Trace Element Composition and Classification of the Chinga Iron Meteorite


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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.

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K. Litasov

Sobolev Institute of Geology and Mineralogy, Siberian Branch

编辑信件的主要联系方式.
Email: klitasov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

A. Ishikawa

University of Tokyo

Email: klitasov@igm.nsc.ru
日本, Tokyo

I. Bazhan

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: klitasov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

D. Ponomarev

Novosibirsk State University

Email: klitasov@igm.nsc.ru
俄罗斯联邦, Novosibirsk

T. Hirata

University of Tokyo

Email: klitasov@igm.nsc.ru
日本, Tokyo

N. Podgornykh

Central Siberian Geological Museum

Email: klitasov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

N. Pokhilenko

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: klitasov@igm.nsc.ru
俄罗斯联邦, Novosibirsk, 630090

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