РУДОНОСНОСТЬ ЗЕЯ-ГИЛЮЙСКОЙ СТРУКТУРЫ ЦЕНТРАЛЬНОГО ТИПА

Abstract

Within the limits of the Upper Priamyrye and according to geomorphologic, geological and geophysical facts, it was founded the separation of Zeya-Gilyuiskaya central type’s structure (CTS) according. It was shown that it is the through-crusted structure of ancient layer which have passed the series of activation stages, mostly of Mesozoic age. Ore-bearing process of CTS was characterized, deposits of gold, copper, nickel, graphite and other minerals regularly take place within the bounds of this structure, also there were founded diamonds’ grains. It’s supposed that platinum- and gold-ore copper-nickel mineralization, gold placers, graphite deposits and diamonds’ discovery have the most practical importance.