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The experimental data in the microseismic frequency range obtained using the seismo-acoustic-hydrophysical measurement complex are analyzed. The emphasis is put on estimating the ratio between the energy of surface sea wind waves in the area of the Japan Sea where the complex was located and the Earth’s crust microdeformations in this frequency range. The experimental evaluate obtained allow us to estimate the energy re-distribution at the hydrosphere-lithosphere boundary.
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Tom
Strony
607--618
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autor
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- V.I. Ilyichev’s Pacific Oceanological Institute, Far-Eastern Branch of Russian Academy of Sciences, Vladivostok, Russia, dolgikh@poi.dvo.ru
Bibliografia
- Bowden, K.F., 1983, Physical Oceanography of Coastal Waters, Ellis Horwood Ltd, New York, 324 pp.
- Dolgikh, G.I., 2003, Laser-interference complex, Seismic Instruments 39, 13-27.
- Gorbachev, K.P., E.G. Krasnov, V.V. Subbotnitsky and N.P. Vasilchenko, 1998, Principles of the mechanics of the deformed solid. Part 1. Publishing House "Ussuri", Vladivostok, 152 pp.
- Monakhov, F.I., 1977, Low-frequency Seismic Noise of the Earth, Nauka, Moscow, 96 pp.
- Webb, S.C., 1992, The equilibrium ocean microseism spectrum, J. Acoust. Soc. Am. 92, 4, 2141-2158.
- Webb, S.C., and C.S. Cox, 1986. Observation and modeling of seafloor microseisms, J. Geophys. Res. 91 (B7), 7343-7358.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0021-0062