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Utsukushi-ga-hara. (Preliminary Note.)", "subitem_title_language": "en"}]}, "item_type_id": "10", "owner": "1", "path": ["1677"], "permalink_uri": "http://hdl.handle.net/10091/4620", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2010-02-12"}, "publish_date": "2010-02-12", "publish_status": "0", "recid": "17226", "relation": {}, "relation_version_is_last": true, "title": ["美ケ原熔岩の自然残留磁気について(序報)"], "weko_shared_id": -1}
美ケ原熔岩の自然残留磁気について(序報)
http://hdl.handle.net/10091/4620
http://hdl.handle.net/10091/46209c3e07de-d8f4-4faa-995e-80a2065ea14a
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2010-02-12 | |||||
タイトル | ||||||
言語 | ja | |||||
タイトル | 美ケ原熔岩の自然残留磁気について(序報) | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | On the Natural Remanent Magnetism of the Lave of Mt. Utsukushi-ga-hara. (Preliminary Note.) | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
著者 |
松崎, 一
× 松崎, 一× 小林, 国夫× 百瀬, 寛一 |
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出版者 | ||||||
出版者 | 信州大学 | |||||
引用 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 信州大學紀要 (2): 1-7(1952) | |||||
書誌情報 |
信州大學紀要 巻 2, p. 1-7, 発行日 1952-07 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | It is the well known fact that the intensity of the natural remanent magnetism of the lava is generally much larger than that of the induced magnetism in the present geomagnetic field. However, the lava has been discovered on the high mountains, the ntensity of which is unusually several tenfolds larger than the ordinary value of the lava. In order to solve this fact, the writers have been engaged in studying the relations between the natural remanent magnetism and the thermo-remanent magnetism, taking the samples from the lava flow of Mt. Utsukushi-ga-hara. Collecting the samples which were continuously closed by each other in the same rock mass from the upper and the lower lava flow respectively, the writers measured both the directions and intensities of the natural and thermo-remanent magnetism of the samples in the same rock mass is not always uniform. However it also shows that the intensity of the thermo-remanent magnetism of the samples is almost constant. The writers discussed briefly about the causes of these results. | |||||
資源タイプ(コンテンツの種類) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Article | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00219843 | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |