The near-field tsunami amplitudes caused by submarine landslides and slumps spreading in two orthogonal directions
- Author
- HAYIR, Abdul1
[1] Division of Mechanics, Civil Engineering Department, Istanbul Technical University, 34469 Maslak, Istanbul, Turkey - Source
Ocean engineering. 2006, Vol 33, Num 5-6, pp 654-664, 11 p ; ref : 16 ref
- CODEN
- OCENBQ
- ISSN
- 0029-8018
- Scientific domain
- Civil engineering; Oceanography
- Publisher
- Elsevier, Amsterdam
- Publication country
- Netherlands
- Document type
- Article
- Language
- English
- Author keyword
- Fast Fourier transform Fourier transform Landslides and slumps Laplace equation Laplace transform Near-field tsunami amplitudes Slow earthquakes Tsunamis Wave focusing
- Keyword (fr)
- Affaissement Champ proche Dynamique océanique Formulation Glissement terrain Modèle mathématique Séisme Transformation Fourier Transformation Laplace Tsunami
- Keyword (en)
- Land subsidence near-field Ocean dynamics Formulation landslides mathematical models earthquakes Fourier transformation Laplace transformations tsunamis
- Keyword (es)
- Hundimiento Campo próximo Dinámica oceánica Formulación Desmoronamiento tierra Modelo matemático Sismo Transformación Laplace Tsunami
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02B Physics of the oceans / 001E02B02 Dynamics of the ocean (upper and deep oceans)
- Discipline
- External geophysics
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 17558953
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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DOI
10.1016/j.oceaneng.2005.05.010 
https://dx.doi.org/10.1016/j.oceaneng.2005.05.010
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