Rock Friction and Earthquake Prediction

InhaltsverzeichnisEditors’ Note.A Review of Rock Mechanics Studies in the United States Pertinent to Earthquake Prediction.Volume Changes During Fracture and Frictional Sliding: A Review.Friction of Rocks.A Note on Permeability Changes in Geologic Material Due to Stress.The Effect of Water on Stress Relaxation of Faulted and Unfaulted Sandstone.Mineralogy and Physical Nature of Clay Goug.Rock Friction-Effect of Confing Pressure, Temperature, and Pore Pressure.Aspects of Asperity-Surface Interaction and Surface Damage of Rocks during Experimental Frictional Sliding.Electrical Resistivity Changes in Rocks During Frictional Sliding and Fracture.Seismic Velocity Changes during Fracture and Frictional Sliding.Dilatancy and Fracture Induced Velocity Changes in Rock and their Relation to Frictional Sliding.Velocity Anomalies: An Alternative Explanation Based on Data from Laboratory Experiments.Creep, Stable Sliding, and Premonitory Slip.Time-Dependent Friction and the Mechanics of Stick-Slip.Transient Creep and Semibrittle Behavior of Crystalline Rocks.Effect of Displacement Rate on the Real Area of Contact and Temperatures Generated During Frictional Sliding of Tennessee Sandstone.Fracture Surface Energy of Olivine.Fault and System Stiffnesses and Stick-Slip Phenomena.Experimental Observations of Elastic Wave Radiation Characteristics from Tensile Cracks and Pre-existing Shear Faults.Model Studies of Shear Displacement along a Pre-existing Fault.Small Faults Formed as Deformation Bands in Sandstone.Development of Faults as Zones of Deformation Bands and as Slip Surfaces in Sandstone.Propagation of Slip along Frictional Surfaces.Rupture and Particle Velocity During Frictional Sliding.Nonuniform Friction as a Physical Basis for EarthquakeMechanics.Comments to “Nonuniform Friction as a Physical Basis for Earthquake Mechanics” by A. Nur.