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- W2261404745 abstract "Measurements of the strength of the magnetic field of the Earth (generally made from an aircraft or helicopter platform) are used to discern the nature of the near-surface geology, since many rocks contain magnetic minerals and are therefore weakly magnetic. Interpretation of the observed field values involves the geophysicist providing an initial estimate of the geology which is then improved or refined using least-squares inverse methods. This paper shows that, providing the model response to the parameters under inversion (such as the depth or position of a geological structure) is non-linear, then the set of models that converge to a given minimum in the misfit surface displays self-similarity and appears to be fractal in nature. The fractal dimension of the resulting basin of attraction can be reduced by increasing the damping of the inversion process." @default.
- W2261404745 created "2016-06-24" @default.
- W2261404745 creator A5059886395 @default.
- W2261404745 date "2002-01-01" @default.
- W2261404745 modified "2023-09-26" @default.
- W2261404745 title "Fractal Basins of Attraction in the Inversion of Geomagnetic Data" @default.
- W2261404745 cites W2087070363 @default.
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- W2261404745 doi "https://doi.org/10.1533/9780857099594.138" @default.
- W2261404745 hasPublicationYear "2002" @default.
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