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上谷地遺跡における熱残留磁化獲得実験
http://hdl.handle.net/10295/1104
http://hdl.handle.net/10295/1104349be7ef-26d7-481a-9685-1014224f3e53
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
nist3.pdf (832.3 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||||||||
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| 公開日 | 2008-09-09 | |||||||||||||
| タイトル | ||||||||||||||
| タイトル | 上谷地遺跡における熱残留磁化獲得実験 | |||||||||||||
| その他のタイトル | ||||||||||||||
| その他のタイトル | Model experiment of thermoremanent magnetization at Uwayati site | |||||||||||||
| 言語 | ||||||||||||||
| 言語 | jpn | |||||||||||||
| 主題 | ||||||||||||||
| 主題Scheme | Other | |||||||||||||
| 主題 | thermoremanent magnetization | |||||||||||||
| 主題 | ||||||||||||||
| 主題Scheme | Other | |||||||||||||
| 主題 | archeomagnetism | |||||||||||||
| 主題 | ||||||||||||||
| 主題Scheme | Other | |||||||||||||
| 主題 | kiln | |||||||||||||
| 主題 | ||||||||||||||
| 主題Scheme | Other | |||||||||||||
| 主題 | temperature distribution | |||||||||||||
| 主題 | ||||||||||||||
| 主題Scheme | Other | |||||||||||||
| 主題 | susceptibility | |||||||||||||
| 主題 | ||||||||||||||
| 主題Scheme | Other | |||||||||||||
| 主題 | 上谷地遺跡 | |||||||||||||
| 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 | |||||||||||||
| 作成者 |
西谷, 忠師
× 西谷, 忠師
× 菊山, 浩喜
× NISHITANI, Tadashi
× KIKUYAMA, Hiroki
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| 内容記述 | ||||||||||||||
| 内容記述タイプ | Other | |||||||||||||
| 内容記述 | Experiment of acquisition of thermoremanent magnetization has been made at Uwayati site in two plain kilns and an open-air fire. The first aim of this experiment is to inspect whether remanent magnetization shows the true Earth's magnetic field. The second aim of it is to reveal the temperature distribution as a function of depth and time. This distribution indicates the relationship between the amount of heat and the dispersion of remanent magnetization. Considerable temperature differences exist according to the structure of kiln and the position of combustion. It reflects to the intensity and direction of remanent magnetization. Archeomagnetic specimens collected from wall side showed more accurate results than that from floor side of a kiln. If we are able to get samples from the wall side, we can estimate most suitable direction of remanent magnetization. This method is effective for a site that experience a low temperature. In an excavated site, it is necessary to reproduce wall faces to reveal the true direction of magnetization. We must pay attention to the location of sampling, because the effect of heat differs from place to place. The floor face covered with ash may receive smaller effect of heating. Susceptibility measurement indicates a rough idea of stability of magnetization. The intensity of remanent magnetization also shows the quality of data. In order to know the correct behavior of secular variation, we should examine a suitable location of sampling and develop the analysis method on the basis of the present experiment. |
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| 出版タイプ | ||||||||||||||
| 出版タイプ | VoR | |||||||||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||||||
| 書誌情報 |
秋田大学鉱山学部資源地学研究施設報告 号 61, p. 51-62, 発行日 1996-03-01 |
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| ISSN | ||||||||||||||
| 収録物識別子タイプ | ISSN | |||||||||||||
| 収録物識別子 | 09139907 | |||||||||||||
| NCID | ||||||||||||||
| 収録物識別子タイプ | NCID | |||||||||||||
| 収録物識別子 | AN1006497X | |||||||||||||
| 出版者 | ||||||||||||||
| 出版者 | 秋田大学鉱山学部附属資源地学研究施設 | |||||||||||||
