Titlebook: Involvement of Fluids in Earthquake Ruptures; Field/Experimental D Teruo Yamashita,Akito Tsutsumi Book 2018 Springer Japan KK 2018 Earthqua

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Laboratory and Field Evidence for the Involvement of Fluids in Earthquake Faulting,e for fluid involvement in earthquake faulting over a range of scales should provide valuable constraints on fault modeling and consequently lead to a better understanding of the diversity of earthquake occurrences. A quantitative understanding of fault rupture processes in the presence of fluid rel

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Seismological Implications of Fluid Effect on Earthquake Occurrence,ustal deformation. Such view has been formed by combining results across diverse geophysical observations. Pore fluids will mainly fulfill a twofold role. One is purely mechanical one that occurs through fluid pressure change and the other is mechano-chemical effect such as stress corrosion cracking

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Fluid-Flow Properties of Fault Zones,s. As introduced in Chaps. . and ., changes in fluid pressure within a fault zone mechanically affect the static and dynamic frictional behavior of the fault. The fluid-flow properties of the fault zone play an important role in determining fluid pressures. Since fault-zone structure is the primary

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Poroelastic Effects on Earthquake Rupture,ce of high-pressure fluid. We assume a simple model as much as possible to understand the elementary process that may underlie apparently complex fault slip behavior. In Sect. ., we introduce 1D fault slip model as an example of simple fault model, which will be assumed throughout this chapter. Such

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Effects of Fluid Migration on the Evolution of Seismicity,ose duration is much shorter than the interseismic periods, but much longer than duration times of dynamic fault slips. Typical examples of such activity will be aftershocks and earthquake swarm; seismological observations actually suggest, as described in Chap. ., that high-pressure fluid affects t

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Book 2018und of modeling of faulting coupled with fluid flow in detail. Field and laboratory evidence to suggest the fluid involvement in earthquake faulting is also carefully explained. All of the provided information constitutes together a basic framework of the fault modeling for a comprehensive understan

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and theoretical views of earthquake faulting.Can be read by.This book furnishes state-of-the-art knowledge about how earthquake faulting is coupled with fluid flow. The authors describe the theoretical background of modeling of faulting coupled with fluid flow in detail. Field and laboratory eviden

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Book 2018luid existing at depths. Consequently, modeling study of earthquake faulting coupled with fluid flow is becoming increasingly active as a field of research. This work is aimed at a wide range of readers, and is especially relevant for graduate students and solid-earth researchers who wish to become more familiar with the field..

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