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Magnetic anomaly inversion is a critical technique in the field of geophysical exploration, playing a significant role in revealing subsurface geological structures, mineral resource prospecting, and geological hazard prediction1. Over the years, numerous researchers have proposed a variety of methods for magnetic anomaly inversion, continuously enriching both the theoretical foundations and practical methodologies in this domain.
In earlier studies, various optimization algorithms were applied to magnetic anomaly inversion. For example, an ant colony optimization method constrained by lithology was developed for pro....