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Palaeo-stress fleld and tectonic evolution of the Mazhan graben area in the Yi-Shu fault zone of the Tan-Lu fault belt, East China
http://hdl.handle.net/10191/47871
http://hdl.handle.net/10191/47871bd94942d-22a7-4c91-9cfd-1df48d12bf12
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
13_29-42.pdf (2.6 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2017-08-31 | |||||
| タイトル | ||||||
| タイトル | Palaeo-stress fleld and tectonic evolution of the Mazhan graben area in the Yi-Shu fault zone of the Tan-Lu fault belt, East China | |||||
| タイトル | ||||||
| タイトル | Palaeo-stress fleld and tectonic evolution of the Mazhan graben area in the Yi-Shu fault zone of the Tan-Lu fault belt, East China | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Mazhan graben | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Yi-Shu fault zone | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Tan-Lu fault belt | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | stress field | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | East China | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||
| タイプ | departmental bulletin paper | |||||
| 著者 |
Zhang, Yan
× Zhang, Yan× Uemura, Takeshi |
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| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The Mazhan graben is located in the Yi-Shu fault zone, which is the middle segment of the Tan-Lu fault belt, one of the oldest and famous large fault belt in China. As a result of the structural analyses on the change of stress field and basin formation, it is clarified that tectonic evolution of the Manzhan graben can be divided into three stages, namely the pre-graben first stage in Palaeozoic to middle Jurassic, the graben-forming second stage in Cretaceous and the post-graben third stage in post-Palaeogene. Palaeo-stress field and tectonic movement have also changed from NW-SE compressive state resulted in thrusting with sinistral shear movement at the first stage, through NNE-SSW compressive state that formed "graben/horst/graben" as the final tectonic framework at the second stage, to NNW-SSE compression with sinistral shearing and rising of the area at the third stage. The fundamental dynamics of these large scale fault movement in East China would be affected by Kular palaeo-plate, however its precise study is problem in the future. | |||||
| 書誌情報 |
Science reports of Niigata University. (Geology) en : Science reports of Niigata University. (Geology) 巻 13, p. 29-42, 発行日 1998-03 |
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| 出版者 | ||||||
| 出版者 | 新潟大学理学部 | |||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 13491237 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AA11436808 | |||||
| 著者版フラグ | ||||||
| 値 | publisher | |||||
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Cite as
Zhang, Yan, Uemura, Takeshi, 1998, Palaeo-stress fleld and tectonic evolution of the Mazhan graben area in the Yi-Shu fault zone of the Tan-Lu fault belt, East China: 新潟大学理学部, 29–42 p.
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