Abstract
Inverse problems often consist in finding a physical quantity (density, diffusivity, conductivity) defined in a certain domain (‘support’). The determination of a solution always requires a mathematical modelling of the corresponding (source or parameter) functions and domains involved. This process can be understood as a certain manner of probing or sounding. In this meaning ‘sounding’ can be directed to the approximation of one or several function values, e.g. by means of the known Backus-Gilbert method, but it is also done by the decomposition procedures to be considered here.
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Ballani, L. (1995). Solving the Inverse Gravimetric Problem: On the Benefit of Wavelets. In: Sansò, F. (eds) Geodetic Theory Today. International Association of Geodesy Symposia, vol 114. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-79824-5_26
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DOI: https://doi.org/10.1007/978-3-642-79824-5_26
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