The objective of this paper is to construct a stable inversion scheme
to determine the conductance of a buried inhomogeneous layer masked by
sedimentary cover. We employ a model which incorporates a surface she
et of conductance S-1(x, y) and a buried sheet of conductance S-2(x, y
). The buried sheet is embedded at a depth d in a layered earth of con
ductivity sigma(z). The sigma(z), d and S-1(x, y) are assumed to be kn
own. We determine S-2(x, y) by inverting the monochromatic horizontal
electromagnetic (EM) field measured at the earth's surface. To do this
, we use Price's matching conditions at the sheets and a stable contin
uation of EM field from the earth's surface onto the buried sheet. Emp
loying synthetic data we demonstrate that the designed inversion schem
e generates a reasonable image of the buried structure. The scheme is
fast, since it doesn't require any forward modelling.