Titlebook: Microscopic and Macroscopic Simulation: Towards Predictive Modelling of the Earthquake Process; Peter Mora,Mitsuhiro Matsu’ura,Jean-Bernar

断断续续

胡言乱语

Extension of the Lattice Solid Model to Incorporate Temperature Related Effectses, particularly considering the high temperatures generated during large slip events. In order to provide a foundation for the study of these heat related effects, the Lattice Solid Model for the study of earthquake dynamics is extended to incorporate the generation and transfer of heat. The therma

gangrene

Hybrid Modelling of Coupled Pore Fluid-solid Deformation Problemsfinite volume formulation for the analysis of the pore fluid and a particle method for the solid in our model. The pore fluid formally occupies the same space as the solid particles. The size of the particles is not necessarily equal to the physical size of materials. A finite volume mesh for the po

fatty-streak

Numerical Simulation of Rock Failure and Earthquake Process on Mesoscopic ScaleThe model consists of a 2-D set of particles linked by three kinds of interactions and arranged into triangular lattice. After the fracture criterion and rules of changes between linking states are given, the particle positions, velocities and accelerations at every time step are calculated using a

frivolous

needle

责难

Dynamic Propagation and Interaction of a Rupture Front on a Planar Fault first that the rupture velocity is controlled by a delicate balance between consumed fracture energy and supplied elastic strain energy. A very sharp boundary in parameter space separates models in which ruptures stop spontaneously from those in which rupture propagates at super-shear speeds. The t

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MAIZE

Spontaneous Rupture Propagation on a Non-planar Fault in 3-D Elastic Mediumtion method (BIEM) in time domain. We removed all singularities in boundary integral equations (BIEs) following the method proposed by . and . (1995, 1998) for a planar fault in a 3-D elastic medium, and analytically evaluated all BIEs for a basic box-like discrete source. As an application of the n

annexation

Constraints on Stress and Friction from Dynamic Rupture Models of the 1994 Northridge, California, Eifference method. The simulations use a rate- and slip-weakening friction law, starting from a range of initial conditions of stress and frictional parameters. A critical balance between initial conditions and friction parameters must be met in order to obtain a moment as well as a final slip distri