syncope 发表于 2025-3-25 07:24:23
http://reply.papertrans.cn/89/8814/881332/881332_21.pngAsymptomatic 发表于 2025-3-25 07:34:09
http://reply.papertrans.cn/89/8814/881332/881332_22.pnganticipate 发表于 2025-3-25 14:40:24
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约会 发表于 2025-3-25 17:54:05
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.Gusiakheadlong 发表于 2025-3-25 21:43:04
http://reply.papertrans.cn/89/8814/881332/881332_25.pngfigurine 发表于 2025-3-26 02:41:36
http://reply.papertrans.cn/89/8814/881332/881332_26.pngFirefly 发表于 2025-3-26 06:03:54
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 numeAVID 发表于 2025-3-26 11:25:12
http://reply.papertrans.cn/89/8814/881332/881332_28.png锯齿状 发表于 2025-3-26 13:44:54
http://reply.papertrans.cn/89/8814/881332/881332_29.png生气的边缘 发表于 2025-3-26 16:54:35
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