Magnetic Characteristics of Some Yamato Meteorites─Magnetic Classification of Stone Meteorites─
13 Yamato stone meteorites have been magnetically examined. They are one enstatite chondrite (E), 6 olivine-bronzite chondrites (H), 2 olivine-hypersthene chondrites (L), one carbonaceous chondrite (C) and 3 achondrites (aC). The intrinsic magnetic parameters of these stone meteorites obtained from...
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National Institute of Polar Research
1976
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ftnipr:oai:nipr.repo.nii.ac.jp:00000590 2023-05-15T17:10:59+02:00 Magnetic Characteristics of Some Yamato Meteorites─Magnetic Classification of Stone Meteorites─ Takesi Nagata Naoji Sugiura 1976-12 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=590 http://id.nii.ac.jp/1291/00000590/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=590&item_no=1&attribute_id=18&file_no=1 en eng National Institute of Polar Research Geophysical Institute, University of Tokyo https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=590 http://id.nii.ac.jp/1291/00000590/ AA00733470 Memoirs of National Institute of Polar Research. Ser. C, Earth sciences, 10, 30-58(1976-12) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=590&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1976 ftnipr 2022-11-12T19:41:26Z 13 Yamato stone meteorites have been magnetically examined. They are one enstatite chondrite (E), 6 olivine-bronzite chondrites (H), 2 olivine-hypersthene chondrites (L), one carbonaceous chondrite (C) and 3 achondrites (aC). The intrinsic magnetic parameters of these stone meteorites obtained from their magnetic hysteresis curves and thermomagnetic curves, together with those of other 7 known chondritic meteorites, are specifically examined in terms of the compositional and petrographical classification of stone meteorites. The saturation magnetization (I_s) and major magnetic transition temperature (Θ_c) in the cooling process can be taken as the representative magnetic parameters in the proposed magnetic classification of stone meteorites. In the I_s versus Θ_c diagram, those examined stone meteorites, 25 in total, are separated into groups namely, I_s (E) > I_s (H) > I_s (L) > I_s (aC), Θ_c (H and L) < Θ_c (E and aC) ≃ 770℃, I_s (C) ≃ I_s (L) but Θ_c (C) < 600℃ < Θ_c (L). Although the boundary between the L-group and the H-group is not sharp enough in the I_s-Θ_c diagram, the L-group chondrites contain a distinctly larger amount of plessite phase which can be magnetically identified. Report Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Yamato ENVELOPE(35.583,35.583,-71.417,-71.417) |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
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ftnipr |
language |
English |
description |
13 Yamato stone meteorites have been magnetically examined. They are one enstatite chondrite (E), 6 olivine-bronzite chondrites (H), 2 olivine-hypersthene chondrites (L), one carbonaceous chondrite (C) and 3 achondrites (aC). The intrinsic magnetic parameters of these stone meteorites obtained from their magnetic hysteresis curves and thermomagnetic curves, together with those of other 7 known chondritic meteorites, are specifically examined in terms of the compositional and petrographical classification of stone meteorites. The saturation magnetization (I_s) and major magnetic transition temperature (Θ_c) in the cooling process can be taken as the representative magnetic parameters in the proposed magnetic classification of stone meteorites. In the I_s versus Θ_c diagram, those examined stone meteorites, 25 in total, are separated into groups namely, I_s (E) > I_s (H) > I_s (L) > I_s (aC), Θ_c (H and L) < Θ_c (E and aC) ≃ 770℃, I_s (C) ≃ I_s (L) but Θ_c (C) < 600℃ < Θ_c (L). Although the boundary between the L-group and the H-group is not sharp enough in the I_s-Θ_c diagram, the L-group chondrites contain a distinctly larger amount of plessite phase which can be magnetically identified. |
format |
Report |
author |
Takesi Nagata Naoji Sugiura |
spellingShingle |
Takesi Nagata Naoji Sugiura Magnetic Characteristics of Some Yamato Meteorites─Magnetic Classification of Stone Meteorites─ |
author_facet |
Takesi Nagata Naoji Sugiura |
author_sort |
Takesi Nagata |
title |
Magnetic Characteristics of Some Yamato Meteorites─Magnetic Classification of Stone Meteorites─ |
title_short |
Magnetic Characteristics of Some Yamato Meteorites─Magnetic Classification of Stone Meteorites─ |
title_full |
Magnetic Characteristics of Some Yamato Meteorites─Magnetic Classification of Stone Meteorites─ |
title_fullStr |
Magnetic Characteristics of Some Yamato Meteorites─Magnetic Classification of Stone Meteorites─ |
title_full_unstemmed |
Magnetic Characteristics of Some Yamato Meteorites─Magnetic Classification of Stone Meteorites─ |
title_sort |
magnetic characteristics of some yamato meteorites─magnetic classification of stone meteorites─ |
publisher |
National Institute of Polar Research |
publishDate |
1976 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=590 http://id.nii.ac.jp/1291/00000590/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=590&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(35.583,35.583,-71.417,-71.417) |
geographic |
Yamato |
geographic_facet |
Yamato |
genre |
Memoirs of National Institute of Polar Research Polar Research |
genre_facet |
Memoirs of National Institute of Polar Research Polar Research |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=590 http://id.nii.ac.jp/1291/00000590/ AA00733470 Memoirs of National Institute of Polar Research. Ser. C, Earth sciences, 10, 30-58(1976-12) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=590&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766067820449234944 |