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ABSTRACT

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Muography is surely one way to shed light on the density structure of the underground, but it is not the only one. Classical gravity surveys also provide information on the mass distribution of the entire Earth. Although these two methods differ in sensitivity, combining the two (joint inversion) would combat the weaknesses of each method and improve the resolution of three‐dimensional imaging. This chapter introduces one formulation of the joint inversion following an early work done by the author’s group, and tries to review further technical developments and applications by other researchers. Future technical prospects are discussed at the end.

Muography

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