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Abstract

Summary

Conversion of P-wave to S-wave and vice versa is a well-known seismic wave propagation phenomenon which occurs when there is a high elastic impedance contrast between two layers. In basins, where a salt layer is present, the presence of converted waves is common.

The case study is located in the Eastern Mediterranean see, offshore Lebanon. This presentation will highlight the similarities between a DHI and a converted wave anomaly. An easy methodology to help seismic interpreters to better identify converted wave pitfall will be described. The result of the converted wave removal applied in a recent PSDM reprocessing will also be presented.

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/content/papers/10.3997/2214-4609.201903148
2019-11-19
2024-03-28
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References

  1. Kumar, J., Bell, M., Salem, M., Martin, T., Fairhead, S.
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