Open AccessModel quakes in the two‐dimensional wave equation
Author(s) -
Shaw Bruce E.
Publication year - 1997
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/97jb02786
Subject(s) - slip (aerodynamics) , physics , exponential function , wave equation , instability , power law , mechanics , boundary value problem , mathematical analysis , classical mechanics , geology , mathematics , statistics , thermodynamics
This paper presents a new two‐dimensional wave equation model of an earthquake fault. The model generates a complex sequence of slip events on a fault with uniform properties when there is a frictional weakening instability. Previous models of long faults in one and two dimensions had the driving in the bulk, giving the Klein‐Gordon equation in the bulk. Here, I place the driving on the boundary, giving the wave equation in the bulk. The different models are, however, shown to behave similarly. I examine a whole range of frictions, with slip weakening as one end‐member case and velocity weakening as the other end‐member case, and show that they display a generic type of slip complexity: there is an exponential distribution of the largest events and, for sufficient weakening, a power law distribution of small events. With the addition of a viscous‐type friction term on the fault, I show that the results are independent of grid resolution, indicating that continuum limit complexity is achieved.