- Conference Article
- 10.2118/229781-ms
Tackling Subsurface Complexity in Middle East Seismic Imaging - Use or Remove Shear Arrivals?
- Nov 03, 2025
- J Brittan + 2 more +2
In areas with high impedance contrast reflectors, which are common offshore in the Middle East, the stark contrast between high-velocity formations (typically salt or carbonates) and the surrounding sediments often gives rise to converted wave modes. These occur when compressional (P-wave) energy transforms into shear (S-wave) energy upon encountering the sharp velocity boundaries at the top or base of a high-velocity body. Since S-waves travel more slowly than P-waves, their arrival times differ, and they can appear as misleading deeper events in seismic records. If not properly managed, this energy can obscure true reflections and hinder accurate subsurface interpretation (Elbassiony et al., 2018). For example, one of the main challenges in hydrocarbon exploration within the Messinian salt province of the Eastern Mediterranean is the contamination of P-wave seismic images by these converted wave modes. In this region, the salt typically has interval velocities around 4200–4300 m/s, while adjacent post- and pre-Messinian sediments range from 2400 to 3000 m/s (Jones and Davison, 2014). This sharp velocity contrast promotes mode conversion, especially at steep salt boundaries, often resulting in complex interference patterns in seismic data. While converted waves can occasionally improve subsurface illumination or provide additional geometric insight, they more often act as noise—particularly problematic for imaging sub-salt targets where precision is crucial. This leads to the dilemma for the imaging geophysicist, shall we use the information provided by these shear arrivals or remove these arrivals as noise? Whilst emerging technologies such as elastic FWI tantalisingly offer the opportunity to exploit the information carried by the shear wave arrivals, in exploration areas with little well control, there are likely to be significant uncertainties in shear velocity information (especially in the shallow subsurface) that may hinder this approach. Thus, for the purpose of this paper we will be generally looking at ways of attenuating these unwanted arrivals – without harming the underlying primary arrivals. Among the various types of converted waves, those involving conversion at both the top and base of the salt—such as PSPP and PPSP modes—are especially problematic due to their strong amplitudes and complex moveout behaviour. Symmetrical conversions like PSSP, although theoretically possible, are rarely observed in practice due to their weaker amplitudes and longer travel times. Traditional suppression techniques, such as velocity-based filtering or targeted muting using travel-time models, often fall short in regions with complex or irregular salt geometries.
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