0. Origin of resistivity anisotropy in rocks.
in rock's resistivity resulted from orientation of elongated rock grains
(fig.1) or from fine layering with different resistivity values.
Anisotropy can result from rock's fracturing (fig.2), pressure,
metamorthism and ore grains, disseminated in rock. We shall
consider here anisotropy with vertical or inclined layering orientation.
119899, Russia, Moscow, Moscow State University, Geological
Faculty, Department of Geophysics
V.A. Shevnin, I.N. Modin
Tel. & fax: (7-095) 939 49 63
Please feel free to send us