Three-Dimensional Finite Difference Simulation of Fault Dynamics: Rectangular Faults with Fixed Rupture Velocity

Abstract

We analyze three-dimensional finite difference solutions for a simple shear-crack model of faulting to determine the effects of fault length and width on the earthquake slip function. The fault model is dynamic, with only rupture velocity, fault dimensions, and dynamic stress-drop prescribed. The numerical solutions are accurate for frequencies up to 5 Hz, and are combined with asymptotic results for shear cracks in order to characterize the slip function at higher frequencies. Near the hypocenter, the slip velocity exhibits a square root singularity whose intensity increases with hypocentral distance. At distances greater than the fault width, w, growth of the velocity intensity ceases, and the slip function becomes nearly invariant with distance along the fault length. Close-form expressions are developed for the dependence of static slip, slip rise time, and slip velocity intensity on fault geometry. The numerical results imply that uniform-dislocation kinematic earthquake models in which slip is represented by a ramp time-function will under-predict high- frequency ground motion relative to low-frequency ground motion. A further implication of the numerical solutions is that the nature of the in-elastic processes at the advancing edge of a long fault will depend on fault width, but will be independent of rupture length.

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Document Details

Document Type
Technical Report
Publication Date
Sep 01, 1981
Accession Number
ADA110064

Entities

People

  • S. M. Day

Organizations

  • Utility Systems Science and Software (United States)

Tags

Communities of Interest

  • Air Platforms

DTIC Thesaurus Topics

  • Aspect Ratio
  • Equations
  • Frequency
  • Frequency Shift
  • Geometry
  • Leading Edges
  • Mechanics
  • Secondary Waves
  • Shear Modulus
  • Shear Stresses
  • Simulations
  • Sliding Friction
  • Square Roots
  • Stress Intensity Factors
  • Three Dimensional
  • Two Dimensional
  • Wave Propagation

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Finite Element Method (FEM) for solving Partial Differential Equations (PDEs)
  • Seismology