A Simultaneous Inversion Method of Microseismic Source Location and Velocity Model
A velocity model and microseismic technology, applied in seismic signal processing and other directions, can solve problems such as unfavorable shallow velocity inversion, and achieve the effect of improving inversion accuracy, high positioning accuracy, and strong inversion stability
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[0048] Below in conjunction with accompanying drawing, the present invention is described in further detail:
[0049] joint tomographic equations
[0050] 1) Ordinary tomographic equation: actual observed travel time from microseismic event i to receiving point k
[0051]
[0052] where u is the slowness field (reciprocal of velocity), τ i is the moment of shock. When locating a microseismic, the source coordinates (x 1 , x 2 , x 3 ), the seismic moment and the slowness field are all unknown parameters.
[0053] The time of arrival received by the geophone (P wave or S wave), using the test source location, the moment of shock generation and the initial velocity model (prior information) to calculate the theoretical arrival time The residual between the two travel times is
[0054] Calculate travel time and observe travel time residuals The perturbation of the source and velocity models can be approximated linearly as
[0055]
[0056] Among them, the sour...
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