Abstract
The solution of the inverse scattering problem for the one-dimensional Schrödinger equation is given by the Marchenko equation. Recently, a Marchenko-type equation has been derived for three-dimensional (3D) acoustic wave fields, whose solution has been shown to recover the Green's functions from points within the medium to its exterior, using only single-sided scattered data. Here we extend this approach to 3D vectorial wave fields that satisfy the elastodynamic wave equation and recover Green's functions from points interior to an elastic, solid-state medium from purely external and one-sided measurements. The method is demonstrated in a solid-earth-like model to construct Green's functions using only subsurface sources, from earth-surface force and deformation sources and particle velocity and stress measurements.
| Original language | English |
|---|---|
| Article number | 063201 |
| Journal | Physical Review E |
| Volume | 90 |
| Issue number | 6 |
| DOIs | |
| Publication status | Published - 1 Dec 2014 |
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Andrew Curtis
- School of Geosciences - Personal Chair of Mathematical Geoscience
Person: Academic: Research Active
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