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Iberulite : ウィキペディア英語版
Iberulite

Iberulites are a particular type of microspherulites that develop in the atmosphere (troposphere), finally falling to the earth's surface. The name comes from the Iberian Peninsula where they were discovered.〔Díaz-Hernández, J.L. (2000). (Aportaciones sólidas a la atmósfera originadas por un incendio forestal en el ámbito mediterráneo ). ''Estudios Geológicos'', 56: 153–161〕
== Definition ==

An iberulite is a ''co-association'' with axial geometry, consisting of well-defined mineral grains, together with non-crystalline compounds, structured around a coarse-grained core with a smectite rind, only one vortex and pinkish color, formed in the troposphere by complex aerosol-water-gas interactions.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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