標(biāo)題: Titlebook: Computational Earthquake Science Part II; Andrea Donnellan,Peter Mora,Xiang-chu Yin Book 2004 Springer Basel AG 2004 aftershock.assimilati [打印本頁] 作者: antihistamine 時(shí)間: 2025-3-21 19:18
書目名稱Computational Earthquake Science Part II影響因子(影響力)
書目名稱Computational Earthquake Science Part II影響因子(影響力)學(xué)科排名
書目名稱Computational Earthquake Science Part II網(wǎng)絡(luò)公開度
書目名稱Computational Earthquake Science Part II網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Computational Earthquake Science Part II被引頻次
書目名稱Computational Earthquake Science Part II被引頻次學(xué)科排名
書目名稱Computational Earthquake Science Part II年度引用
書目名稱Computational Earthquake Science Part II年度引用學(xué)科排名
書目名稱Computational Earthquake Science Part II讀者反饋
書目名稱Computational Earthquake Science Part II讀者反饋學(xué)科排名
作者: preservative 時(shí)間: 2025-3-21 21:42 作者: gerrymander 時(shí)間: 2025-3-22 03:05
Das Ordnungswidrigkeitenverfahren,s include the computation of synthetic seismograms for several simple rupture scenarios with planar and curved fault approximations of the 1994 Northridge earthquake. We use the boundary integral equation method (BIEM) to compute the dynamic rupture process, which includes the normal stress effects 作者: 泥沼 時(shí)間: 2025-3-22 04:45 作者: 誰在削木頭 時(shí)間: 2025-3-22 08:48
https://doi.org/10.1007/978-3-8349-8081-6the rupture, the material properties of the rocks surrounding the faults, the initial state of stress on the faults, and a constitutive formulation that determines when the faults can slip. In numerical simulations each of these factors appears to play a significant role in rupture propagation, at t作者: Deference 時(shí)間: 2025-3-22 16:39 作者: Deference 時(shí)間: 2025-3-22 19:39 作者: Common-Migraine 時(shí)間: 2025-3-22 23:12
https://doi.org/10.1007/978-3-322-98469-2eature extraction, visualization, statistics, numerical simulation, and communication. We discuss their features and their use in an integrated manner to handle large-scale problems in earthquake physics and other nonlinear problems in the solid earth geosciences.作者: ZEST 時(shí)間: 2025-3-23 03:23
https://doi.org/10.1007/978-3-322-98469-2sion, scale-localization analysis, feature extraction, statistics, numerical simulation, visualization, and communication. Second-generation wavelets represent a recent improvement of the wavelet algorithm, allowing for greater flexibility in the spatial domain and other computational advantages. We作者: ARC 時(shí)間: 2025-3-23 07:23
https://doi.org/10.1007/978-3-663-02052-3roject in Japan, the proposed subsystem is effective for the visualization of large-scale geoscientific data, and can be concurrent with computation subsystems on the same high-performance parallel computer. Moreover, several parallel visualization methods are developed for large unstructured datase作者: Processes 時(shí)間: 2025-3-23 10:41 作者: DECRY 時(shí)間: 2025-3-23 14:07
https://doi.org/10.1007/978-3-663-02052-3 test the Critical Point Hypothesis. Twelve earthquakes in the catalog were chosen based on a criterion for the number of nearby events. Results show that seven sequences with numerous events recorded leading up to the main earthquake exhibited accelerating moment release. Two occurred near in time 作者: 地名表 時(shí)間: 2025-3-23 18:30 作者: 帶子 時(shí)間: 2025-3-24 00:32 作者: 拋射物 時(shí)間: 2025-3-24 05:24 作者: perpetual 時(shí)間: 2025-3-24 10:24 作者: 補(bǔ)角 時(shí)間: 2025-3-24 11:11
Pageoph Topical Volumeshttp://image.papertrans.cn/c/image/232255.jpg作者: 大雨 時(shí)間: 2025-3-24 15:07
Computational Earthquake Science Part II978-3-0348-7875-3Series ISSN 2504-3625 Series E-ISSN 2504-3633 作者: 輕推 時(shí)間: 2025-3-24 20:06
https://doi.org/10.1007/978-3-322-98469-2eature extraction, visualization, statistics, numerical simulation, and communication. We discuss their features and their use in an integrated manner to handle large-scale problems in earthquake physics and other nonlinear problems in the solid earth geosciences.作者: Gleason-score 時(shí)間: 2025-3-24 23:22
