To the method of estimation of background and anomalous nickel contents in basic-ultrabasic rocks
Abstract
One of the most promising criteria of nickel bearing capacity of basic-ultrabasic massifs is naturally considered to be the content of nickel, the main component of copper-nickel ores, in non-ore rocks. The main difficulty in applying this criterion is the unevenness of the background nickel content, which in the series of basic-ultrabasic rocks increases from the most acidic representatives of the series to the most basic ones. This phenomenon was first taken into account by D. V. Polferov.
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