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A two-dimensional numerical model study and comparison of the polar dipole-dipole and Schlumberger resistivity arrays are presented. A catalog of dipole-dipole and Schlumberger apparent resistivity pseudo-sections is presented. It is concluded that: for the Schlumberger array, data can be accurately interpreted only if the resistivity structure is horizontally layered, and conductive bodies having a depth of burial greater than their width are not observed; for the dipole-dipole array, complex anomaly patterns unrelated in appearance to the causative structure result from simple models; hence, a familiarity with model results is essential to interpretation of these data.

osti oai (u.s. department of energy office of scientific and technical information)

Telluric and D. C. resistivity techniques applied to the geophysical investigation of basin and range geothermal systems. Part II. A numerical model study of the dipole--dipole and Schlumberger resistivity methods