/

/

フィロケイ酸塩高層断層の摩擦特性における織物の役割

JoVE Journal
Environment
Author Produced

This content is Free Access.

JoVE Journal Environment

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

Please note that all translations are automatically generated. Click here for the English version.

フィロケイ酸塩高層断層の摩擦特性における織物の役割

2,851 Views

•

07:39 min

•

November 06, 2021

DOI:

10.3791/62821-v

DOI:

10.3791/62821-v

•

07:39 min

November 06, 2021

•

1 Views

Cristiano Collettini^1,4, Telemaco Tesei², Fabio Trippetta¹, Marco M. Scuderi¹, Eliza Richardson³, Chris Marone^1,3, Giacomo Pozzi⁴, Cecilia Viti⁵

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

Summary

その場所での形状でせせられたフィロシリケートリッチな断層の摩擦は、粉末等価物の摩擦よりも有意に低い。

Explore More Videos

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

Read Article