Abstract

The explosive atmospheric electrogenic paragenesis we studied was found to contain over 100 mineral species, varieties, and non-crystalline phases (carbonaceous minerals, phases and compounds, native metals and alloys, carbides, silicides, nitrides, halides, chalcogenides, oxides, silicates and alumosilicates, and oxysalts. The paragenesis is characterized by an abnormally low level of mineralogical organization, which indicates a deep origin of the material in the explosive facies of volcanic eruptions, including carbonaceous minerals, phases, and organic compounds.

中文翻译：

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堪察加半岛和千岛群岛最近爆发的喷发物引起的弹射性矿物相共生。第2部分。托尔巴奇克型钻石的辅助矿物

摘要

我们研究到的爆炸性大气电成因共生被发现包含100多种矿物种类，变种和非晶态相（碳质矿物，相和化合物，天然金属和合金，碳化物，硅化物，氮化物，卤化物，硫族化物，氧化物，硅酸盐和共生的特征是异常低水平的矿物组织，这表明该物质在火山喷发的爆炸相中是深层起源，包括碳质矿物，相和有机化合物。