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  1. D300 大学院環境学研究科
  2. D300a 雑誌掲載論文
  3. 学術雑誌

Long-term changes in the Coulomb failure function on inland active faults in southwest Japan due to east-west compression and interplate earthquakes

http://hdl.handle.net/2237/20457
8a9f3da7-b39a-4fbb-9824-b72a925b51ff
名前 / ファイル ライセンス アクション
Shikakura_Fukahata_Hirahara_JGR2014org.pdf Shikakura_Fukahata_Hirahara_JGR2014org.pdf (1.4 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2014-07-14
タイトル
タイトル Long-term changes in the Coulomb failure function on inland active faults in southwest Japan due to east-west compression and interplate earthquakes
著者 Shikakura, Yosuke

× Shikakura, Yosuke

WEKO 53383

Shikakura, Yosuke

Search repository
Fukahata, Yukitoshi

× Fukahata, Yukitoshi

WEKO 53384

Fukahata, Yukitoshi

Search repository
Hirahara, Kazuro

× Hirahara, Kazuro

WEKO 53385

Hirahara, Kazuro

Search repository
権利
権利情報 ©2013. American Geophysical Union.
キーワード
主題Scheme Other
主題 inland active fault
キーワード
主題Scheme Other
主題 Coulomb failure function
キーワード
主題Scheme Other
主題 viscoelasticity
キーワード
主題Scheme Other
主題 historical earthquake
キーワード
主題Scheme Other
主題 interplate earthquake along the Nankai Trough
キーワード
主題Scheme Other
主題 southwest Japan
抄録
内容記述 Inland earthquake activity in and around the Kinki region, southwest Japan, increases in the period from several decades before to about a decade after the occurrence of great interplate earthquakes along the Nankai Trough. To quantitatively investigate this relationship, we calculated long-term changes in the Coulomb failure function (ΔCFF) on inland active faults in this region with viscoelastic slip response functions. As sources for the change in CFF, we investigated east-west compression within the Niigata-Kobe Tectonic Zone (NKTZ), historical interplate earthquakes and interseismic locking along the Nankai Trough subduction zone, and historical inland earthquakes in this region. Among these sources, the NKTZ east-west compression is the primary cause of the long-term changes in CFF. The changes in CFF due to interplate earthquakes are mostly negative on reverse faults and positive on strike-slip faults. This result suggests that the inland reverse faulting activity mostly increases before interplate earthquakes and decreases after the earthquakes, whereas strike-slip activity is mostly suppressed before interplate earthquakes and increases thereafter. This suggestion is supported by spatiotemporal pattern of historical inland earthquakes if focal mechanisms of historical earthquakes correspond to fault geometries in the region. The calculated changes in CFF are usually consistent with the occurrence of historical inland earthquakes. If we use the change in shear stress instead of the change in CFF, this consistency is enhanced, which suggests low apparent coefficients of friction in this region.
内容記述タイプ Abstract
出版者
出版者 Wiley
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
ISSN
収録物識別子タイプ ISSN
収録物識別子 2169-9356
書誌情報 Journal of Geophysical Research: Solid Earth

巻 119, 号 1, p. 502-518, 発行日 2014-01
著者版フラグ
値 author
URI
識別子 http://dx.doi.org/10.1002/2013JB010156
識別子タイプ DOI
URI
識別子 http://hdl.handle.net/2237/20457
識別子タイプ HDL
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