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

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Mechanics, Structure and Evolution of Fault Zones978-3-0346-0138-2Series ISSN 2504-3625 Series E-ISSN 2504-3633

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https://doi.org/10.1007/978-3-0346-0138-2Borehole; Fault Surfaces; Fault Zones; Topography; development; earthquake; environment; evolution; fault; fa

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Mechanics, Structure and Evolution of Fault Zones,gths and usually have complex geometries including bends, jogs, and intersections. The material around these complexities is subjected to large stress concentrations, which lead during continuing deformation to the generation of new fracture and granular damage with an associated evolution of the el

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Segmentation along Strike-Slip Faults Revisited,zones and the capacity of fault seal. Furthermore, segment interactions and coalescence are the fundamental processes for fault growth. To contribute to this end, we investigated the architecture of strike-slip faults by combining field observations in the Valley of Fire State Park, Nevada, and the

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Influence of Outcrop Scale Fractures on the Effective Stiffness of Fault Damage Zone Rocks,of mesoscopic (outcrop-scale) damage zone fractures on the effective stiffness of the fault zone rocks. The Bear Creek fault zones were active at depths between 4 and 15 km and localize mesoscopic off-fault damage into tabular zones between two subparallel boundary faults, producing a fracture-induc

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,Geometry of the Nojima Fault at Nojima-Hirabayashi, Japan — II. Microstructures and their Implicatiation features that explain their measured present-day strengths and permeabilities and provide insight on the evolution of these properties in the fault zone. The least deformed damage-zone rocks contain two sets of nearly perpendicular (60–90° angles), roughly vertical fractures that are concentra

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The Energetics of Cataclasis Based on Breakage Mechanics,etween the energetics and the micromechanics that drive the process of confined comminution. Given this ability, our model not only describes the entire stress-strain response of the material, but also connects this response to predicting the evolution of the grain size distribution. The latter fact