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The 2007 Noto Peninsula, Japan, Earthquake (Mw 6.7): Damage to Wooden Structures

2008; Seismological Society of America; Volume: 79; Issue: 1 Linguagem: Inglês

10.1785/gssrl.79.1.20

1938-2057

Masumi Yamada, Seong‐Chan Park, Toshiyuki Mori,

Earthquake and Disaster Impact Studies

Research Article| January 01, 2008 The 2007 Noto Peninsula, Japan, Earthquake (Mw 6.7): Damage to Wooden Structures Masumi Yamada; Masumi Yamada Kyoto University Gokasho, Uji, 611-0011, Japan masumi@eqh.dpri.kyoto-u.ac.jp (M.Y.) Search for other works by this author on: GSW Google Scholar Sun-Cheon Park; Sun-Cheon Park Kyoto University Gokasho, Uji, 611-0011, Japan masumi@eqh.dpri.kyoto-u.ac.jp (M.Y.) Search for other works by this author on: GSW Google Scholar Jim Mori Jim Mori Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2008) 79 (1): 20–24. https://doi.org/10.1785/gssrl.79.1.20 Article history first online: 14 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Masumi Yamada, Sun-Cheon Park, Jim Mori; The 2007 Noto Peninsula, Japan, Earthquake (Mw 6.7): Damage to Wooden Structures. Seismological Research Letters 2008;; 79 (1): 20–24. doi: https://doi.org/10.1785/gssrl.79.1.20 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search The 2007 Noto Peninsula earthquake (Mw 6.7, Mjma 6.9) produced strong shaking throughout central Japan with substantial damage to more than 14,500 buildings. The shallow event occurred close to the Japan Sea coast (37.22°N, 136.69°E, depth 11 km) on 25 March 2007 at 00:41:58 GMT. Analyses of seismic data showed that it was a thrust fault (striking northeast and dipping downward to the southeast) with dimensions of about 15 × 30 km2 (figure 1; Aoi and Sekiguchi 2007). There was no significant surface faulting from the earthquake but Global Positioning System measurements showed... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.