Imaging velocity analysis method of seismic scattering P-S converted wave

Abstract

The invention relates to an imaging velocity analysis method of a seismic scattering P-S converted wave, comprising the following steps of: firstly, reading the seismic data of a seismic scattering P-P wave into a two-dimensional array F, and computing the position and the coordinate of a scattering point; secondly, arbitrarily selecting a velocity vPk to overlap or correlate scattering amplitudes of shot-geophone distances and weigh to sum the energy of the same scattering point so as to obtain a corresponding average amplitude; thirdly, making a seismic scattering P-P wave velocity spectrum; fourthly, reading the seismic data of the seismic scattering P-S converted wave into a two-dimensional array E, and computing the position and the coordinate of the scattering point; fifthly, taking an acquired seismic scattering P wave velocity to overlap or correlate the scattering amplitudes of the shot-geophone distances and weigh to sum the energy of the same scattering point so as to obtain the corresponding average amplitude; and sixthly, making a seismic scattering P-S converted wave velocity spectrum. The invention increases the overlapping times of a velocity analysis technology and enables the focusing capability of effective scattered wave energy to be higher.

Description

technical field [0001] The invention belongs to the technical field of seismic wave velocity parameter extraction and imaging processing, in particular to a seismic scattering P-S converted wave imaging velocity analysis method. Background technique [0002] Velocity is the basis of seismic wave propagation and one of the key factors in imaging. The accuracy of velocity acquisition is directly related to the accuracy of seismic wave imaging. The time-distance curve of the reflected converted wave is neither symmetrical nor hyperbolic to the common conversion point. The traditional hyperbolic approximation is not applicable to the converted wave at all. Inherent characteristics of the distance relationship: first, even if it is a horizontal reflection layer of a uniform medium, the horizontal position of the conversion reflection point of the converted wave changes with the offset, the depth of the reflection layer, and the ratio of longitudinal and transverse waves; second, ...

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Problems solved by technology

The time-distance curve of the reflected converted wave is neither symmetrical nor hyperbolic to the common conversion point. The traditional hyperbolic approximation is not applicable to the converted wave at all. Inherent characteristics of the distance relationship: first, even if it is a horizontal reflection layer of a uniform medium, the horizontal position of the conversion reflection point of the converted wave changes with the offset, the depth of the reflection layer, and the ratio of longitudinal and transverse waves; second, the reflection The time-distance curve of the converted wave is not a hyperbola. If the hyperbolic time-distance relationship is used for velocity analysis, the correct shear-wave velocity value will not be obtained, especially for medium-shallow layers and large offsets. In addition, Common conversion point CC

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