A Method of Seismic Source Location Based on P-wave Arrival Time and Waveform Amplitude
A technology of waveform amplitude and seismic source positioning, which is applied in seismology, seismic signal processing, measuring devices, etc., can solve the problems of positioning accuracy and precision randomness, automatic and accurate picking, etc., achieve high accuracy, improve positioning accuracy and Accuracy, clear results
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[0064] From step 2, the focal coordinates of one localization can be obtained as follows:
[0065] Table 1 The actual coordinates and primary positioning coordinates of the five groups of seismic sources
[0066]
[0067]
[0068] From Step 3, Step 4, and Step 5, Table 2 can be obtained as follows:
[0069] Table 2 K-v function relational expression of 5 groups of seismic sources
[0070]
[0071]
[0072] From step 6, the coordinates of the secondary seismic source can be obtained as shown in the table below
[0073] Table 3 The actual coordinates and secondary positioning coordinates of the five groups of seismic sources
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[0075] It can be seen from Table 3 that after speed correction, the accuracy of the secondary positioning coordinates is significantly higher than that of the primary positioning coordinates.
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