Trace Element Composition and Classification of the Chinga Iron Meteorite
- Авторы: Litasov K.D.1, Ishikawa A.2, Bazhan I.S.1, Ponomarev D.S.3, Hirata T.2, Podgornykh N.M.4, Pokhilenko N.P.1
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Учреждения:
- Sobolev Institute of Geology and Mineralogy, Siberian Branch
- University of Tokyo
- Novosibirsk State University
- Central Siberian Geological Museum
- Выпуск: Том 478, № 1 (2018)
- Страницы: 62-66
- Раздел: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/191945
- DOI: https://doi.org/10.1134/S1028334X18010063
- ID: 191945
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Аннотация
A complete microelement analysis of the Chinga meteorite was performed, and the possibility of attributing it together with a number of other iron meteorites into the IVC subgroup, which is transition between IVA and IVB is proposed.
Об авторах
K. Litasov
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Автор, ответственный за переписку.
Email: klitasov@igm.nsc.ru
Россия, Novosibirsk, 630090
A. Ishikawa
University of Tokyo
Email: klitasov@igm.nsc.ru
Япония, Tokyo
I. Bazhan
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: klitasov@igm.nsc.ru
Россия, Novosibirsk, 630090
D. Ponomarev
Novosibirsk State University
Email: klitasov@igm.nsc.ru
Россия, Novosibirsk
T. Hirata
University of Tokyo
Email: klitasov@igm.nsc.ru
Япония, Tokyo
N. Podgornykh
Central Siberian Geological Museum
Email: klitasov@igm.nsc.ru
Россия, Novosibirsk, 630090
N. Pokhilenko
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: klitasov@igm.nsc.ru
Россия, Novosibirsk, 630090
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