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A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex
https://doi.org/10.15094/00003023
https://doi.org/10.15094/0000302343f8ac54-c101-48b7-b30a-3777e4a2ba41
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000044140 (842.7 kB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1998-10-01 | |||||
タイトル | ||||||
タイトル | A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | paleointensity | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Thelliers method | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | secondary magnetization | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | the Napier Complex | |||||
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 | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003023 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Ueno, Naoko
× Ueno, Naoko× Ogishima, Tomoko× Ishikawa, Naoto× Funaki, Minoru |
|||||
著者所属(英) | ||||||
en | ||||||
Natural Science Laboratory, Toyo University | ||||||
著者所属(英) | ||||||
en | ||||||
Mejiro Gakuen High School | ||||||
著者所属(英) | ||||||
en | ||||||
School of Earth Sciences, IHS, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Secondary magnetization produced during a thermal experiment in Thelliers' method was studied on 12 samples from the Mt. Riiser-Larsen area for that paleomagnetic data already been reported (N. ISHIKAWA and M. FUNAKI: Proc. NIPR Symp. Antarct. Geosci., 10, 79, 1997), and considered suitable for paleomagnetic study from the rock magnetic characteristics of samples. A remeasurement test of NRM on the same temperature step (NRM-check) as well as PTRM (PTRM-check) in air and in vacuum revealed secondary magnetization concerned with NRM and TRM which appeared at the same temperature, around 350℃, that would be explained by the oxidation of sulfide observed under a microscope. Secondary magnetization around 550℃ which appeared in air might also be caused by magneto-mineralogical change. These results are supported by the large variation of initial susceptibility around 300℃ and 550℃. Both the secondary magnetization of NRM and that of PTRM produced in vacuum were comparable to in air. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1130866X | |||||
書誌情報 |
Polar geoscience 巻 11, p. 125-131, 発行日 1998-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |