Abstract
As we already mentioned in Sect. 6.1, the data of unknown functions F ϵ L 2(ℬ) are usually only indirectly given as data of tomographic problems. For example, the inverse gravimetric problem consists of finding the mass density ρ ϵ L 2(ℬ)for a given gravitational potential V on ℝ3 ∖ ℬ such that (Formula presented) 10.1.
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Michel, V. (2013). Splines. In Applied and Numerical Harmonic Analysis (pp. 265–287). Springer International Publishing. https://doi.org/10.1007/978-0-8176-8403-7_10
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