微x射线荧光定位在氧化铁结块中铁带的应用，评价其形成和反应速率

The Journal of the Geological Society of Japan Pub Date : 2022-01-15 DOI:10.5575/geosoc.2022.0008

N. Katsuta, S. Sirono, Ayako Umemura, Hirokazu Kawahara, H. Yoshida

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引用次数: 0

摘要

在沉积岩和火成岩中经常观察到氧化铁列色岗带，它们是在水岩相互作用的风化蚀变过程中形成的。本文采用微x射线荧光(μ -XRF)成像技术研究了侏罗纪纳瓦霍地区氧化铁结核中的铁带

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Applications of micro-X-ray fluorescence mapping to iron bands in iron-oxide concretion to evaluate its formation and reaction rate

: Fe oxide Liesegang bands have often been observed in sedimentary and igneous rocks, and they are formed during weathering and alteration by water–rock interactions. In this study, micro-X-ray ﬂuo rescence ( μ -XRF) mapping was used to study the Fe bands in an Fe oxide concretion from the Jurassic Navajo

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The Journal of the Geological Society of Japan

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