GEOCHRONOLOGY OF MESOZOIC GRANITOIDS AND ASSOCIATED MOLYBDENUM MINERALIZATION IN THE WESTERN PART OF THE DZHUGDZHUR-STANOVOI SUPERTERRANE

Abstract

The Dzhugdzhur superterrane located at the south-eastern margin of the Siberian Craton is one of the key structures of the eastern margin of Asia. It is made up of the traditionally distinguished Early and Late Precambrian complexes and numerous Early–Late Mesozoic intrusive and volcanoplutonic associations [2 and others]. The functioning of magmatic and ore systems of different ages and types in various geodynamic settings in the course of complex and multistage evolution of tectonic structures produced no less intricate metallogenic specifics of the region.