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ESAIM: Proc., 2009, Vol. 26, pp. 1-23
DOI: 10.1051/proc/2009002
An inverse problem for faults in elastic half space
Darko VolkovDepartment of Mathematical Sciences, Worcester Polytechnic Institute, Worcester MA 01609, United States;
darko@wpi.edu
Published online: 25 April 2009
Abstract
This paper starts from a model in geophysics for
the quasi static evolution of displacement fields occurring
during the destabilization of fractured plates.
We use the equations of linear elasticity in half space
with traction free conditions on the surface and given tangential
dislocations on the fault. We first discuss the derivation
of the adequate Green's tensor for this problem. We then use this
Green's tensor to obtain a simple and efficient approximation to
the surface displacement field. Next we show how to solve the fault inverse problem from
measurements of surface displacements. We first give the solution in closed form.
We then illustrate it on numerical examples which demonstrate the robustness
of our reconstruction algorithm.
Mathematics Subject Classification. 35P15, 45E99, 74L05, 86A15
Key words: Linear elasticity, Green's tensors in half space, surface displacements, faults in half space, inverse problems.
© EDP Sciences, ESAIM 2009
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