Reverse Time Migration Imaging Method and Device

Abstract

The invention provides a reverse time migration imaging method and device. The method includes the following steps that: a shot of data are obtained; a depth domain velocity field is transformed to pyramid grids from regular grids; the coordinates of anisotropy parameters delta and epsilon, a symmetry axis tile angle parameter theta and a symmetry axis azimuth parameter phi are transformed to the pyramid grids from the regular grids; finite difference wave field simulation is performed on a wave field generated by excitation by using a coupling second-order partial differential equation of the pyramid grids, so that a wave field corresponding to a shot point and a wave field corresponding to a detection point can be obtained; imaging is performed on the wave field corresponding to the shot point and the wave field corresponding to the detection point by using a cross-correlation imaging condition; an imaging result is interpolated to the regular grids, the imaging result which has been interpolated to the regular grids is adopted as a single-shot imaging result of the shot point. With the method and device of the invention adopted, the technique problem that changing grids cannot be utilized to perform imaging in a horizontal direction and a vertical direction simultaneously can be solved, and changing grids can be utilized to perform imaging in a horizontal direction and a vertical direction simultaneously in a horizontal direction and a vertical direction.

Description

technical field [0001] The invention relates to the technical field of geological exploration, in particular to a reverse time migration imaging method and device. Background technique [0002] Reverse Time Migration (RTM) technology is based on the full acoustic wave equation, completely obeys the physical laws of the wave in the acoustic medium, and completely simulates various wave phenomena in the process of seismic wave field propagation with high precision, making it more suitable for velocity For seismic wave imaging problems in complex structural regions with drastic changes, especially when there are gyroscopic waves and prism reflection phenomena in the wave field, reverse time migration (RTM) can show advantages over one-way wave equation migration. [0003] Since the reverse time migration (RTM) simulates the propagation of seismic waves through the difference method in the time-space domain, this method can be easily and naturally extended to the imaging problem...

AI Technical Summary

Problems solved by technology

[0004] The wave field simulation for the acoustic wave and elastic wave equation is the basis of the migration imaging method based on the wave equation. The commonly used numerical calculation methods include: the finite element method and the finite difference method. Among them, the finite element method has the advantages of Great flexibility, but the downside is that it lacks the ability to apply to high-order algorithms, especially considering frequency-dependent dispersion

[0006] However, how to use changing grids for imaging in the horizontal direction (X\Y) and vertical direction (Z) at the same time, has not yet proposed an effective solution

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