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The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults
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The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults

Article DOI: 10.3791/62821-v • 07:39 min • November 6th, 2021
November 6th, 2021 •
1,4, 2, 1, 1, 3, 1,3, 4, 5
1Dipartimento di Scienze della Terra, Sapienza Università di Roma, 2Dipartimento di Geoscienze, Università di Padova, 3Department of Geoscience, The Pennsylvania State University, 4Istituto Nazionale di Geofisica e Vulcanologia, 5Dipartimento di Scienze Fisiche, della Terra e dell’Ambiente, Università di Siena

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Summary
Automatic Translation

Friction of phyllosilicates-rich faults sheared in their in situ geometry is significantly lower than friction of their powdered equivalents.

Tags

Fabric Frictional Properties Phyllosilicate-rich Tectonic Faults In-situ Geometry Powders Fluid-assisted Reaction Softening Granular Minerals Phyllosilicates Fracturing Processes Permeability Hydrous Fluids Dissolution Platy Phyllosilicates Foliated Microstructures Slip Shear Zones Continuity Outcrop Scale Crustal-scale Faults Anisotropy
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