Study of metallic Fe-Ni-Co alloy and stony part isolated from Seymchan meteorite using X-ray diffraction, magnetization measurement and Mössbauer spectroscopy

Author:

Oshtrakh M.I.,Maksimova A.A.,Goryunov M.V.,Petrova E.V.,Felner I.,Chukin A.V.,Grokhovsky V.I.

Funder

Institute of Physics and Technology, Ural Federal University

Ekaterinburg, Russian Federation

Ministry of Education and Science of the Russian Federation

Government of the Russian Federation

Publisher

Elsevier BV

Subject

Inorganic Chemistry,Organic Chemistry,Spectroscopy,Analytical Chemistry

Reference31 articles.

1. Seymchan: a main group pallasite – not an iron meteorite;van Niekerk;Meteorit. & Planet. Sci.,2007

2. Main-group pallasites: thermal history, relationship to IIIAB irons, and origin;Yang;Geochim. Cosmochim. Acta,2010

3. Study of 57Fe occupying the M1 and M2 sites in olivine from pallasites Omolon and Seymchan using Mössbauer spectroscopy;Oshtrakh;Meteorit. & Planet. Sci.,2010

4. Study of olivines from Omolon and Seymchan meteorites using X-ray diffraction and Mössbauer spectroscopy with a high velocity resolution;Oshtrakh,2012

5. Variations in quadrupole splitting of the 57Fe in the M1 and M2 sites of meteoritic olivines with different origin;Oshtrakh;Hyperfine Interact.,2013

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