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Discussion

Seismic data are usually acquired with geophone layouts that record information from multiple source locations. The redundancy in the coverage is necessary to eliminate gaps in the data, estimate velocity, and image the data. Thus, the direct relation between the traveltime field and the source location allows us to estimate attributes that can help in interpolation, velocity estimation and possibly imaging. Specifically:

However, the formulation developed here has limitations. Chief among them is the need to evaluate derivatives of velocity and traveltime fields. Since velocities may include discontinuities, their derivatives are not easy to evaluate. However, similar to the ray-based methods, one can simply smooth the velocity field.

Since traveltime fields that contain all arrivals satisfy the eikonal equation, the source perturbation can be applied to traveltimes extracted from other methods, such as ray tracing or escape equations. Therefore, they can include most energetic arrivals as opposed to first-arrival traveltimes.


next up previous [pdf]

Next: Conclusions Up: Alkhalifah and Fomel: Source Previous: Marmousi example

2013-04-02