A hydroelastic stationary problem on the tsunami waves generation
Žurnal vyčislitelʹnoj matematiki i matematičeskoj fiziki, Tome 44 (2004) no. 11, pp. 2084-2093 Cet article a éte moissonné depuis la source Math-Net.Ru

Voir la notice de l'article

@article{ZVMMF_2004_44_11_a13,
     author = {R. Gonz\'alez-Gonz\'alez and S. Sekerzh-Zenkovich},
     title = {A hydroelastic stationary problem on the tsunami waves generation},
     journal = {\v{Z}urnal vy\v{c}islitelʹnoj matematiki i matemati\v{c}eskoj fiziki},
     pages = {2084--2093},
     year = {2004},
     volume = {44},
     number = {11},
     language = {en},
     url = {http://geodesic.mathdoc.fr/item/ZVMMF_2004_44_11_a13/}
}
TY  - JOUR
AU  - R. González-González
AU  - S. Sekerzh-Zenkovich
TI  - A hydroelastic stationary problem on the tsunami waves generation
JO  - Žurnal vyčislitelʹnoj matematiki i matematičeskoj fiziki
PY  - 2004
SP  - 2084
EP  - 2093
VL  - 44
IS  - 11
UR  - http://geodesic.mathdoc.fr/item/ZVMMF_2004_44_11_a13/
LA  - en
ID  - ZVMMF_2004_44_11_a13
ER  - 
%0 Journal Article
%A R. González-González
%A S. Sekerzh-Zenkovich
%T A hydroelastic stationary problem on the tsunami waves generation
%J Žurnal vyčislitelʹnoj matematiki i matematičeskoj fiziki
%D 2004
%P 2084-2093
%V 44
%N 11
%U http://geodesic.mathdoc.fr/item/ZVMMF_2004_44_11_a13/
%G en
%F ZVMMF_2004_44_11_a13
R. González-González; S. Sekerzh-Zenkovich. A hydroelastic stationary problem on the tsunami waves generation. Žurnal vyčislitelʹnoj matematiki i matematičeskoj fiziki, Tome 44 (2004) no. 11, pp. 2084-2093. http://geodesic.mathdoc.fr/item/ZVMMF_2004_44_11_a13/

[1] Rod'yapolskii G. S., “Vozbuzhdenie dlinnoi gravitatsionnoi volny v okeane seismicheskim istochnikom v kore”, Izv. AN SSSR. Fiz. Zemli, 1968, no. 1, 7–24

[2] Zvolinskii N. V., Nikitin I. S., Sekerzh-Zenkovich S. Ya., “Vozbuzhdenie voln tsunami i voln Releya garmonicheskim tsentrom rasshireniya”, Izv. AN SSSR. Fiz. Zemli, 1991, no. 2, 34–44

[3] Kravtsov A. V., Sekerzh-Zenkovich S. Ya., “Vozbuzhdenie voln tsunami i voln Releya sfericheskim tsentrom rasshireniya”, Vulkanologiya i seismologiya, 1995, no. 2, 93–100 | MR

[4] Alexeev A. S., Gusyakov V. K., “Numerical modelling of tsunami and seismic surface waves generation by submarine earthquake”, Tsunami Res. Symposium. Bull. Roy. Soc. N. Z., 1976, no. 15, 243–251

[5] Kanamori H., “Mechanism of tsunami earthquakes”, Phys. Earth Planet. Inter., 1972, no. 6, 349–359

[6] Yamashita T., Sato R., “Generation of tsunami by a fault model”, J. Phys. Earth, 1974, no. 22, 415–440

[7] Yamashita T., Sato R., “Correlation of tsunami and sub-oceanic Rayleigh wave amplitudes. Possibility of the use of Rayleigh wave in tsunami warning system”, J. Phys. Earth, 1976, no. 24, 397–416

[8] Ward S. N., “Relationships of tsunami generation and an earthquake source”, J. Phys. Earth, 1980, no. 28, 441–474

[9] Ward S. N., “On tsunami nucleation. 1: A point source”, J. Geophys. Res., 1981, no. 86, 7895–7900 | DOI

[10] Comer R., “Tsunami generation: a comparison of traditional and normal mode approaches”, Geophys. J. R. Astron. Soc., 1984, no. 77, 29–41 | Zbl

[11] González F. I., “Tsunami! Predicting destruction by monster waves”, Sci. American, May 1999, 44–55

[12] Kanamori H., Kikuchi M., “The 1992 Nicaragua earthquake: a slow tsunami earthquake associated with subducted sediments”, Nature, 361 (1993), 714–716 | DOI

[13] Benioff H., “Source wave forms of three earthquakes”, Bull. Seismological Soc. America, 53:5 (1963), 893–903

[14] Ewing W., Jardetzky W., Elastic waves in layered media, McGraw Hill, New York, 1957 | MR | Zbl