Nanohematite from Ferruginous Quartzites of Kursk Magnetic Anomaly According to Transmission Electron Microscopy Data
- 作者: Zhukhlistov A.P.1, Novikov V.M.1
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隶属关系:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- 期: 卷 63, 编号 1 (2018)
- 页面: 79-83
- 栏目: Real Structure of Crystals
- URL: https://journals.rcsi.science/1063-7745/article/view/192195
- DOI: https://doi.org/10.1134/S1063774518010224
- ID: 192195
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详细
Transmission electron microscopy study of ferruginous quartzite (jaspilites) from the Lebedinsky field of Kursk magnetic anomaly has revealed for the first time hematite nanoformations (about 10 nm in size), sp. gr. R3̅, which coexist with hematite, sp. gr. R3̅c, in the same crystallographic orientation or manifest themselves as individual nanoinclusions in the substrate of poorly crystallized magnetite. On the assumption that, in correspondence with the energy-dispersive X-ray analysis data, octahedral sites in the hematite structure can be occupied by only Fe cations, several structural models are proposed explain the hematite symmetry lowering to R3̅.
作者简介
A. Zhukhlistov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
编辑信件的主要联系方式.
Email: anzhu@igem.ru
俄罗斯联邦, Moscow, 109017
V. Novikov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: anzhu@igem.ru
俄罗斯联邦, Moscow, 109017
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