Abstract
In the composition of the explosive-atmoelectrogenic paragenes studied by us, more than 100 mineral species, varieties and non-crystalline phases are found - carbon minerals, phases and compounds, native metals and alloys, carbides, silicides, nitrides, halides, chalcogenides, oxides, silicates and aluminosilicates, oxygen salts. The studied paragenes is characterized by an abnormally low level of mineralogical organization, which indicates the deep origin of the substance in the explosive facies of volcanic eruptions, including carbon minerals, phases and organic compounds.
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