Similarities between mode III crack growth patterns and strike-slip faults
T Cambonie1, Y Klinger2, V Lazarus3
1ENTPE, LTDS, Univ Lyon, UMR CNRS 5513, 3 rue Maurice Audin, 69518 Vaulx en Velin Cedex, France.
Summary
Strike-slip faults form segments due to crack propagation in Earth's crust, mimicking mode III fracture mechanics. This study investigates this brittle fracture scenario using experiments and theory.
Area of Science:
- Geophysics
- Earth Science
- Fracture Mechanics
Background:
- Strike-slip faults exhibit segmented, non-linear geometries.
- The origin of fault segmentation remains a key question in tectonics.
Purpose of the Study:
- To investigate the hypothesis that fault segmentation results from bottom-up crack propagation.
- To explore the role of mode III loading in brittle fracture of the Earth's crust.
Main Methods:
- Conducting physical model experiments simulating crack propagation.
- Developing theoretical explanations within the framework of brittle fracture mechanics.
Main Results:
- Model experiments demonstrate the formation of segmented structures consistent with fault geometries.
- Theoretical analysis supports the plausibility of mode III loading driving segmentation.
Conclusions:
- Fault segmentation can be explained by a crack propagation model under mode III loading.
- This fracture mechanics approach offers new insights into earthquake and fault dynamics.
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