Horizontal sliding of kilometre-scale hot spring area during the 2016 Kumamoto earthquake

We report horizontal sliding of the kilometre-scale geologic block under the Aso hot springs (Uchinomaki area) caused by vibrations from the 2016 Kumamoto earthquake (Mw 7.0). Direct borehole observations demonstrate the sliding along the horizontal geological formation at ~50 m depth, which is wher...

Descripción completa

Detalles Bibliográficos
Autores principales: Tsuji, Takeshi, Ishibashi, Jun’ichiro, Ishitsuka, Kazuya, Kamata, Ryuichi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5317158/
https://www.ncbi.nlm.nih.gov/pubmed/28218298
http://dx.doi.org/10.1038/srep42947

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5317158/
https://www.ncbi.nlm.nih.gov/pubmed/28218298
http://dx.doi.org/10.1038/srep42947

Ejemplares similares