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首页> 外文期刊>The American mineralogist >Eruption style and crystal size distributions: Crystallization of groundmass nanolites in the 2011 Shinmoedake eruption
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Eruption style and crystal size distributions: Crystallization of groundmass nanolites in the 2011 Shinmoedake eruption

机译:喷发风格和晶体尺寸分布:2011年ShinMoEdake爆发中的陆地纳米结晶

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摘要

Crystallization of groundmass minerals may record the physicochemical conditions of magmatic processes upon eruption and is thus a topic of interdisciplinary research in the disciplines of mineralogy, petrology, and volcanology. Recent studies have reported that the groundmass crystals of some volcanic rocks exhibit a break in their crystal size distribution (CSD) slopes that range from a few micrometers to hundreds of nanometers. The crystals consisting of the finer parts of the break were defined as nanolites. In this study, we report the presence of nanometer-scale crystals down to 1 nm in the pyroclasts of the 2011 eruption of Shinmoedake, the Kirishima volcano group, based on field emission-scanning electron microscopy (FE-SEM) and transmission electron microscopy (TEM).
机译:基础矿物的结晶可以在爆发时记录岩浆过程的物理化学条件,因此是矿物学,岩石学和火山学学科的跨学科研究的主题。 最近的研究报道说,一些火山岩的碎晶晶体在其晶体尺寸分布(CSD)斜坡上突破,其范围为几微米至数百纳米。 由突破细粒部分组成的晶体被定义为纳米岩。 在本研究中,基于场发射扫描电子显微镜(Fe-SEM)和透射电子显微镜(Fe-SEM)和透射电子显微镜(Fe-SEM)和透射电子显微镜( TEM)。

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