https://doi.org/10.1007/978-3-0348-7875-3aftershock; assimilation; earthquake; energy; environment; fault; fault zone; geophysics; modeling; modelling作者: Inferior 時(shí)間: 2025-3-25 04:55 作者: ethnology 時(shí)間: 2025-3-25 10:37
A Wavelet Toolkit for Visualization and Analysis of Large Data Sets in Earthquake Researcheature extraction, visualization, statistics, numerical simulation, and communication. We discuss their features and their use in an integrated manner to handle large-scale problems in earthquake physics and other nonlinear problems in the solid earth geosciences.作者: idiopathic 時(shí)間: 2025-3-25 14:02 作者: figure 時(shí)間: 2025-3-25 18:06 作者: floodgate 時(shí)間: 2025-3-25 20:30 作者: unstable-angina 時(shí)間: 2025-3-26 02:33 作者: 赦免 時(shí)間: 2025-3-26 05:12
https://doi.org/10.1007/978-3-663-02052-3here AMR was observed but no large event followed. The relationship between AMR and Load-Unload Response Ratio (LURR) was studied. Both methods predict similar critical region sizes, however, the critical point time using AMR is slightly earlier than the time of the critical point LURR anomaly.作者: multiply 時(shí)間: 2025-3-26 10:42
Steuertipps für Versicherungsvermittler for infinitesimal deformations by the non-symmetric part of the displacement gradient. As a model for gouge material we propose a continuum description for an assembly of spherical particles of equal radius in which the particle rotation is treated as an independent degree of freedom. Based on this作者: 幼稚 時(shí)間: 2025-3-26 14:54
https://doi.org/10.33283/978-3-86298-865-5terplate coupling. The GPS data also detected a silent earthquake event on the interface of the Philippine Sea slab east of the Boso Peninsula in the middle of May, 1996. The silent rupture propagated over a 50 km * 50 km wide area during about a week. The maximum slip was approximately 50 mm and th作者: amygdala 時(shí)間: 2025-3-26 18:58
2504-3625 orithms, data assimilation and understanding, and applications of models to earthquakes. This part also contains articles on the computational approaches and challenges of constructing earthquake models..978-3-7643-7143-2978-3-0348-7875-3Series ISSN 2504-3625 Series E-ISSN 2504-3633 作者: 運(yùn)動的我 時(shí)間: 2025-3-26 21:57
Computational Earthquake Science Part IIearthquake precursory phenomena and the earthquake cycle. They will have direct application to earthquake hazard studies and earthquake engineering, and the potential to yield spin-offs in sectors such as mining, geophysical exploration, high performance computing, material science, and geotechnical作者: DEFER 時(shí)間: 2025-3-27 05:03
On The Effects Of Non-planar Geometry for Blind Thrust Faults on Strong Ground Motion can change 1-Hz peak velocities by up to a factor of 2-3 near the fault. Our tests suggest that the differences in waveform are larger on the hanging wall compared to those on the footwall, although the differences in amplitude are larger in the forward rupture direction (footwall). The results imp作者: 欲望小妹 時(shí)間: 2025-3-27 08:09
Finite-element Simulation of Seismic Ground Motion with a Voxel Meshs 1.2 ~ 1.4 times longer computation time. The voxel mesh can be generated considerably faster than the popular tetrahedral mesh. Both ground motions and static displacements due to a point or line source can be calculated using the voxel FEM approach. Comparisons with the reflectivity method and th作者: 描述 時(shí)間: 2025-3-27 13:21
A Parallel Implementation of the Lattice Solid Model for the Simulation of Rock Mechanics and Earthqe models with several millions of particles have shown that the parallel implementation of the Lattice Solid Model can achieve a high parallel-efficiency of about 80% for large numbers of processors on different computer architectures.作者: Kidney-Failure 時(shí)間: 2025-3-27 16:17
