Titlebook: Mechanics, Structure and Evolution of Fault Zones; Yehuda Ben-Zion,Charles Sammis Book 2010 Birkh?user Basel 2010 Borehole.Fault Surfaces.

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,Geometry of the Nojima Fault at Nojima-Hirabayashi, Japan — I. A Simple Damage Structure Inferred f with the fault zone width inferred from trapped seismic wave analysis and other evidence. The fault zone core or shear axis contains clays with permeabilities of approximately 0.1 to 1 microdarcy at 50 MPa effective confining pressure (10 to 30 microdarcy at . pressures). Within a few meters of the

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Nonplanar Faults: Mechanics of Slip and Off-fault Damage,ive secondary faults. Predicted rates of stress relaxation with distance from major faults with random fractal roughness follow a power-law relationship that is consistent with reported clustering of background seismicity up to 15 kilometers from faults.

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Landslides, Ice Quakes, Earthquakes: A Thermodynamic Approach to Surface Instabilities,rring at rates in the order of 10. to 10. s.. We discuss these processes using examples of landslides and ice quakes or glacial surges. We will then illustrate how the mechanical mechanisms derived from these near-surface processes can be applied to deformation near the base of the seismogenic crust

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