Температуры образования хромпиропов геоблоков Украинского Щита и перспективы их алмазоносности

Abstract

On the basis of determination of maintenance of nickel in a depth high-chromium pyrops, selected in the different areas of the Ukrainian shield (US), the temperature terms of environment of their mineralogenesis are set. It one of main parameters, allowing to estimate the prospects of diamondiferous of both separate kimberlite bodies and blocks of US on the whole.