Geochemistry of the Archaean granulites of the south of the Aldan shield

For the first time, the initial nature of the granulitis of the late Archarician South Deep Complex representing the Lower Non -Nicno formations of the south of the Aldan shield was established. Based on the geological data, the patterns of the distribution of the main Petro-gene elements and intxile elements, it is shown that the protolites of the granulitis of the South complex are lime-base volcanoes and mosquituity-toleite series, as well as terrigenous-ambulance breeds. Petroological models of the formation of the volcanic of lime--base and mosquititis of the-toleite series, based on the mechanism of plumovy tectonics, are proposed. For geochemists, petrologists and geologists involved in the study of metamorphic rocks