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

DOI :

10.3791/62821-v

7:39 min

November 6th, 2021

November 6th, 2021

2,793 Views

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

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

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