Abstract:Stratigraphic imaging, an approximate inversion of the spatial variation of the physical properties of subsurface strata, is of great value for the exploration and development of lithological and unconventional reservoirs. In this paper, a stratigraphic imaging method involving the relative perturbation of wave impedance of the reflector is proposed according to the idea of wave equation migration. On the basis of a smooth subsurface me-dium model featuring accurate kinematic characte-ristics of seismic waves, a linear forward expression of seismic data based on the relative perturbation of wave impedance of the reflector is derived by applying the seismic wave propagation theory. Then, the relative perturbation of wave impedance is obtained through approximate inversion from seismic data according to the linear inversion theory. A method of stratigraphic imaging with seismic data that is based on wave equation migration and takes wave impedance variation as the main target is constructed. During stratigraphic imaging, angle decomposition of the wavefield generates angle-domain common imaging-point gathers for stratigraphic imaging. In contrast, stratigraphic imaging results under an angle-domain average can be obtained quickly when angle decomposition of the wavefield is not performed. When the seismic data are described by the acoustic wave equation, the proposed stratigraphic imaging method can be employed to obtain stratum imaging based on the relative perturbation of acoustic wave impedance. When the seismic data are described by the scalar wave equation, the proposed method can be applied to attain stratum imaging based on relative velocity perturbation. Compared with the reverse time migration method based on seismic data, the proposed stratigraphic imaging method has the same calculation process and a comparable amount of calculation. This method also achieves a satisfactory stratigraphic imaging effect when it is applied to a test with synthetic seismic data.
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