Hp. Huang et Dc. Fraser, Mapping of the resistivity, susceptibility, and permittivity of the earth using a helicopter-borne electromagnetic system, GEOPHYSICS, 66(1), 2001, pp. 148-157
Interpretation of helicopter-borne electromagnetic (EM) data is commonly ba
sed on the mapping of resistivity (or conductivity) under the assumption th
at the magnetic permeability is that of free space and dielectric permittiv
ity can be ignored. However, the data obtained from a multifrequency EM sys
tem may contain information about the magnetic permeability and dielectric
permittivity as well as the conductivity. Our previous work has shown how h
elicopter EM data may be transformed to yield the resistivity and magnetic
permeability or, alternatively, the resistivity and dielectric permittivity
. A method has now been developed to recover the resistivity, magnetic perm
eability, and dielectric permittivity together from the transformation of h
elicopter EM data based on a half-space model. A field example is presented
from an area which exhibits both permeable and dielectric properties. This
example shows that the mapping of resistivity, magnetic permeability, and
dielectric permittivity together yields more credible results than if the p
ermeability or permittivity is ignored.