Email this article Trace Element Composition and Classification of the Chinga Iron Meteorite
- Authors: 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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Affiliations:
- Sobolev Institute of Geology and Mineralogy, Siberian Branch
- University of Tokyo
- Novosibirsk State University
- Central Siberian Geological Museum
- Issue: Vol 478, No 1 (2018)
- Pages: 62-66
- Section: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/191945
- DOI: https://doi.org/10.1134/S1028334X18010063
- ID: 191945
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Abstract
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.
About the authors
K. D. Litasov
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Author for correspondence.
Email: klitasov@igm.nsc.ru
Russian Federation, Novosibirsk, 630090
A. Ishikawa
University of Tokyo
Email: klitasov@igm.nsc.ru
Japan, Tokyo
I. S. Bazhan
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: klitasov@igm.nsc.ru
Russian Federation, Novosibirsk, 630090
D. S. Ponomarev
Novosibirsk State University
Email: klitasov@igm.nsc.ru
Russian Federation, Novosibirsk
T. Hirata
University of Tokyo
Email: klitasov@igm.nsc.ru
Japan, Tokyo
N. M. Podgornykh
Central Siberian Geological Museum
Email: klitasov@igm.nsc.ru
Russian Federation, Novosibirsk, 630090
N. P. Pokhilenko
Sobolev Institute of Geology and Mineralogy, Siberian Branch
Email: klitasov@igm.nsc.ru
Russian Federation, Novosibirsk, 630090
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