Depth migration of crustal-scale seismic reflection profiles: A case study in the Bohai Bay basin

Abstract

The application of the pre-stack depth migration (PSDM) method using deep seismic reflection data is still a challenge. In this paper, a deep seismic reflection dataset collected from the Bohai Bay Basin is used to test the applicability of the pre-stack depth migration method. After improving the signal-to-noise ratio of the prestack gathers and building an accurate velocity model capturing lateral and vertical variations, a high-quality pre-stack depth migration profile is obtained. This profile shows detailed crustal structures and an undulating Moho. The depth difference between the east and west sides of the Moho imaged in the profile is about 6 km. The Moho is disrupted by several discontinuities. Compared with conventionally stacked time-migration profiles, the pre-stack depth migration profile provides a higher-resolution subsurface image with accurate depth information. Combining geological and geophysical data, the pre-stack depth migration profile reveals geologic structures responsible for crust thinning during the destruction of the North China Craton. The profile also provides more accurate depth domain information for further study of crust-mantle interaction in this area.

Improved Seismic Imaging Through Petrophysical Approach Using Thomsen's Parameter Estimation in Anisotropic Prestack Depth Migration (Psdm)

“…If the lateral velocity variation is large, this time migration cannot produce a sub-surface image properly and correctly. To shortcoming this, migration techniques are carried out indepth migration, where the migration results are displayed in the depth region shown in Figure 2, resulting in subsurface images following actual geological conditions [14]. According to Thomsen, seismic anisotropy is a dependence on seismic velocity on angles.…”