Geophysical Journal | 2007 volume 29 1

The inverse problem of gravimetry in a class of horizontally-layered model

© Bulakh E.G., Markova M.N.

The inverse problem of gravimetry in such a posing is being solved. One horizontal stratum is given. The position of a low boundary of this stratum is an argument required. Exuberant gravity of masses, which are placed inside a horizontal stratum, is a function of three coordinates. The approximating construction of this function is introduced. It is possible to input into a condition of a problem some data on fixed points, in which the value of exuberant gravity is known. If the field of variation of anomaly of gravity force concerning a field in a fixed point is given, the allocation of exuberant gravity inside a horizontal stratum is restored.

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