Spatio-temporal Scanning and Statistical Test of the Accelerating Moment Release (AMR) Model Using Ahere AMR was observed but no large event followed. The relationship between AMR and Load-Unload Response Ratio (LURR) was studied. Both methods predict similar critical region sizes, however, the critical point time using AMR is slightly earlier than the time of the critical point LURR anomaly.作者: PIZZA 時(shí)間: 2025-3-27 20:52 作者: 推延 時(shí)間: 2025-3-28 00:30
Interplate Coupling in the Kanto District, Central Japan, and the Boso Peninsula Silent Earthquake iterplate coupling. The GPS data also detected a silent earthquake event on the interface of the Philippine Sea slab east of the Boso Peninsula in the middle of May, 1996. The silent rupture propagated over a 50 km * 50 km wide area during about a week. The maximum slip was approximately 50 mm and th作者: Frenetic 時(shí)間: 2025-3-28 03:36
https://doi.org/10.1007/978-3-8349-8081-6he kilometer length scale. Observational evidence of the earth indicates that at least the first three of the elements, geometry, material, and stress, can vary over many scale dimensions. Future research on earthquake rupture dynamics needs to consider at which length scales these features are significant in affecting rupture propagation.作者: hallow 時(shí)間: 2025-3-28 06:45
https://doi.org/10.1007/978-3-322-98469-2 effect of the incoherent field via statistical modelling. We will discuss wavelet properties and how they can be utilized and integrated in handling large-scale problems in earthquake physics and other nonlinear phenomena in the geosciences.作者: 天真 時(shí)間: 2025-3-28 14:00 作者: 馬籠頭 時(shí)間: 2025-3-28 17:32 作者: 他去就結(jié)束 時(shí)間: 2025-3-28 20:14 作者: Constrain 時(shí)間: 2025-3-29 01:56
Book 2004 embraces dynamic rupture and wave propagation, computational environment and algorithms, data assimilation and understanding, and applications of models to earthquakes. This part also contains articles on the computational approaches and challenges of constructing earthquake models..作者: 調(diào)色板 時(shí)間: 2025-3-29 05:19 作者: 迫擊炮 時(shí)間: 2025-3-29 08:00 作者: 裝入膠囊 時(shí)間: 2025-3-29 14:54
https://doi.org/10.1007/978-3-662-68569-3tained for each model are similar, showing that the solution of the dynamic problem is non-unique. In other words, it is not always possible to separate strength drop and the slip-weakening distance using rupture modeling, in agreement with the conclusions by GUATTERI and SPUDICH (2000).作者: 疲憊的老馬 時(shí)間: 2025-3-29 17:35
https://doi.org/10.1007/978-3-663-02052-3ssimilation of non-primary data could yield biased simulation results. We present a primary data set for the San Andreas and Imperial faults for comparison with non-primary data in existing databases, and propose standard formats and structure for paleoseismic data assimilation into numerical simulation models.作者: EPT 時(shí)間: 2025-3-29 20:30
Guided Waves from Sources Outside Faults: An Indication for Shallow Fault Zone Structure?ll outside a FZ continuous with depth. The results support, in conjunction with recent observational evidence, a model for natural faults with shallow trapping structures rather than ones that span the entire seismogenic zone. This may have implications for fault mechanics as well as for aspects of shaking hazard near faults.作者: characteristic 時(shí)間: 2025-3-30 02:03 作者: 反話 時(shí)間: 2025-3-30 07:10
Assimilation of Paleoseismic Data for Earthquake Simulationssimilation of non-primary data could yield biased simulation results. We present a primary data set for the San Andreas and Imperial faults for comparison with non-primary data in existing databases, and propose standard formats and structure for paleoseismic data assimilation into numerical simulation models.作者: ANN 時(shí)間: 2025-3-30 10:02 作者: Lipoma 時(shí)間: 2025-3-30 16:00
