Magnetic analysis of Antactic ordinary chondrites and achondrites on the basis of a magnetic binary system model

Magnetic hysteresis cycles of 9 ordinary chondrites and 10 achondrites, collected mainly from Antarctica, are analyzed on the basis of a newly proposed model of a non-interactive magnetic binary system, by taking into account their thermomagnetic characteristics for identifying ferromagnetic phases...

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Main Authors: Takesi Nagata, Minoru Funaki
Format: Report
Language:English
Published: National Institute of Polar Research 1989
Subjects:
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http://id.nii.ac.jp/1291/00004493/
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00004493 2023-05-15T13:49:01+02:00 Magnetic analysis of Antactic ordinary chondrites and achondrites on the basis of a magnetic binary system model Takesi Nagata Minoru Funaki 1989-10 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4493 http://id.nii.ac.jp/1291/00004493/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4493&item_no=1&attribute_id=18&file_no=1 en eng National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4493 http://id.nii.ac.jp/1291/00004493/ AA10784627 Proceedings of the NIPR Symposium on Antarctic Meteorites, 2, 310-325(1989-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4493&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1989 ftnipr 2023-01-28T20:04:07Z Magnetic hysteresis cycles of 9 ordinary chondrites and 10 achondrites, collected mainly from Antarctica, are analyzed on the basis of a newly proposed model of a non-interactive magnetic binary system, by taking into account their thermomagnetic characteristics for identifying ferromagnetic phases involved. All the chondrites and achondrites examined consist of a high-coercivity (a) component and a low-coercivity (b) component. In ordinary chondrites, the (a) component is often identified to be tetrataenite (tetragonal-ordered crystal of FeNi) having an apparent coercive force H^<(a)>_C≳10^3 Oe (TT-type phase), while in other chondrites the (a) component comprises fine grains of shape-anisotropic single-domain structure (A. SD-type phase) having H^<(a)>_C=(2∿5)×10^2 Oe. The (b) component consists of mostly multi-domain grains of kamacite and/or taenite of H^<(b)>_C≲20 Oe. In most achondrites, the (a) component comprises A. SD-type phase of H^<(a)>_C=(2∿5)×10^2 Oe except a special case consisting of a small amount of tetrataenite. The structure of the (b) component in achondrites is the same as in ordinary chondrites. An anomalous hump-shape rise in saturation magnetization (I_s) between 330℃ and Curie point of taenite (540∿590℃) during the initial heating process is found in diogenites and a eucrite. The thermomagnetic hump is considered here to be due to an increase of A. SD-type phase of taenite associated with a relatively smaller increase of the (b) component multi-domain phase. However, a possible metallographical interpretation of the hump phenomenon has not yet been obtained. Report Antarc* Antarctica National Institute of Polar Research Repository, Japan Curie Point ENVELOPE(-63.483,-63.483,-64.833,-64.833) The Hump ENVELOPE(-63.250,-63.250,-64.367,-64.367)
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description Magnetic hysteresis cycles of 9 ordinary chondrites and 10 achondrites, collected mainly from Antarctica, are analyzed on the basis of a newly proposed model of a non-interactive magnetic binary system, by taking into account their thermomagnetic characteristics for identifying ferromagnetic phases involved. All the chondrites and achondrites examined consist of a high-coercivity (a) component and a low-coercivity (b) component. In ordinary chondrites, the (a) component is often identified to be tetrataenite (tetragonal-ordered crystal of FeNi) having an apparent coercive force H^<(a)>_C≳10^3 Oe (TT-type phase), while in other chondrites the (a) component comprises fine grains of shape-anisotropic single-domain structure (A. SD-type phase) having H^<(a)>_C=(2∿5)×10^2 Oe. The (b) component consists of mostly multi-domain grains of kamacite and/or taenite of H^<(b)>_C≲20 Oe. In most achondrites, the (a) component comprises A. SD-type phase of H^<(a)>_C=(2∿5)×10^2 Oe except a special case consisting of a small amount of tetrataenite. The structure of the (b) component in achondrites is the same as in ordinary chondrites. An anomalous hump-shape rise in saturation magnetization (I_s) between 330℃ and Curie point of taenite (540∿590℃) during the initial heating process is found in diogenites and a eucrite. The thermomagnetic hump is considered here to be due to an increase of A. SD-type phase of taenite associated with a relatively smaller increase of the (b) component multi-domain phase. However, a possible metallographical interpretation of the hump phenomenon has not yet been obtained.
format Report
author Takesi Nagata
Minoru Funaki
spellingShingle Takesi Nagata
Minoru Funaki
Magnetic analysis of Antactic ordinary chondrites and achondrites on the basis of a magnetic binary system model
author_facet Takesi Nagata
Minoru Funaki
author_sort Takesi Nagata
title Magnetic analysis of Antactic ordinary chondrites and achondrites on the basis of a magnetic binary system model
title_short Magnetic analysis of Antactic ordinary chondrites and achondrites on the basis of a magnetic binary system model
title_full Magnetic analysis of Antactic ordinary chondrites and achondrites on the basis of a magnetic binary system model
title_fullStr Magnetic analysis of Antactic ordinary chondrites and achondrites on the basis of a magnetic binary system model
title_full_unstemmed Magnetic analysis of Antactic ordinary chondrites and achondrites on the basis of a magnetic binary system model
title_sort magnetic analysis of antactic ordinary chondrites and achondrites on the basis of a magnetic binary system model
publisher National Institute of Polar Research
publishDate 1989
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4493
http://id.nii.ac.jp/1291/00004493/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4493&item_no=1&attribute_id=18&file_no=1
long_lat ENVELOPE(-63.483,-63.483,-64.833,-64.833)
ENVELOPE(-63.250,-63.250,-64.367,-64.367)
geographic Curie Point
The Hump
geographic_facet Curie Point
The Hump
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4493
http://id.nii.ac.jp/1291/00004493/
AA10784627
Proceedings of the NIPR Symposium on Antarctic Meteorites, 2, 310-325(1989-10)
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4493&item_no=1&attribute_id=18&file_no=1
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