Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake
Large subduction zone earthquakes like the M 9.0 Tohoku earthquake of 2011 are followed by transient surface deformation. Here, the authors show this to be caused by rapid flow taking place in the asthenosphere due to temporarily decreased viscosity because of coseismic stress.
Guardado en:
Autores principales: | , , , , , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2019
|
Materias: | |
Acceso en línea: | https://doaj.org/article/542f503d09464e1ab52c72d38500b8d4 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:542f503d09464e1ab52c72d38500b8d4 |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:542f503d09464e1ab52c72d38500b8d42021-12-02T17:32:40ZRapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake10.1038/s41467-019-08984-72041-1723https://doaj.org/article/542f503d09464e1ab52c72d38500b8d42019-03-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-08984-7https://doaj.org/toc/2041-1723Large subduction zone earthquakes like the M 9.0 Tohoku earthquake of 2011 are followed by transient surface deformation. Here, the authors show this to be caused by rapid flow taking place in the asthenosphere due to temporarily decreased viscosity because of coseismic stress.Ryoichiro AgataSylvain D. BarbotKohei FujitaMamoru HyodoTakeshi IinumaRyoko NakataTsuyoshi IchimuraTakane HoriNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-11 (2019) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Science Q |
spellingShingle |
Science Q Ryoichiro Agata Sylvain D. Barbot Kohei Fujita Mamoru Hyodo Takeshi Iinuma Ryoko Nakata Tsuyoshi Ichimura Takane Hori Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake |
description |
Large subduction zone earthquakes like the M 9.0 Tohoku earthquake of 2011 are followed by transient surface deformation. Here, the authors show this to be caused by rapid flow taking place in the asthenosphere due to temporarily decreased viscosity because of coseismic stress. |
format |
article |
author |
Ryoichiro Agata Sylvain D. Barbot Kohei Fujita Mamoru Hyodo Takeshi Iinuma Ryoko Nakata Tsuyoshi Ichimura Takane Hori |
author_facet |
Ryoichiro Agata Sylvain D. Barbot Kohei Fujita Mamoru Hyodo Takeshi Iinuma Ryoko Nakata Tsuyoshi Ichimura Takane Hori |
author_sort |
Ryoichiro Agata |
title |
Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake |
title_short |
Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake |
title_full |
Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake |
title_fullStr |
Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake |
title_full_unstemmed |
Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake |
title_sort |
rapid mantle flow with power-law creep explains deformation after the 2011 tohoku mega-quake |
publisher |
Nature Portfolio |
publishDate |
2019 |
url |
https://doaj.org/article/542f503d09464e1ab52c72d38500b8d4 |
work_keys_str_mv |
AT ryoichiroagata rapidmantleflowwithpowerlawcreepexplainsdeformationafterthe2011tohokumegaquake AT sylvaindbarbot rapidmantleflowwithpowerlawcreepexplainsdeformationafterthe2011tohokumegaquake AT koheifujita rapidmantleflowwithpowerlawcreepexplainsdeformationafterthe2011tohokumegaquake AT mamoruhyodo rapidmantleflowwithpowerlawcreepexplainsdeformationafterthe2011tohokumegaquake AT takeshiiinuma rapidmantleflowwithpowerlawcreepexplainsdeformationafterthe2011tohokumegaquake AT ryokonakata rapidmantleflowwithpowerlawcreepexplainsdeformationafterthe2011tohokumegaquake AT tsuyoshiichimura rapidmantleflowwithpowerlawcreepexplainsdeformationafterthe2011tohokumegaquake AT takanehori rapidmantleflowwithpowerlawcreepexplainsdeformationafterthe2011tohokumegaquake |
_version_ |
1718380247537156096 |