Isotropic angle-domain elastic reverse-time migration |

**Jia Yan and Paul Sava**

*Center for Wave Phenomena*

Colorado School of Mines

Multicomponent data are not usually processed with specifically
designed procedures, but with procedures analogous to the ones used
for single-component data. In isotropic media, the vertical
and horizontal components of the data are commonly taken as
proxies for the P- and S-wave modes which are imaged
independently with acoustic wave
equations. This procedure works only if the vertical and
horizontal component accurately represent P- and S-wave modes, which
is not true in general. Therefore, multicomponent images constructed
with this procedure exhibit artifacts caused by the incorrect wave
mode separation at the surface.

An alternative procedure for elastic imaging uses the full vector fields for wavefield reconstruction and imaging. The wavefields are reconstructed using the multicomponent data as a boundary condition for a numerical solution to the elastic wave equation. The key component for wavefield migration is the imaging condition that evaluates the match between wavefields reconstructed from sources and receivers. For vector wavefields, a simple component-by-component cross-correlation between two wavefields leads to artifacts caused by crosstalk between the unseparated wave modes. An alternative method is to separate elastic wavefields after reconstruction in the subsurface and implement the imaging condition as cross-correlation of pure wave modes instead of the Cartesian components of the displacement wavefield. This approach leads to images that are easier to interpret, since they describe reflectivity of specified wave modes at interfaces of physical properties.

As for imaging with acoustic wavefields, the elastic imaging condition can be formulated conventionally (cross-correlation with zero lag in space and time), as well as extended to non-zero space and time lags. The elastic images produced by an extended imaging condition can be used for angle decomposition of primary (PP or SS) and converted (PS or SP) reflectivity. Angle gathers constructed with this procedure have applications for migration velocity analysis and amplitude versus angle analysis.

- Introduction
- Wavefield imaging

- Conventional elastic imaging conditions
- Imaging with scalar wavefields
- Imaging with vector displacements
- Imaging with scalar and vector potentials

- Extended elastic imaging conditions

- Angle decomposition

- Examples

- Discussion
- Conclusions
- Acknowledgment
- Bibliography
- About this document ...

Isotropic angle-domain elastic reverse-time migration |

2013-08-29