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Stable gradient design method for the inverse gravimetry problem. (Russian) Zbl 1038.86007
Theoretical and numerical analysis of problems of the interpretation of gravimetry observation data connected with a definition of shapes of underground anomaly-formed structures was considered in several papers. In this article two formulations of inverse gravimetry problems, corresponding to the definition of the shape of a limited anomaly-formed inclusion and to finding a contact surface of two media are presented. The integral equations are solved by a gradient type method. Results of free falling acceleration measuring on a given section of a daily surface are used.

MSC:
86A20 Potentials, prospecting
86A22 Inverse problems in geophysics
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