Grid successive dissection method used for microseismic positioning
A grid division and microseismic technology, applied in seismology, seismic signal processing, geophysical measurement, etc., can solve problems such as reducing positioning efficiency, increasing computing time, restricting practicability, etc., to improve positioning accuracy, reduce Workload, effect of high microseismic positioning accuracy
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Embodiment 1
[0047] The single-size grid of the original algorithm is used to perform a single global subdivision of the target area. A 5-layer formation model is simulated by computer, and the velocity values of the 1st to 5th layers are as follows:
[0048] 800m / s, 1000m / s, 1700m / s, 2200m / s, 2700m / s, the perforation position is (225, -147, -962), and the simulated seismic waveform is described by 50Hz seismic wavelet.
[0049] A. Define a three-dimensional target area near the perforation, that is, microseismic events may occur in this area. In this embodiment, the target area is selected based on the perforation coordinates. The three-dimensional coordinates of the selected target area are X∈[-300,300], Y∈[-300,300], Z∈[-1000,-800]. The microseismic ground geophones are arranged in a star shape, with a total of 6 survey lines, and each survey line has 16 geophones (96 channels), such as Figure 4 shown. To select one as the reference trace M, it is required that this trace ...
Embodiment 2
[0064] The perforation positioning is carried out by using the method of grid subdivision successively. For the convenience of comparison, the simulation model is the same as that of Example 1, where the velocity values of layers 1 to 5 are: 800m / s, 1000m / s, 1700m / s, 2200m / s, 2700m / s, and the perforation positions are (225 , -147, -962), the simulated seismic waveform is described by 50Hz seismic wavelet.
[0065] A. Define a three-dimensional target area near the perforation, that is, microseismic events may occur in this area. In this embodiment, the target area is selected based on the perforation coordinates. The three-dimensional coordinates of the selected target area are X∈[-300,300], Y∈[-300,300], Z∈[-1000,-800]. The microseismic ground geophones are arranged in a star shape, with a total of 6 survey lines, and each survey line has 16 geophones (96 channels), such as Figure 4 shown. To select one as the reference trace M, it is required that this trace has ...
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