... earthquake magnitude and depth i m ax Examples of co-seismic vertical deformation of bottom due to finite rectangular fault h= 30 km MW = 9 d ip = 30° ra ke = 30° hm = 9 .3 References Bolshakova A.V., Nosov M.A. Parameters of tsunami source versus ...
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Ссылки http://ocean.phys.msu.ru/science/nosov/EGU2011_tsunami%20vs%20eq.pdf -- 1087.3 Кб -- 31.03.2011 Похожие документы
... We consider various earthquake magnitudes (Mw = 7 and 8) and various ocean depths ranging from 100 m to 10000 m. We demonstrate that for the Mw=8 earthquake, mass water velocity in elastic oscillations reaches value of 2.5 m/s. Contribution of ...
... description of tsunami generation, an earthquake is considered to instantly cause ... for the tsunamigenic Centr al Kuril Islands earthquakes o f (a) and of January 13 ...
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Ссылки http://ocean.phys.msu.ru/science/nosov/EGU2010_initial_condition.pdf -- 1885.8 Кб -- 12.01.2012 Похожие документы
... Mikhail Nosov Anastasiya Moshenceva Residual hydrodynamic fields in the ocean due to tsunamigenic earthquakes (fragment) EGU General Assembly 2011 Tokachi-oki 2003 Sumatra 2004 ...
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Ссылки http://ocean.phys.msu.ru/science/nosov/EGU2011_Residual%20Fields.pdf -- 521.9 Кб -- 12.01.2012 Похожие документы
... earthquake magnitudefrequency relationship S-wave speed probability of earthquake ... earthquakes; Intraplate: earthquakes which occur within the lithospheric plate ...
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Ссылки http://ocean.phys.msu.ru/courses/geo/lectures-addons/12/2004%20Kanamori%2C%20%20Brodsky%20The%20Physics%20of%20Earthquakes.pdf -- 2258.6 Кб -- 28.01.2005 Похожие документы