Seismic source location method eliminating influences of velocity errors
A technology for seismic source location and velocity elimination, which is applied in the field of resource mining and seismic exploration, can solve the problems of velocity model inversion difficulties, multiple solutions, and large errors, and achieve the effect of eliminating strong dependence
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Embodiment 1
[0061] Example 1 uses a theoretical model for testing. figure 1 It is the diagram of the model in Example 1, with five layers in total, the speed of each layer is V1, V2, V3, V4, V5, and two seismic sources A and B are placed, wherein the asterisk is the seismic source A, and the circle is the seismic source B. Point A is set at (1100, 1200), point B is set at (950, 1350), and the ground observation position is (10-1000) meters, as shown by the arrow in the figure, A is a known point, and B is the position to be positioned point.
[0062] figure 2 is the observed travel time (that is, when the observations of A and B arrive, steps 1, 2, and 3 are used), figure 2 Series 1 is the curve at point A, series 2 is the curve at point B, ( figure 2 The middle thick line (above) is series 2) The time unit is seconds. Table 1 shows the positioning of seismic source point B by using the present invention under different models. In the model, only the velocity changes, and the depth...
Embodiment 2
[0068] image 3 It is the profile of the source A observed by a certain actual data, two observation lines in different orientations (the arrangement of the receiver points, a total of two lines of receivers are received, and one observation line refers to the arrangement of many receivers along a certain line. ), where the position of point A is known as (3353126.0, 338361.0, 2145.1).
[0069] Figure 4 It is the profile of source B observed by some actual data, and the location of source B is unknown.
[0070] Figure 5-1 is true image 3 The travel time picked up after performing residual correction (residual correction is a correction method in seismic exploration, using mathematical methods to eliminate small time difference changes in seismic traces to make the time curve smoother), Figure 5-2 is true Figure 4 Travel time picked up after residual correction (for image 3 and Figure 4 The travel time picked up after residual correction is Figure 5-1 and Figu...
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