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首页> 外文期刊>Journal of Volcanology and seismology >Microparticles of Native Metals, Sulfides, and Oxides in Andesitic Ashes of Karymskii Volcano
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Microparticles of Native Metals, Sulfides, and Oxides in Andesitic Ashes of Karymskii Volcano

机译:基本金属,硫化物和氧化物在Karymskii火山的胚胎中的微粒

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摘要

New data on accessory mineral phases found in ashes of the erupting Karymskii Volcano as microdispersed particles of native metals (Al, Fe, and Zn), intermetallic compounds, sulfides and oxides of iron, and carbonaceous substances are presented. Dominating submicron particles of native Al and Fe are largely confined to coarse-grained ash fractions; this is supported by extensive observations. The co-occurrence of iron oxide and sulfide particles of the same size possibly indicates extremely heterogeneous conditions of gas transport reactions during the eruption. The presence of native metals and carbonaceous compounds may attest to periods of a highly reducing environment in the fluid system supplying Karymskii Volcano.
机译:提出了爆发的Karymskii火山灰烬中发现的辅助矿物相的新数据作为天然金属(Al,Fe和Zn),金属间化合物,铁的金属间化合物,硫化物和氧化物和碳质物质。 占主导地位Al和Fe的亚微米颗粒主要限制在粗粒灰分中; 这是通过广泛的观察来支持的。 相同尺寸的氧化铁和硫化物颗粒的共同发生可能表明喷发过程中的气体传输反应的极其异质条件。 本地金属和碳质化合物的存在可以证明供应Karymskii火山的流体系统中的高度还原环境。

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