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  1. 900 信州大学刊行物
  2. 信州大學紀要
  3. Vol. 02

美ケ原熔岩の自然残留磁気について(序報)

http://hdl.handle.net/10091/4620
9c3e07de-d8f4-4faa-995e-80a2065ea14a
名前 / ファイル ライセンス アクション
Shinshu_Bulletin02-01.pdf Shinshu_Bulletin02-01.pdf (453.4 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-02-12
タイトル
タイトル 美ケ原熔岩の自然残留磁気について(序報)
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
その他(別言語等)のタイトル
その他のタイトル On the Natural Remanent Magnetism of the Lave of Mt. Utsukushi-ga-hara.(Preliminary Note.)
著者 松崎, 一

× 松崎, 一

WEKO 49058

松崎, 一

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小林, 国夫

× 小林, 国夫

WEKO 49059

小林, 国夫

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百瀬, 寛一

× 百瀬, 寛一

WEKO 49060

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
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
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