Seismic horizon automatic extraction device and method based on dynamic planning
A dynamic programming and automatic extraction technology, applied in seismic signal processing and other directions, can solve problems such as high computational cost, inability to reveal geological structure information, and inability to automatically extract accurate seismic horizons with consistent phases, reducing computational costs, time saving effect
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Embodiment 1
[0072] Such as image 3 Shown are horizons extracted from 2D seismic images using the slope-based method and using the dynamic programming method, respectively. image 3 (a) is the input original 2D seismic image; image 3 The white dotted line in (b) is the horizon picked up by the traditional slope-based method; image 3 The white dotted line in (c) is the horizon picked up by the method of dynamic programming in the present invention. It can be seen that the position of the white arrow has been significantly improved, image 3 The result in (c) is more accurate.
Embodiment 2
[0074] Such as Figure 4 Shown is the comparison chart between the results of this method and manual interpretation. in, Figure 4 (a) shows the actual 3D seismic image of a certain area, and the white arrow shows the target horizon (indicating the position of the black trough); Figure 4 (b) It is the result of manual interpretation, the phase jump phenomenon of the horizon is very obvious, and there are obvious grid-like artifacts; Figure 4 (c) as a result of the present invention, with Figure 4 (b) is the initial horizon, the result after updating by dynamic programming. It can be seen that the phases of the planes picked up by the dynamic programming method are more consistent (basically all black), and the grid-like artifacts are also eliminated.
Embodiment 3
[0076] Such as Figure 5 As shown, among them, Figure 5 (a) is the input original 3D seismic image, and the white arrow indicates the target layer (white peak position); Figure 5 (b) is the result obtained by the slope-based method; Figure 5 (c) is the result obtained by the present invention. As can be seen, Figure 5 The horizons in (c) have more consistent phases, and more detailed geological structures can be obtained, such as the channel information indicated by the white arrow. Figure 6 for from Figure 5 The comparison results of the 2D profiles: where Figure 6 (b) for Figure 6 In the area shown by the black box in (a), it can be clearly seen that the result obtained based on the method of the present invention (black dotted line) is significantly better than the result obtained by the slope-based method (white solid line).
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