Nanoparticles and amorphous materials are common constituents of the shallow sections of active faults. Understanding the conditions at which nanoparticles are produced and their effects on friction can further improve our understanding of fault mechanics and earthquake energy budgets. Here we present the results of 59 rotary shear experiments conducted at room humidity conditions on gouge consisting of mixtures of smectite (Ca-montmorillonite) and quartz. Experiments with 60, 50, 25, 0 wt.% Ca-montmorillonite, were performed to investigate the influence of variable clay content on nanoparticle production and their influence on frictional processes. All experiments were performed at a normal stress of 5 MPa, slip rate of , and at a displace...
Understanding the internal mechanisms controlling fault friction is crucial for understanding seismo...
The presence of smectite (saponite) in fault gouge from the Central Deforming Zone of the San Andrea...
In this multimethodological study, microstructural observations of fault rocks are combined with mic...
Nanoparticles and amorphous materials are common constituents of the shallow sections of active faul...
Smectite clays are the main constituent of slipping zones found in subduction zone faults at shallow...
During earthquake propagation, geologic faults lose their strength, then strengthen as slip slows an...
Smectite clays occur in subduction zone fault cores at shallow depth (approximately 1 km; e.g., Japa...
Identification of the nano-scale to micro-scale mechanochemical processes occurring during fault sli...
Frictional motion between sliding contact surfaces is critical to artificial and natural mechanical ...
Experiments performed on dolomite or Mg-calcite gouges at seismic slip rates (v > 1 m/s) and displac...
To examine whether faults can be lubricated by preexisting and newly formed nanoparticles, we perfor...
Smectite clays occur in subduction zone fault cores at shallow depth (approximately 1 km; e.g., Japa...
We report an experimental and microstructural study of the frictional properties of simulated fault ...
Understanding the internal mechanisms controlling fault friction is crucial for understanding seismo...
The presence of smectite (saponite) in fault gouge from the Central Deforming Zone of the San Andrea...
In this multimethodological study, microstructural observations of fault rocks are combined with mic...
Nanoparticles and amorphous materials are common constituents of the shallow sections of active faul...
Smectite clays are the main constituent of slipping zones found in subduction zone faults at shallow...
During earthquake propagation, geologic faults lose their strength, then strengthen as slip slows an...
Smectite clays occur in subduction zone fault cores at shallow depth (approximately 1 km; e.g., Japa...
Identification of the nano-scale to micro-scale mechanochemical processes occurring during fault sli...
Frictional motion between sliding contact surfaces is critical to artificial and natural mechanical ...
Experiments performed on dolomite or Mg-calcite gouges at seismic slip rates (v > 1 m/s) and displac...
To examine whether faults can be lubricated by preexisting and newly formed nanoparticles, we perfor...
Smectite clays occur in subduction zone fault cores at shallow depth (approximately 1 km; e.g., Japa...
We report an experimental and microstructural study of the frictional properties of simulated fault ...
Understanding the internal mechanisms controlling fault friction is crucial for understanding seismo...
The presence of smectite (saponite) in fault gouge from the Central Deforming Zone of the San Andrea...
In this multimethodological study, microstructural observations of fault rocks are combined with mic...