Regionalization of global electromagnetic induction data - A theoretical model

Details Regionalization of global electromagnetic induction data - A theoretical model Regionalization of global electromagnetic induction data - A theoretical model

Dec 1981

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981pepi...27..159h&link_type=abstract

Physics of the Earth and Planetary Interiors, vol. 27, Dec. 1981, p. 159-163.

Physics

Geophysics

3

Earth Planetary Structure, Electrical Resistivity, Electromagnetism, Geoelectricity, Geophysics, Planetology, Inhomogeneity, Magnetic Induction, Vertical Distribution

Scientific paper

Systematic differences are found between global response functions derived from single observatories and those derived from global averages. It is demonstrated that reasonable differences in the depth to the conductosphere result in significant differences in the response functions at single observatories, which appear to be easily resolvable within the expected error-bars of actual observations. It is concluded that the global response function from a single site or a closely spaced group of sites can be used to infer a regionally-representative model for the earth, providing that systematic bases introduced in data processing and interpretation are minimized.

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