Surface rupture of the 2008 M6.9 Iwate-Miyagi Nairiku Earthquake at Aratozawa dam : Reverse fault reactivation of a late Miocene caldera-collapse normal fault
-
- OSOZAWA Soichi
- Department of Earth Sciences, Graduate School of Science, Tohoku University
Bibliographic Information
- Other Title
-
- 荒砥沢ダムにおける2008年岩手・宮城内陸地震(M6.9)の地表地震断層 : 後期中新世カルデラ縁正断層が再動した逆断層
- アラト ザワ ダム ニ オケル 2008ネン イワテ ミヤギ ナイリク ジシン M6 9 ノ チヒョウ ジシン ダンソウ コウキ チュウシンセイ カルデラエン セイ ダンソウ ガ サイドウ シタ ギャクダンソウ
Search this article
Abstract
The 2008 M6.9 Iwate-Miyagi Nairuku earthquake generated a reverse-fault surface rupture that was observed at the Aratozawa dam site area. This faulting reactivated a normal fault formed by late Miocene caldera collapse. The earthquake triggered numerous and voluminous landslides in the hanging wall of the fault, upstream of Aratozawa dam.
Journal
-
- Earth Science (Chikyu Kagaku)
-
Earth Science (Chikyu Kagaku) 63 (5), 321-326, 2009
The Association for the Geological Collaboration in Japan
- Tweet
Keywords
Details 詳細情報について
-
- CRID
- 1390001204234283392
-
- NII Article ID
- 110007359522
-
- NII Book ID
- AN00141269
-
- ISSN
- 21897212
- 03666611
-
- NDL BIB ID
- 10448567
-
- Text Lang
- ja
-
- Data Source
-
- JaLC
- NDL
- CiNii Articles
- KAKEN
-
- Abstract License Flag
- Disallowed