Iron meteorites and their weathering products: high velocity resolution Mossbauer spectroscopy of the iron-bearing minerals

被引：12
|
作者：
Goryunov, Mikhail V. [1 ,2 ]
Yakovlev, Grigoriy A. [1 ]
Chukin, Andrei V. [3 ]
Grokhovsky, Victor I. [1 ]
Semionkin, Vladimir A. [1 ,2 ]
Oshtrakh, Michael I. [1 ,2 ]
机构：
[1] Ural Fed Univ, Inst Phys & Technol, Dept Phys Tech & Devices Qual Control, Ekaterinburg 620002, Russia
[2] Ural Fed Univ, Inst Phys & Technol, Dept Expt Phys, Ekaterinburg 620002, Russia
[3] Ural Fed Univ, Inst Phys & Technol, Dept Theoret Phys & Appl Math, Ekaterinburg 620002, Russia
来源：
EUROPEAN JOURNAL OF MINERALOGY | 2016年 / 28卷 / 03期
关键词：
iron meteorites; weathering; alpha-Fe(Ni; Co); alpha(2)-Fe(Ni; Co) and gamma-Fe(Ni; phases; magnetite; maghemite and goethite; siderite; Mossbauer spectroscopy; FE-NI ALLOYS;
D O I：
10.1127/ejm/2016/0028-2545
中图分类号：
P57 [矿物学];
学科分类号：
070901 ;
摘要：
The iron meteorites Anyujskij IIAB, Sikhote-Alin IIAB, Sterlitamak IIIAB, Aliskerovo IIIE-an and Dronino iron-ung and products of Dronino meteorite weathering in clay sand were studied using Mossbauer spectroscopy with a high velocity resolution. Components revealed in the complex Mossbauer spectra were related to corresponding iron-bearing minerals. A difference in the oxidation products of two Dronino fragments was observed. The presence of siderite was found in the external surface oxidation layer in the second fragment, which may be a result of goethite bioreduction in clay sand.
引用
收藏
页码：601 / 610
页数：10
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