Item type |
学術雑誌論文 / Journal Article(1) |
公開日 |
2013-02-05 |
タイトル |
|
|
タイトル |
Precise aftershock distribution and crustal structure in and around the northern focal area of the 2008 Iwate-Miyagi Nairiku Earthquake |
キーワード |
|
|
主題Scheme |
Other |
|
主題 |
The 2008 Iwate-Miyagi Nairiku Earthquake |
キーワード |
|
|
主題Scheme |
Other |
|
主題 |
high-density seismic array observation |
キーワード |
|
|
主題Scheme |
Other |
|
主題 |
seismic tomography |
キーワード |
|
|
主題Scheme |
Other |
|
主題 |
aftershock distribution |
キーワード |
|
|
主題Scheme |
Other |
|
主題 |
fault reactivation |
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 |
journal article |
著者 |
Kurashimo, Eiji
Sato, Hiroshi
Abe, Susumu
Iwasaki, Takaya
Iidaka, Iidaka
Kato, Naoko
Koshiya, Shin
Kawanaka, Taku
Hirata, Naoshi
|
著者(機関) |
|
|
値 |
Earthquake Research Institute, the University of Tokyo |
著者(機関) |
|
|
値 |
Earthquake Research Institute, the University of Tokyo |
著者(機関) |
|
|
値 |
JGI, Inc. |
著者(機関) |
|
|
値 |
Earthquake Research Institute, the University of Tokyo |
著者(機関) |
|
|
値 |
Earthquake Research Institute, the University of Tokyo |
著者(機関) |
|
|
値 |
Earthquake Research Institute, the University of Tokyo |
著者(機関) |
|
|
値 |
Iwate University |
著者(機関) |
|
|
値 |
JGI, Inc. |
著者(機関) |
|
|
値 |
Earthquake Research Institute, the University of Tokyo |
登録日 |
|
|
日付 |
2013-02-05 |
書誌情報 |
Earth, planets and space
巻 63,
号 8,
p. 949-954,
発行日 2011-01-01
|
ISSN |
|
|
収録物識別子タイプ |
ISSN |
|
収録物識別子 |
1343-8832 |
Abstract |
|
|
内容記述タイプ |
Other |
|
内容記述 |
The 2008 Iwate-Miyagi Nairiku Earthquake (Mj 7.2) occurred on June 14, 2008, at the eastern flank of the Ou backbone range, in the central part of northern Honshu, Japan. In the northern part of the focal area, seismic reflection/refraction experiments conducted in 2006 and 2007 revealed a series of west-dipping faults. To investigate the relation between these faults and aftershocks, we conducted a high-density seismic array observation across the northern focal area. The arrival times of earthquakes were used in a joint inversion for earthquake locations and velocity structure. The Vp structure shows tilted blocks and the block boundaries coincide with the revealed west-dipping faults. These faults were interpreted to have formed during the Miocene extension. The aftershock distribution shows a concentration on a plane dipping westward approximately 40° beneath the eastern margin of the Ou backbone range. The zone of aftershock concentration can be correlated to the known range-bounding fault inferred from seismic profiling and does not coincide with the known active reverse fault (Dedana fault). These results indicate the significance of the potential source fault located along the boundary of the Ou backbone range. |
出版者 |
|
|
出版者 |
Terra Scientific Pub. Co |
権利 |
|
|
権利情報 |
Copyright c The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences; TERRAPUB. |
DOI |
|
|
関連タイプ |
isIdenticalTo |
|
|
識別子タイプ |
DOI |
|
|
関連識別子 |
10.5047/eps.2011.04.001 |
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 |