Trace Element Composition and Classification of the Chinga Iron Meteorite
- Авторлар: 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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Мекемелер:
- Sobolev Institute of Geology and Mineralogy, Siberian Branch
- University of Tokyo
- Novosibirsk State University
- Central Siberian Geological Museum
- Шығарылым: Том 478, № 1 (2018)
- Беттер: 62-66
- Бөлім: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/191945
- DOI: https://doi.org/10.1134/S1028334X18010063
- ID: 191945
Дәйексөз келтіру
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.
Авторлар туралы
K. Litasov
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Хат алмасуға жауапты Автор.
Email: klitasov@igm.nsc.ru
Ресей, Novosibirsk, 630090
A. Ishikawa
University of Tokyo
Email: klitasov@igm.nsc.ru
Жапония, Tokyo
I. Bazhan
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: klitasov@igm.nsc.ru
Ресей, Novosibirsk, 630090
D. Ponomarev
Novosibirsk State University
Email: klitasov@igm.nsc.ru
Ресей, Novosibirsk
T. Hirata
University of Tokyo
Email: klitasov@igm.nsc.ru
Жапония, Tokyo
N. Podgornykh
Central Siberian Geological Museum
Email: klitasov@igm.nsc.ru
Ресей, Novosibirsk, 630090
N. Pokhilenko
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: klitasov@igm.nsc.ru
Ресей, Novosibirsk, 630090
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