|
|
||||||||
U.S. GEOLOGICAL SURVEY, MENLO PARK, CALIFORNIA 94025
Abstract
Direct numerical evaluation of shear strain on a fault plane using the representation theorem is not possible because source points near the field point give large and canceling contributions to the integral. The representation theorem for strain can be integrated by parts to obtain an expression valid everywhere and suitable for numerical evaluation on the fault plane. Stress-drop evaluated by this method for the circular dislocation of Keylis-Borok agrees well with the analytic solution.
Footnotes
* Publication authorized by the Director, U.S. Geological Survey.
This article has been cited by other articles:
![]() |
E. Fukuyama and R. Madariaga Integral equation method for plane crack with arbitrary shape in 3D elastic medium Bulletin of the Seismological Society of America, April 1, 1995; 85(2): 614 - 628. [Abstract] [PDF] |
||||
![]() |
J. VIRIEUX and R. MADARIAGA Dynamic faulting studied by a finite difference method Bulletin of the Seismological Society of America, April 1, 1982; 72(2): 345 - 369. [Abstract] [PDF] |
||||
![]() |
J. BOATWRIGHT Quasi-dynamic models of simple earthquakes: Application to an aftershock of the 1975 Oroville, California, earthquake Bulletin of the Seismological Society of America, February 1, 1981; 71(1): 69 - 94. [Abstract] [PDF] |
||||
![]() |
W. H. BAKUN, R. M. STEWART, C. G. BUFE, and S. M. MARKS Implication of seismicity for failure of a section of the San Andreas Fault Bulletin of the Seismological Society of America, February 1, 1980; 70(1): 185 - 201. [Abstract] [PDF] |
||||
![]() |
S. K. SINGH Slip and stress drop on a circular fault Bulletin of the Seismological Society of America, April 1, 1977; 67(2): 279 - 284. [Abstract] [PDF] |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |