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11. 地殼の下層物質の密度にこ就いて
https://doi.org/10.15083/0000034320
https://doi.org/10.15083/00000343207be1b2b1-317f-40b9-b6ae-5bf367eb7606
名前 / ファイル | ライセンス | アクション |
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ji0222003.pdf (305.9 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2008-06-06 | |||||
タイトル | ||||||
タイトル | 11. 地殼の下層物質の密度にこ就いて | |||||
言語 | ja | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15083/0000034320 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | 11. Die Dichte der unter der Erdkruste liegenden Materie | |||||
著者 |
坪井, 忠二
× 坪井, 忠二 |
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著者別名 | ||||||
識別子 | 133429 | |||||
識別子Scheme | WEKO | |||||
姓名 | Tsuboi, Chuji | |||||
著者所属 | ||||||
著者所属 | 地球物理學敎室 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Der sogennante Helmertsche Kusteneffekt der Schwerekraftverteilung hangt, wenm er von der Airyschen Theorie ausgelegt wird, sowohl von der Dicke der Erdkruste als auch von der Dichte der unterliegenden Materie ab. Um die beobachtete Schwerekraftverteilung zu erklaren, lassen sie sich nicht eindeutig sondern nur paarweise bestimmen. Da man aus einigen anderen geophysikalischen Forschungen schlieszt dass die Erdkrustendicke etwa 60km ist, so muss die Dichte der subkrustalen Materie auch den dazu entsprechenden Wert, namlich 3.0 haben. | |||||
書誌情報 |
東京帝國大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, Tokyo Imperial University 巻 22, 号 2-4, p. 105-109, 発行日 1946-07-30 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00408972 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00029699 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
日本十進分類法 | ||||||
主題 | 453 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | 東京帝国大学地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute, Tokyo Imperial University |