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Modeling of slow slip events along the deep subduction zone in the Kii Peninsula and Tokai regions, southwest Japan

Author
SHIBAZAKI, Bunichiro1 ; OBARA, Kazushige2 ; MATSUZAWA, Takanori3 ; HIROSE, Hitoshi3
[1] International Institute of Seismology and Earthquake Engineering, Tsukuba, Japan
[2] Earthquake Research Institute, University of Tokyo, Tokyo, Japan
[3] National Research Institute for Earth Science and Disaster Prevention, Tsukuba, Japan
Source

Journal of geophysical research. 2012, Vol 117, Num B6 ; B06311.1-B06311.15 ; ref : 1 p.1/4

ISSN
0148-0227
Scientific domain
Astronomy earth cosmic environment; Geology; Geophysics; Climatology, meteorology; Oceanography
Publisher
American Geophysical Union, Washington, DC
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Basse fréquence Court terme Déplacement Frottement Glissement Haute résolution Hypocentre Interface Modèle 3 dimensions Modélisation Plaque Simulation Vitesse Zone subduction Péninsule Kii Asie Extrême Orient Honshu Japon
Keyword (en)
low frequency Short term displacements friction slip high resolution hypocenter interfaces three-dimensional models Modeling plates simulation velocity subduction zones Kii Peninsula Asia Far East Honshu Japan
Keyword (es)
Corto plazo Alta resolucion Hipocentro Interfase Modelo 3 dimensiones Modelización Placa Simulación Velocidad Zona subducto Península Kii Asia Extremo Oriente Honshu Japón
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
26363701

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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