Open AccessMineral-phase paragenes in explosive products of modern emergencies of Kamchatka and Kuril volcanoes. Part 2. Minerals-satellites of tolbach type diamond
Author(s) -
В. И. Силаев,
Г. А. Карпов,
Л. П. Аникин,
L. P. Vergasova,
В. Н. Филиппов,
Kirill V. Tarasov
Publication year - 2019
Publication title -
vulkanologiâ i sejsmologiâ
Language(s) - English
Resource type - Journals
ISSN - 0203-0306
DOI - 10.31857/s0203-03062019636-49
Subject(s) - mineral , volcano , explosive material , geochemistry , geology , aluminosilicate , carbon fibers , diamond , presolar grains , nitride , mineralogy , materials science , astrobiology , chemistry , metallurgy , meteorite , chondrite , nanotechnology , catalysis , composite number , biochemistry , organic chemistry , composite material , physics , layer (electronics)
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.