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

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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요약
Automatic Translation

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

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Keywords: Fabric Frictional Properties Phyllosilicate-rich Tectonic Faults Fluid-assisted Reaction Softening Phyllosilicates Fracturing Permeability Hydrous Fluids Quartz Feldspar Calcite Foliated Microstructures Phyllosilicate Shear Zones Anisotropy Kinematic Indicators Rock Deformation Apparatus Wafers Granular Material
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