The Role of Shear Fabric in Controlling Breakdown Processes During Laboratory Slow‐Slip Events

Understanding the physical mechanisms at the origin of slow‐slip events has been proven a very challenging task. In particular, little is known on the role of fault heterogeneity during slow slip. In this study, we provide evidences that fault fabric controls slip velocity time histories during slow...

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Veröffentlicht in:	Journal of geophysical research. Solid earth 2020-11, Vol.125 (11), p.n/a
Hauptverfasser:	Scuderi, Marco M., Tinti, Elisa, Cocco, Massimo, Collettini, Cristiano
Format:	Artikel
Sprache:	eng
Schlagworte:	Acceleration Anhydrite Breakdown Deceleration Deformation Dolomite Dolostone Fabrics Friction Geophysics Heterogeneity Laboratories Mechanics Microstructure Quartz RSF friction Shear zone Slip velocity slip velocity function slow‐slip events Velocity
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