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The trench-trench-trench type triple junction and tectonic evolution of Japan
https://doi.org/10.14945/00000342
https://doi.org/10.14945/0000034289367af8-3dac-475d-be60-12e001fbed86
名前 / ファイル | ライセンス | アクション |
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KJ00000102401.pdf (815.0 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2008-01-25 | |||||||
タイトル | ||||||||
言語 | en | |||||||
タイトル | The trench-trench-trench type triple junction and tectonic evolution of Japan | |||||||
言語 | ||||||||
言語 | eng | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | triple junction | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | plate tectonics | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | Neogene tectonics of Japan | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | bending of zonal structure | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | minimum curvature | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | Pacific Small Circle | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | Mogami Small Circle | |||||||
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 | |||||||
ID登録 | ||||||||
ID登録 | 10.14945/00000342 | |||||||
ID登録タイプ | JaLC | |||||||
著者 |
Niitsuma, Nobuaki
× Niitsuma, Nobuaki
WEKO
181
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書誌情報 |
Geoscience reports of Shizuoka University 巻 23, p. 1-8, 発行日 1996-07 |
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出版者 | ||||||||
出版者 | Shizuoka University. Institute of Geosciences | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 455 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | The topography around the trench-trench-trench triple junction off the Kanto Plain and Neogene tectonic evolution of the Japanese Island Arcs have been examined. The most important factors for the tectonics are the deformations of the subductive boundary around the triple junction for retention of the minimum curvature of subduction of the thick Pacific Plate along an irregular boundary with an uncinate process, created by the retreat of the Izu Trench on the Philippine Sea Plate. The Great Bend of the zonal structure in central Japan, the east-west compressional stress field in the Southwest Japan, and the tectonic evolution of northeast Honshu can be systematically explained with the deformations. | |||||||
ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03886298 | |||||||
NII論文ID | ||||||||
関連タイプ | isIdenticalTo | |||||||
識別子タイプ | NAID | |||||||
関連識別子 | 110000413369 | |||||||
NII書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AN00103190 | |||||||
フォーマット | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | application/pdf | |||||||
著者版フラグ | ||||||||
出版タイプ | VoR | |||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |