Abstract:The response characteristics of small-scale Karst fracture-cavity units in Dengying Formation of the central Sichuan paleo-uplift are not distinct on the seismic profile, which makes the seismic characterization difficult for fracture cavities in Dengying Formation. To strengthen the seismic reflection characteristics and predict the distribution of small-scale fracture cavities, we perform the scattering imaging on the full-azimuth common dip-angle gather with the full-azimuth local angle-domain imaging method. This intensifies the seismic reflection characteristics of small-scale fracture cavities. According to the strong energy spectrum characteristics of the small-scale fracture cavities in the scattering imaging, the energy body attributes are extracted from scattering imaging data for the description of the fracture cavity development cha-racteristics. The following conclusions are obtained:① The full-azimuth local angle-domain imaging method is more effective than the conventional Kirchhoff migration imaging method; ② The scattering imaging data volume can enhance the seismic reflection characteristics of discontinuous geolo-gical bodies and reflect the geological phenomena such as small-scale fracture cavities; ③ With the reservoir in Dengying Formation in the central Sichuan paleo-uplift as an example, the energy body attribute features extracted from the scattering imaging data volume are better than those extracted from the conventional post-stack seismic data in the reflection of the distribution of discontinuous geological bodies such as fracture cavities.
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