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How to Confirm “Complete Zeroing” in TL Dating of Fault Movement -Case of the Higashiura Fault,Awaji Island in Japan-
http://hdl.handle.net/10105/394
http://hdl.handle.net/10105/394fb8968e9-7243-4bd1-b6ed-e34dda3e1af2
| 名前 / ファイル | ライセンス | アクション |
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| アイテムタイプ | 紀要論文 / Departmental Bulletin Paper(1) | |||||||||
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| 公開日 | 2010-06-10 | |||||||||
| タイトル | ||||||||||
| タイトル | How to Confirm “Complete Zeroing” in TL Dating of Fault Movement -Case of the Higashiura Fault,Awaji Island in Japan- | |||||||||
| 言語 | ||||||||||
| 言語 | eng | |||||||||
| キーワード | ||||||||||
| 主題 | Complete zeroing, TL dating, Fault movement, Higashiura Fault | |||||||||
| 資源タイプ | ||||||||||
| 資源タイプ | departmental bulletin paper | |||||||||
| 著者 |
HIRAGA, Shozo
× HIRAGA, Shozo
× NAGATOMO, Tsuneto
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| 抄録 | ||||||||||
| 内容記述タイプ | Abstract | |||||||||
| 内容記述 | An idea of "effective erasure depth(EED)" is introduced to confirm the so-called "zeroing" in TL dating of fault movement.EED is the depth from the grain surface to a boundary,outside/inside which the paleodose accumulated until faulting was completely/partially erased at the event. Applying this idea to TL dating of the Higashiura Fault,Awaji island in Japan, the zeroing of quartz was confirmed for fine grains collected from the highly and moderately fractured subzones,and the TL age of the fault movement was assessed as O.32±0.03Ma | |||||||||
| 書誌情報 |
奈良教育大学紀要. 自然科学 巻 44, 号 2, p. 17-25, 発行日 1995-11-24 |
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| ISSN | ||||||||||
| 収録物識別子タイプ | ISSN | |||||||||
| 収録物識別子 | 05472407 | |||||||||
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| 収録物識別子タイプ | NCID | |||||||||
| 収録物識別子 | AN00181070 | |||||||||
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| 出版タイプ | VoR | |||||||||
| 出版者 | ||||||||||
| 出版者 | 奈良教育大学 | |||||||||