Paleoseismic study of the Kamishiro Fault on the northern segment of the Itoigawa–Shizuoka Tectonic Line, Japan

The M(w) 6.2 (Mj 6.8) Nagano (Japan) earthquake of 22 November 2014 produced a 9.3-km long surface rupture zone with a thrust-dominated displacement of up to 1.5 m, which duplicated the pre-existing Kamishiro Fault along the Itoigawa–Shizuoka Tectonic Line (ISTL), the plate-boundary between the Eura...

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Detalles Bibliográficos
Autores principales: Lin, Aiming, Sano, Mikako, Wang, Maomao, Yan, Bing, Bian, Di, Fueta, Ryoji, Hosoya, Takashi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Netherlands 2016
Materias:
Original Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5496973/
https://www.ncbi.nlm.nih.gov/pubmed/28729808
http://dx.doi.org/10.1007/s10950-016-9629-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5496973/
https://www.ncbi.nlm.nih.gov/pubmed/28729808
http://dx.doi.org/10.1007/s10950-016-9629-x

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