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標(biāo)題: Titlebook: Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II; Mitsuhiro Matsu’ura,Peter Mora,Xiang-chu Yin Boo [打印本頁]

作者: Truman    時(shí)間: 2025-3-21 18:08
書目名稱Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II影響因子(影響力)




書目名稱Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II影響因子(影響力)學(xué)科排名




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書目名稱Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II被引頻次




書目名稱Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II被引頻次學(xué)科排名




書目名稱Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II年度引用




書目名稱Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II年度引用學(xué)科排名




書目名稱Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II讀者反饋




書目名稱Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II讀者反饋學(xué)科排名





作者: Abrade    時(shí)間: 2025-3-21 23:50

作者: acolyte    時(shí)間: 2025-3-22 01:26
Phenomena in the Neighbourhood of Hope,numerically simulated the earthquake generation cycles repeated in a seismogenic region on a plate interface, and examined space-time changes in shear stress, slip deficits and fault constitutive properties during one complete cycle in detail. The occurrence of unstable dynamic slip brings about dec
作者: 領(lǐng)先    時(shí)間: 2025-3-22 06:05
A Philosophical Critique of Thought, the amount of fault slip at the first earthquake cycle is smaller than the total relative plate motion. This small amount of fault slip in the viscoelastic medium was considered to be one factor explaining the small seismic coupling observed at several subduction zones. Our simulation, however, sh
作者: 喃喃訴苦    時(shí)間: 2025-3-22 09:18
The Cognitive Component of Amusement, argument has been employed. A wavelet solution, with a length-scale corresponding to 256 degrees, would need a filter with over 400 spherical harmonics centering around . 157 for an optimal spatial fit. The computational effort with the bandpass filter technique greatly exceeds those associated wit
作者: 火車車輪    時(shí)間: 2025-3-22 15:00
https://doi.org/10.1007/978-3-319-30779-4ponse to a series of harmonic perturbations of the director orientation. The Fourier spectra of the initial folding velocity are compared for different viscosity ratios..Turning to the nonlinear regime we analyze viscoelastic folding histories up to 40% shortening. The effect of layering manifests i
作者: 火車車輪    時(shí)間: 2025-3-22 19:20
https://doi.org/10.1007/978-3-319-71571-1lt networks through observations alone is complicated by our inability to study the problem in a manner familiar to laboratory scientists, by means of controlled, fully reproducible experiments. We have therefore been motivated to construct a numerical simulation technology that will allow us to stu
作者: thwart    時(shí)間: 2025-3-22 21:40

作者: ACME    時(shí)間: 2025-3-23 04:27

作者: Yourself    時(shí)間: 2025-3-23 09:19

作者: Working-Memory    時(shí)間: 2025-3-23 12:52
Norio Kambayashi,Kyohei Hirano,Izumi Mitsui global evolution of strain energy correlations within the system. The second stable mode produces Gutenberg-Richter statistics, with near-linear energy release and no significant global correlation evolution. A model with effectively short-range interactions preferentially displays Gutenberg-Richte
作者: Expostulate    時(shí)間: 2025-3-23 14:40

作者: 的闡明    時(shí)間: 2025-3-23 19:45

作者: intertwine    時(shí)間: 2025-3-24 01:56

作者: commensurate    時(shí)間: 2025-3-24 03:19
Introductionns into such models. Simulation of the complete earthquake generation process is an ambitious challenge. Recent advances in high performance computer technology and numerical simulation methodology are bringing this vision within reach.
作者: adumbrate    時(shí)間: 2025-3-24 08:45

作者: Ascendancy    時(shí)間: 2025-3-24 14:07

作者: 謊言    時(shí)間: 2025-3-24 16:08

作者: CRATE    時(shí)間: 2025-3-24 21:02
Large Amplitude Folding in Finely Layered Viscoelastic Rock Structuresponse to a series of harmonic perturbations of the director orientation. The Fourier spectra of the initial folding velocity are compared for different viscosity ratios..Turning to the nonlinear regime we analyze viscoelastic folding histories up to 40% shortening. The effect of layering manifests i
作者: 玩笑    時(shí)間: 2025-3-25 02:02

作者: angiography    時(shí)間: 2025-3-25 07:16

作者: Anticlimax    時(shí)間: 2025-3-25 07:51
Stress Correlation Function Evolution in Lattice Solid Elasto-dynamic Models of Shear and Fracture Zccurs in the lead-up to the largest event and is accompanied by an increasing rate of moderate-sized events and power-law acceleration of Benioff strain release. In the case of an intact sample system subjected to compression, the evolution occurs only after a mature fracture system has developed. T
作者: 不容置疑    時(shí)間: 2025-3-25 14:07
Pattern Dynamics and Forecast Methods in Seismically Active Regionsto events in seismically active areas that show coherent regions associated with the future occurrence of major earthquakes in the same areas. These results strongly support the hypothesis that seismic activity is highly correlated across many space and time scales within large volumes of the earth’
作者: 可卡    時(shí)間: 2025-3-25 15:50

