Abstract
A new concept of cluster evolutionary minerageny is based on the idea of the formation of the Earth from the primary stellar material, which was preserved in the planet’s core. Its further destruction due to decay of heavy nuclear matter results in fragmentation of the material until the appearance of superheavy elements with their further nuclear dissociation. As a result, protomagma arises and penetrates to the upper mantle in the form of plume flows. This process supports the reactions that control the formation of chemical elements, minerals, ores, and rocks, which compose the upper mantle and the Earth’s crust. The processes of nuclear dissociation lead to the release of energy and decompression of matter. This initiates an increase in the Earth’s volume, its geotectonic activity, and the creation of the hydrosphere and atmosphere.
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