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Mineral-petrochemical and geochemical features of ultrametamorphic process of the focus-dome type

Abstract

Distribution of petrogeneous and oregeneous (Au, Ag, Hg) chemical elements in metamorphic zones of the Kedrovskiy focus-dome construction in Northern Transbaikalia is shown and discussed. The conclusion is drawn about absence of substance essential migration during local focus-dome ultrametamorphism

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