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1. Introduction The development of gravity and magnetic inversion methods has always been an important research direction in geophysical exploration (Zhdanov, 2002; Zeng, 2005; Guan, 2005) [1,2,3]. However, to perform effective inversion, one must understand and execute forward modeling first. Since both gravity and magnetic exploration are based on potential field theory, the process of calculating theoretical observations involves potential field integration.
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