Magnetic analysis of an Antarctic mesosiderite, ALH-77219

Magnetic analyses are made on an Antarctic mesosiderite ALH-77219,and chemical analyses of metallic grains in the mesosiderite are carried out with the aid of an EPMA. The EPMA analyses show that the metallic phases in ALH-77219 are composed of kamacite of 5-6wt% Ni and taenite of about 50wt% Ni. Th...

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Main Authors: Takesi Nagata, Minoru Funaki
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 1983
Subjects:
Online Access:https://doi.org/10.15094/00008363
https://doaj.org/article/72a9dd43cda94b8b816f3c8dc835d570
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spelling ftdoajarticles:oai:doaj.org/article:72a9dd43cda94b8b816f3c8dc835d570 2023-05-15T14:02:14+02:00 Magnetic analysis of an Antarctic mesosiderite, ALH-77219 Takesi Nagata Minoru Funaki 1983-09-01T00:00:00Z https://doi.org/10.15094/00008363 https://doaj.org/article/72a9dd43cda94b8b816f3c8dc835d570 EN JA eng jpn National Institute of Polar Research https://doi.org/10.15094/00008363 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00008363 0085-7289 2432-079X https://doaj.org/article/72a9dd43cda94b8b816f3c8dc835d570 Antarctic Record, Iss 79, Pp 1-10 (1983) Geography (General) G1-922 article 1983 ftdoajarticles https://doi.org/10.15094/00008363 2022-12-31T11:46:32Z Magnetic analyses are made on an Antarctic mesosiderite ALH-77219,and chemical analyses of metallic grains in the mesosiderite are carried out with the aid of an EPMA. The EPMA analyses show that the metallic phases in ALH-77219 are composed of kamacite of 5-6wt% Ni and taenite of about 50wt% Ni. The thermomagnetic analyses show that the mesosiderite ALH-77219 contains kamacite phase of about 6wt% Ni on average of 19.3% in weight and taenite phase of about 54wt% Ni on average of 6.3% in weight. The major parts of the taenite phase are of the superlattice structure of tetrataenite, which has a large magnetic anisotropy. Article in Journal/Newspaper Antarc* Antarctic Directory of Open Access Journals: DOAJ Articles Antarctic
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
Japanese
topic Geography (General)
G1-922
spellingShingle Geography (General)
G1-922
Takesi Nagata
Minoru Funaki
Magnetic analysis of an Antarctic mesosiderite, ALH-77219
topic_facet Geography (General)
G1-922
description Magnetic analyses are made on an Antarctic mesosiderite ALH-77219,and chemical analyses of metallic grains in the mesosiderite are carried out with the aid of an EPMA. The EPMA analyses show that the metallic phases in ALH-77219 are composed of kamacite of 5-6wt% Ni and taenite of about 50wt% Ni. The thermomagnetic analyses show that the mesosiderite ALH-77219 contains kamacite phase of about 6wt% Ni on average of 19.3% in weight and taenite phase of about 54wt% Ni on average of 6.3% in weight. The major parts of the taenite phase are of the superlattice structure of tetrataenite, which has a large magnetic anisotropy.
format Article in Journal/Newspaper
author Takesi Nagata
Minoru Funaki
author_facet Takesi Nagata
Minoru Funaki
author_sort Takesi Nagata
title Magnetic analysis of an Antarctic mesosiderite, ALH-77219
title_short Magnetic analysis of an Antarctic mesosiderite, ALH-77219
title_full Magnetic analysis of an Antarctic mesosiderite, ALH-77219
title_fullStr Magnetic analysis of an Antarctic mesosiderite, ALH-77219
title_full_unstemmed Magnetic analysis of an Antarctic mesosiderite, ALH-77219
title_sort magnetic analysis of an antarctic mesosiderite, alh-77219
publisher National Institute of Polar Research
publishDate 1983
url https://doi.org/10.15094/00008363
https://doaj.org/article/72a9dd43cda94b8b816f3c8dc835d570
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Antarctic Record, Iss 79, Pp 1-10 (1983)
op_relation https://doi.org/10.15094/00008363
https://doaj.org/toc/0085-7289
https://doaj.org/toc/2432-079X
doi:10.15094/00008363
0085-7289
2432-079X
https://doaj.org/article/72a9dd43cda94b8b816f3c8dc835d570
op_doi https://doi.org/10.15094/00008363
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