Supplementary Notes on the Magnetic Classification of Stony Meteorites

P(論文) A magnetic classification of stony meteorites on the basis of their saturation magnetization (I_s) and their major magnetic transition temperature (Θ_c) in the cooling process is revised by making use of recently reported chemical and petrographic data. The average values of (I_s in emu/gm, Θ_...

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Main Author: Nagata, Takesi
Language:English
Published: 1978
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/893/files/KJ00000011866.pdf
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00000893 2024-09-09T19:51:58+00:00 Supplementary Notes on the Magnetic Classification of Stony Meteorites Nagata, Takesi 1978-02 application/pdf https://nipr.repo.nii.ac.jp/record/893/files/KJ00000011866.pdf eng eng Memoirs of National Institute of Polar Research. Special issue 8 233 239 AA00733561 https://nipr.repo.nii.ac.jp/record/893/files/KJ00000011866.pdf 1978 ftnipr 2024-06-17T04:04:30Z P(論文) A magnetic classification of stony meteorites on the basis of their saturation magnetization (I_s) and their major magnetic transition temperature (Θ_c) in the cooling process is revised by making use of recently reported chemical and petrographic data. The average values of (I_s in emu/gm, Θ_c in ℃) of enstatite chondrites (E), bronzite chondrites (H), hypersthene chondrites (L), carbonaceous chondrites (C) and achondrites (aC) are given by (48.0,764), (30.9,653), (12.5,656), (9.7,562) and (0.3,788) respectively. As either or both I_s and Θ_c values of each groups are distinctly separated from one another, stony meteorites can be classified reasonably well on the I_s∿Θ_c diagram. departmental bulletin paper Other/Unknown Material Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description P(論文) A magnetic classification of stony meteorites on the basis of their saturation magnetization (I_s) and their major magnetic transition temperature (Θ_c) in the cooling process is revised by making use of recently reported chemical and petrographic data. The average values of (I_s in emu/gm, Θ_c in ℃) of enstatite chondrites (E), bronzite chondrites (H), hypersthene chondrites (L), carbonaceous chondrites (C) and achondrites (aC) are given by (48.0,764), (30.9,653), (12.5,656), (9.7,562) and (0.3,788) respectively. As either or both I_s and Θ_c values of each groups are distinctly separated from one another, stony meteorites can be classified reasonably well on the I_s∿Θ_c diagram. departmental bulletin paper
author Nagata, Takesi
spellingShingle Nagata, Takesi
Supplementary Notes on the Magnetic Classification of Stony Meteorites
author_facet Nagata, Takesi
author_sort Nagata, Takesi
title Supplementary Notes on the Magnetic Classification of Stony Meteorites
title_short Supplementary Notes on the Magnetic Classification of Stony Meteorites
title_full Supplementary Notes on the Magnetic Classification of Stony Meteorites
title_fullStr Supplementary Notes on the Magnetic Classification of Stony Meteorites
title_full_unstemmed Supplementary Notes on the Magnetic Classification of Stony Meteorites
title_sort supplementary notes on the magnetic classification of stony meteorites
publishDate 1978
url https://nipr.repo.nii.ac.jp/record/893/files/KJ00000011866.pdf
genre Memoirs of National Institute of Polar Research
Polar Research
genre_facet Memoirs of National Institute of Polar Research
Polar Research
op_relation Memoirs of National Institute of Polar Research. Special issue
8
233
239
AA00733561
https://nipr.repo.nii.ac.jp/record/893/files/KJ00000011866.pdf
_version_ 1809921312800374784