CONDUCTIVITY SPECTRA OF ROCKS FROM THE CRAIGMONT ORE ENVIRONMENT
The conductivities of rocks of a suite from the Craigmont ore environment were studied as functions of frequency over the four decades 1,000 to 0.1 cps. The following were observed on a plot of linear conductivity vs log frequency. (1) Rocks mineralized with disseminated sulfides and magnetite yield low‐to‐moderate induced polarization (I.P.) and have conductivity‐frequency spectra which are concave‐up. (2) As veining increases, the spectra tend to straighten, and become sensibly straight when much of the metallics are interconnected; such rocks are characterized by low to large I.P. (3) Massive specular hematite cores yield a large I.P. and have spectra which are markedly concave‐up. For comparison, (4) clay‐containing sandstones yield low to moderate I.P. and have spectra which are slightly convex‐up. Consequently, the combination of I.P. magnitude and spectral analysis permits distinction of the various mineralization types.