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Titlebook: Submarine Landslides and Tsunamis; Ahmet C. Yalçiner,Efim N. Pelinovsky,Costas E. Syn Book 2003 Springer Science+Business Media Dordrecht

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Tsunami of ŞArkoy-Mürefte 1912 Earthquake: Western Marmara, Turkeyt zone (Ms=7.4). The eastern termination of the associated faulting is in the Marmara Sea. On the basis of archiving and library studies, geological field surveys, and offshore investigations, the 1912 earthquake produced a tsunami. The mechanism of this co-seismic tsunami may be assigned to an unde
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Spatial, and Temporal Periodicity in the Pacific Tsunami Occurrencetitude of the area, and it varies with time. The time-dependent variations of seismicity suggest a 6-year-period of activity. Such time interval is well known as a period of Chandler pole motion. To analyze the Pacific tsunami distribution, we use the Historical Tsunami Database compiled by V.Gusiak
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Numerical Modeling of Tsunami Generation by Submarine and Subaerial Landslidescantly increased scientific interest in landslides, and slide-generated tsunamis. Theoretical investigations and laboratory modeling further indicate that purely submarine landslides are ineffective at tsunami generation compared with subaerial slides. In the present study, we undertook several nume
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Analytical Models of Tsunami Generation by Submarine Landslidesl describes the properties of the generated tsunami waves usually well for all regimes expect the resonance case. The nonlinear-dispersive model based on the forced Korteweg-de Vries equation is developed to describe the resonant mechanism of the tsunami wave generation by the landslide moving with
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