Method for inversing a wavenumber domain of underground three-dimensional magnetic distribution by magnetic total tensor gradient
A full-tensor, wavenumber-domain technology, applied in the field of geophysical exploration, can solve the problems of low inversion efficiency and large amount of calculation of large data volume models, so as to improve inversion efficiency and inversion accuracy, simple calculation, and reduce attenuation sexual effect
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[0055] Three-dimensional wavenumber domain inversion is a hotspot and development trend in the current research on gravity and magnetic data processing and interpretation, and it is used to quickly reconstruct the three-dimensional physical property distribution in the underground half space. Through the magnetic full tensor gradient anomaly data, more information reflecting the characteristics and details of the field source can be obtained, which is beneficial to fine underground geological interpretation. This implementation takes two combined upright cuboids as an example: the two upright cuboids (1) have the same physical properties and the same buried depth, such as figure 1 As shown in A; (2) The physical properties are different, and the buried depth is different, such as figure 1 Shown in B. Using a magnetic full tensor gradient inversion method for the three-dimensional magnetic distribution in the subsurface, such as Figure 4 shown in sequence. The method compri...
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