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The western extension of the fault can be traced as far as Nakazima and Yanagisima, about 2km north of Koyama mati where, along the fault, the Misaka series thrusts over not only the Asigara beds but also a little younger Plio-Pleistocene(?) Yanagisima beds. An exposure of the fault at Nakazima shows that a green, altered andesite of the Misaka series rests on a nearly-horizonatally bedded, pumiceous tuffs and sands of the Yanagisima beds, with fault-breccias about 2m thick between them. The faultplane, which is represented by a flat, thin film of fault-gouge sandwiched in between the fault-breccias, dips about 45° north with an east-west strike. The fault does not cut the lower-Pleistocene Yuhune beds which are extensively distributed thereabouts, consisting of gravels and tuffaceous sands. 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28. 神繩衝上斷層の西翼に就いて
https://doi.org/10.15083/0000034363
https://doi.org/10.15083/0000034363140a5af4-7a62-4540-bf1b-71a399aed858
名前 / ファイル | ライセンス | アクション |
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ji0203003.pdf (1.6 MB)
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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 | 28. 神繩衝上斷層の西翼に就いて | |||||
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 | 10.15083/0000034363 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | 28. Note on the West Wing of Kannawa Thrust-Fault | |||||
著者 |
津屋, 弘逵
× 津屋, 弘逵 |
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著者別名 | ||||||
識別子 | 133523 | |||||
識別子Scheme | WEKO | |||||
姓名 | Tsuya, Hiromichi | |||||
著者所属 | ||||||
著者所属 | 地震研究所 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The Kannawa thrust-fault, along which the lower-Pliocene Asigara beds in the area immediate northeast of the Hakone volcano are overthrusted from the north by the Miocene Misaka series of the Tanzawa Mountainland, runs nearly in an east-west direction for a distance of more than 15km, crossing the valley of the Kawati-gawa, the main tributary of the Sakawa-gawa, at Yamaitiba. The western extension of the fault can be traced as far as Nakazima and Yanagisima, about 2km north of Koyama mati where, along the fault, the Misaka series thrusts over not only the Asigara beds but also a little younger Plio-Pleistocene(?) Yanagisima beds. An exposure of the fault at Nakazima shows that a green, altered andesite of the Misaka series rests on a nearly-horizonatally bedded, pumiceous tuffs and sands of the Yanagisima beds, with fault-breccias about 2m thick between them. The faultplane, which is represented by a flat, thin film of fault-gouge sandwiched in between the fault-breccias, dips about 45° north with an east-west strike. The fault does not cut the lower-Pleistocene Yuhune beds which are extensively distributed thereabouts, consisting of gravels and tuffaceous sands. With these facts in mind, it is suggested that the Kannawa thrust-fault may be either latest Pliocene or earliest Pleistocene. | |||||
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 20, 号 3, p. 322-336, 発行日 1942-11-15 |
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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 |