Titlebook: Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part I; Mitsuhiro Matsu’ura,Peter Mora,Xiang-chu Yin Book

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Experimental Study of the Process Zone, Nucleation Zone and Plastic Area of Earthquakes by the Shado of about 30o. Using this sample and by means of shadow optical method of caustics and microcrack location, the process zone, nucleation zone and plastic area of earthquakes were studied experimentally, and the strain variation in the shadow area was monitored. From the result, we comprehend the fol

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Simulation of the Influence of Rate- and State-dependent Friction on the Macroscopic Behavior of Comfault gouge zones. One important aspect of this is the interaction between the friction law governing the behavior of the fault on the microscopic level and the resulting macroscopic behavior of the fault zone. Numerical simulations offer a possibility to investigate the behavior of faults on many d

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Slip- and Time-dependent Fault Constitutive Law and its Significance in Earthquake Generation Cyclesnt fault constitutive law that rationally unifies the slip-dependent law and the rate-and state-dependent law. In this constitutive law the slip-weakening results from the abrasion of surface asperities that proceeds irreversibly with fault slip. On the other hand, the restoration of shear strength

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Numerical Simulation of Fault Zone Guided Waves: Accuracy and 3-D Effectsseismic head and trapped waves are generated which may be indicative of the structure of fault zones at depth. Observations above several fault zones suggest that they are common features of near fault radiation, yet their interpretation may be highly ambiguous. Analytical methods have been develope

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Regional Seismic Wavefield Computation on a 3-D Heterogeneous Earth Model by Means of Coupled Travelng theory originally developed to perform very low frequency . <~0.01– 0.05 Hz) seismic wavefield computation. It is a Greens function approach for multiple scattering within a defined volume and employs a truncated traveling wave basis set using the locked mode approximation. Interactions between i

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