Electromagnetic Method
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The most common electromagnetic method of exploration is the induced polarization of massive sulfide deposits (MSD). By sticking a couple of electrodes into the earth and running a current through them, IP and resistivity can be measured. IP is basically a measure of a circuit's storage capacity for electrical energy. When a circuit is run through some section of the earth and the IP reading drops dramatically, there is a high probability that an MSD is lurking below the surface. This is great because massive sulfide deposits are very valuable and usually contain a conglomeration of Zn, Pb, Au, Ag, and Cu.