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首页> 外文期刊>Journal of Volcanology and seismology >Mineral Phase Paragenesis in Explosive Ejecta Discharged by Recent Eruptions in Kamchatka and the Kuril Islands. Part 1. Diamonds, Carbonaceous Phases, and Condensed Organoids
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Mineral Phase Paragenesis in Explosive Ejecta Discharged by Recent Eruptions in Kamchatka and the Kuril Islands. Part 1. Diamonds, Carbonaceous Phases, and Condensed Organoids

机译:爆炸爆炸矿床植入爆发的矿物阶段植入在堪察加和Kuril群岛中排出。 第1.钻石,碳质阶段和凝聚有器材

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摘要

Ejecta of recent volcanic eruptions were found to contain a carbonaceous mineral phase paragenesis of explosive atmospheric electrogenic origin. The paragenesis involves diamonds of octahedral habitus with non-aggregated nitrogen defects (without signs of mantle burning), disordered graphite, shungite-like bitumen (kerite-anthraxolite), carbonaceous globules (clustered allotropes of dicarbon composition), metal carbon nano-microcomposites resulting from thermal impact decomposition of metal organic compounds, and abiogenic organic compounds. The carbonaceous paragenesis identified here is considered as a unique natural phenomenon that indicates the existence of a global process that favor endogenous carbonization of the Earth's crust during crust-mantle interactions.
机译:最近火山爆发的喷射物含有炸药矿物相瓣膜爆炸性大气引发。 Paraganesis涉及八面体栖息地的钻石,具有非聚集的氮缺损(没有甲状腺燃烧的迹象),石墨无序的石墨,类似的沥青(Kerite-炭疽沸石),碳质球果(含二碳组合物的聚集型异形),金属碳纳米微孔复合材料 来自金属有机化合物的热冲击分解和辐条有机化合物。 这里鉴定的碳质植物被认为是一种独特的自然现象,表明存在在地壳 - 地幔相互作用期间最有利于地壳的内源性碳化的全局过程。

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