The slip-rate, state-, temperature-, and normal-stress-dependence of fault frictionKey points

The mechanics of slow-slip events and earthquakes is controlled by the constitutive behavior of rocks in active fault zones, which is sensitive to many factors encompassing lithology, temperature, confining and pore-fluid pressure, and slip-rate, among others. Understanding the frictional properties...

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Bibliographic Details
Main Author: Sylvain Barbot
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2025-08-01
Series:Earthquake Science
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674451925000230
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