We compute displacement and stress due to a normal fault by means of two-dimensional plane-strain finite-element analysis. To do so, we apply a system of forces to the fault nodes and develop an iterative algorithm serving to determine the force magnitudes for any slip distribution. As a sample case, we compute the force magnitudes assuming uniform slip on a 10-km two-dimensional normal fault. The numerical model generates displacement and stress fields that compare well with the analytical solution. In fact, we found little difference in displacements (<5%), displacement orientation (<15°), and stress components (<35%, half of which due to slip tolerance). We analyze such misfit, and discuss how the error propagates from displacem...
Closed-form analytic expressions for the displacements and stresses at any point of either of two ho...
We model the coseismic and postseismic stress changes and the surface deformation caused by earthqua...
Wepresent a procedure formatching a displacement field to a given strain field, or vice-versa, over ...
We compute displacement and stress due to a normal fault by means of two-dimensional plane-strain fi...
We used the finite element method (FEM) to simulate the temporal evolution of an inhomogeneous stres...
Given a fault plane and its slip vector, the stress tensor which caused the displacement is sought. ...
Stresses in a block around a dipping fracture simulating a damage zone of a fault are reconstructed ...
in this report are defined according to Fig. 1. sx and sy are the normal stresses in the x and y dir...
We present algorithms for analytically calculating the displacements, strains, and stresses associat...
Vita.The growth of slip along a bend in a fault is analyzed using complex variable techniques of pla...
This research is an investigation into two different aspects of the faulting process. The first part...
The conventional stress inversion methods estimate only four of the six independent parameters of th...
A new approach for identifying past slip events in strike-slip fault systems without geological mark...
The goals of this thesis were to understand the impact of uncertainties and modeling methods on the ...
A number of authors have recently simulated shallow reverse and normal faulting. Oglesby et al (1997...
Closed-form analytic expressions for the displacements and stresses at any point of either of two ho...
We model the coseismic and postseismic stress changes and the surface deformation caused by earthqua...
Wepresent a procedure formatching a displacement field to a given strain field, or vice-versa, over ...
We compute displacement and stress due to a normal fault by means of two-dimensional plane-strain fi...
We used the finite element method (FEM) to simulate the temporal evolution of an inhomogeneous stres...
Given a fault plane and its slip vector, the stress tensor which caused the displacement is sought. ...
Stresses in a block around a dipping fracture simulating a damage zone of a fault are reconstructed ...
in this report are defined according to Fig. 1. sx and sy are the normal stresses in the x and y dir...
We present algorithms for analytically calculating the displacements, strains, and stresses associat...
Vita.The growth of slip along a bend in a fault is analyzed using complex variable techniques of pla...
This research is an investigation into two different aspects of the faulting process. The first part...
The conventional stress inversion methods estimate only four of the six independent parameters of th...
A new approach for identifying past slip events in strike-slip fault systems without geological mark...
The goals of this thesis were to understand the impact of uncertainties and modeling methods on the ...
A number of authors have recently simulated shallow reverse and normal faulting. Oglesby et al (1997...
Closed-form analytic expressions for the displacements and stresses at any point of either of two ho...
We model the coseismic and postseismic stress changes and the surface deformation caused by earthqua...
Wepresent a procedure formatching a displacement field to a given strain field, or vice-versa, over ...