Trace Element Composition and Classification of the Chinga Iron Meteorite


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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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