Magnetic Classification of Antarctic Achondrites
P(論文) The magnetic hysteresis curves and the thermomagnetic curves of 17 Antarctic achondrites are measured. The saturation magnetization (I_s) of 3 ureilites ranges 2.2-6.4emu/gm while I_s is smaller than 0.53emu/gm for 7 diogenites, 6 eucrites and 1 howardite. By the thermomagnetic analysis, the I...
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ftnipr:oai:nipr.repo.nii.ac.jp:00001102 2024-09-09T19:08:48+00:00 Magnetic Classification of Antarctic Achondrites Nagata, Takesi 1980-12 application/pdf https://nipr.repo.nii.ac.jp/record/1102/files/KJ00000011628.pdf eng eng Memoirs of National Institute of Polar Research. Special issue 17 219 232 AA00733561 https://nipr.repo.nii.ac.jp/record/1102/files/KJ00000011628.pdf 1980 ftnipr 2024-06-17T04:00:22Z P(論文) The magnetic hysteresis curves and the thermomagnetic curves of 17 Antarctic achondrites are measured. The saturation magnetization (I_s) of 3 ureilites ranges 2.2-6.4emu/gm while I_s is smaller than 0.53emu/gm for 7 diogenites, 6 eucrites and 1 howardite. By the thermomagnetic analysis, the I_s value of each achondrite is resolved into the saturation magnetization of kamacite, I_s (α), that of plessite, I_s (α+γ), that of taenite I_s (γ), and that of shreibersite, I_s (Ph). Results show that I_s (α)/I_s ≲ 0.40 for diogenites, whereas 1 ≳ I_s (α)/I_s ≳ 0.79 for eucrites and howardites, which indicate that Ni-content in metallic nickel-irons in diogenites is definitely larger than that in eucrites and howardites. On an I_s (α)/I_s versus I_s diagram, therefore, the three groups of achondrite are well separately grouped, just as so in the magnetic classification of chondrites. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Antarctic |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
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ftnipr |
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English |
description |
P(論文) The magnetic hysteresis curves and the thermomagnetic curves of 17 Antarctic achondrites are measured. The saturation magnetization (I_s) of 3 ureilites ranges 2.2-6.4emu/gm while I_s is smaller than 0.53emu/gm for 7 diogenites, 6 eucrites and 1 howardite. By the thermomagnetic analysis, the I_s value of each achondrite is resolved into the saturation magnetization of kamacite, I_s (α), that of plessite, I_s (α+γ), that of taenite I_s (γ), and that of shreibersite, I_s (Ph). Results show that I_s (α)/I_s ≲ 0.40 for diogenites, whereas 1 ≳ I_s (α)/I_s ≳ 0.79 for eucrites and howardites, which indicate that Ni-content in metallic nickel-irons in diogenites is definitely larger than that in eucrites and howardites. On an I_s (α)/I_s versus I_s diagram, therefore, the three groups of achondrite are well separately grouped, just as so in the magnetic classification of chondrites. departmental bulletin paper |
author |
Nagata, Takesi |
spellingShingle |
Nagata, Takesi Magnetic Classification of Antarctic Achondrites |
author_facet |
Nagata, Takesi |
author_sort |
Nagata, Takesi |
title |
Magnetic Classification of Antarctic Achondrites |
title_short |
Magnetic Classification of Antarctic Achondrites |
title_full |
Magnetic Classification of Antarctic Achondrites |
title_fullStr |
Magnetic Classification of Antarctic Achondrites |
title_full_unstemmed |
Magnetic Classification of Antarctic Achondrites |
title_sort |
magnetic classification of antarctic achondrites |
publishDate |
1980 |
url |
https://nipr.repo.nii.ac.jp/record/1102/files/KJ00000011628.pdf |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Memoirs of National Institute of Polar Research Polar Research |
genre_facet |
Antarc* Antarctic Memoirs of National Institute of Polar Research Polar Research |
op_relation |
Memoirs of National Institute of Polar Research. Special issue 17 219 232 AA00733561 https://nipr.repo.nii.ac.jp/record/1102/files/KJ00000011628.pdf |
_version_ |
1809823062106832896 |