A Discontinuous 3D Joint Inversion Method Based on Smooth Focus Regularization
A joint inversion and smoothing technology, applied in geophysical surveying, instruments, etc., can solve problems such as difficult convergence and low resolution, achieve the effects of reducing local false anomalies, improving resolution, and solving difficult convergence
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[0020] like figure 1 As shown in , a discontinuous 3D joint inversion method based on smooth focus regularization includes the following steps:
[0021] 1) Read in the observation data of 3D gravity, gravity gradient and magnetotelluric, read in the initial model, set the expected fitting difference and the maximum number of iterations, calculate and record the initial fitting difference.
[0022] 2) Based on the traditional focusing regularization, the gravity and gravity gradient data are combined to perform several separate density inversions, and iterate until the initial structure of the density model is revealed. Based on smooth focusing regularization, the magnetotelluric data are independently inverted several times for resistivity, and iterated until the initial structure of the resistivity model is revealed. The fit difference is calculated and recorded for each iteration.
[0023] 3) Alternately perform discontinuous cross-gradient joint inversion on the density m...
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