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Pressure effect on magnetic hysteresis parameters of single-domain magnetite contained in natural plagioclase crystal
https://doi.org/10.24517/00067018
https://doi.org/10.24517/00067018cc4fbbd3-472f-44b2-88ed-f2d72df83b2a
| 名前 / ファイル | ライセンス | アクション |
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SC-PR-USUI-Y-202-394.pdf (677.8 kB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||||
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| 公開日 | 2022-09-02 | |||||||
| タイトル | ||||||||
| タイトル | Pressure effect on magnetic hysteresis parameters of single-domain magnetite contained in natural plagioclase crystal | |||||||
| 言語 | ||||||||
| 言語 | eng | |||||||
| 資源タイプ | ||||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
| 資源タイプ | journal article | |||||||
| ID登録 | ||||||||
| ID登録 | 10.24517/00067018 | |||||||
| ID登録タイプ | JaLC | |||||||
| 著者 |
Sato, Masahiko
× Sato, Masahiko× Yamamoto, Yuhji× Nishioka, Takashi× Kodama, Kazuto× Mochizuki, Nobutatsu× Usui, Yoichi× Tsunakawa, Hideo |
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| 著者別表示 |
臼井, 洋一
× 臼井, 洋一
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| 提供者所属 | ||||||||
| 内容記述タイプ | Other | |||||||
| 内容記述 | 金沢大学理工研究域地球社会基盤学系 | |||||||
| 書誌情報 |
Geophysical Journal International 巻 202, 号 1, p. 394-401, 発行日 2015-05-02 |
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| ISSN | ||||||||
| 収録物識別子タイプ | ISSN | |||||||
| 収録物識別子 | 0956-540X | |||||||
| ISSN | ||||||||
| 収録物識別子タイプ | ISSN | |||||||
| 収録物識別子 | 1365-246X | |||||||
| NCID | ||||||||
| 収録物識別子タイプ | NCID | |||||||
| 収録物識別子 | AA10717798 | |||||||
| DOI | ||||||||
| 関連タイプ | isIdenticalTo | |||||||
| 識別子タイプ | DOI | |||||||
| 関連識別子 | 10.1093/gji/ggv154 | |||||||
| 出版者 | ||||||||
| 出版者 | Oxford University Press / The Royal Astronomical Society | |||||||
| 抄録 | ||||||||
| 内容記述タイプ | Abstract | |||||||
| 内容記述 | This study investigates pressure effects on the magnetic properties of non-interacting singledomain (SD) magnetite. Using a high-pressure cell specially designed for a Magnetic Property Measurement System, magnetic hysteresis measurements were conducted under high pressures of up to 1 GPa on natural plagioclase crystals containing much acicular SD magnetite. Coercivity and saturation magnetization were nearly constant with pressure, while saturation remanent magnetization and coercivity of remanence decreased with pressure at moderate rates of -8 per cent GPa-1 and -18 per cent GPa-1, respectively. These results suggest that temperature effects govern the magnetic behaviour of acicular SD magnetite grains in the middle and lower crusts. © The Authors 2015. | |||||||
| 権利 | ||||||||
| 権利情報 | Copyright © The Authors 2015. Published by Oxford University Press on behalf of The Royal Astronomical Society. | |||||||
| 著者版フラグ | ||||||||
| 出版タイプ | VoR | |||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||
| 関連URI | ||||||||
| 識別子タイプ | URI | |||||||
| 関連識別子 | https://academic.oup.com/gji/article/202/1/394/591883 | |||||||
| 関連名称 | https://academic.oup.com/gji/article/202/1/394/591883 | |||||||
| 関連URI | ||||||||
| 識別子タイプ | URI | |||||||
| 関連識別子 | https://academic.oup.com/gji | |||||||
| 関連名称 | https://academic.oup.com/gji | |||||||
| 関連URI | ||||||||
| 識別子タイプ | URI | |||||||
| 関連識別子 | http://www.oxfordjournals.org/ | |||||||
| 関連名称 | http://www.oxfordjournals.org/ | |||||||