作者: 詳細(xì)目錄    時(shí)間: 2025-3-25 21:13

作者: 裙帶關(guān)系    時(shí)間: 2025-3-26 02:02

作者: engagement    時(shí)間: 2025-3-26 08:19
Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II
作者: CHURL    時(shí)間: 2025-3-26 09:34
https://doi.org/10.1057/9781137426024investigated. The sequence of deformation mechanisms during movement over a ramp is discussed. It is also found that this kind of frictional model is suitable to represent the rate-dependent behavior of fault slipping due to the movement over a ramp and the tractions on fault interface for treating the low frictional problem of fault-bend folds.
作者: 內(nèi)行    時(shí)間: 2025-3-26 14:39

作者: BAN    時(shí)間: 2025-3-26 18:08

作者: 帳單    時(shí)間: 2025-3-26 22:54
Combined GPS and InSAR Models of Postseismic Deformation from the Northridge Earthquakeng the postseismic processes. Fault afterslip and shallow deformation dominate the deformation field in the two years following the earthquake. Lower crustal deformation may play an important role later in the earthquake cycle.
作者: 動(dòng)物    時(shí)間: 2025-3-27 02:15

作者: Aerophagia    時(shí)間: 2025-3-27 08:19

作者: 警告    時(shí)間: 2025-3-27 09:31
2504-3625 laboratory-based fault constitutive laws as a basic equation governing earthquake rupture, quantitative description of tectonic loading driven by plate motion, and a microscopic approach to study fault zone processes. The fault constitutive law plays the role of an interface between microscopic proc
作者: 難取悅    時(shí)間: 2025-3-27 17:31
Mantle Convection Modeling with Viscoelastic/Brittle Lithosphere: Numerical Methodology and Plate Termation viscoelasticity with a strain-dependent yield stress. This is applied to a plate-deformation problem. Numerical accuracy is demonstrated relative to analytic benchmarks, and the characteristics of the method are discussed.
作者: 盲信者    時(shí)間: 2025-3-27 19:50

作者: A精確的    時(shí)間: 2025-3-28 00:20
https://doi.org/10.1007/978-3-031-11004-7technique to scientific analysis of seismicity and GPS data from the southern California region. Preliminary results indicate that the technique can isolate distinct classes of earthquakes from seismicity data.
作者: Lipoma    時(shí)間: 2025-3-28 05:38
3-D Viscoelastic FEM Modeling of Crustal Deformation in Northeast Japaneity, reasonably explains the observed movement. Finally, we stress that the viscoelastic effect should be taken into consideration in the analyses, even if no earthquakes occur in the analyzed period.
作者: 使腐爛    時(shí)間: 2025-3-28 09:26
A Hidden Markov Model Based Tool for Geophysical Data Explorationtechnique to scientific analysis of seismicity and GPS data from the southern California region. Preliminary results indicate that the technique can isolate distinct classes of earthquakes from seismicity data.
作者: Licentious    時(shí)間: 2025-3-28 12:06
Pageoph Topical Volumeshttp://image.papertrans.cn/e/image/300911.jpg
作者: jarring    時(shí)間: 2025-3-28 18:08

作者: Fretful    時(shí)間: 2025-3-28 19:03

作者: Euthyroid    時(shí)間: 2025-3-29 02:12
Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part II978-3-0348-8197-5Series ISSN 2504-3625 Series E-ISSN 2504-3633
作者: 統(tǒng)治人類    時(shí)間: 2025-3-29 07:03
The Alien World: Attention and the Habitual,-based fault constitutive laws as a basic equation governing earthquake rupture, quantitative description of tectonic loading driven by plate motion, and a microscopic approach to study fault zone processes. The fault constitutive law plays the role of an interface between microscopic processes in f
作者: Cubicle    時(shí)間: 2025-3-29 08:37

作者: champaign    時(shí)間: 2025-3-29 13:03
A Philosophical Critique of Thoughtcity of the earth on great interplate earthquake fault slip. We construct a 2-D viscoelastic FEM model of northeast Japan, which consists of an elastic upper crust and a viscoelastic mantle wedge under gravitation overlying the subducting elastic Pacific plate. Instead of the dislocation model presc
作者: Genetics    時(shí)間: 2025-3-29 18:10
https://doi.org/10.1057/9781137426024e-and state-dependent frictional law is introduced to represent the faulting processes and frictional behaviors of fault interface. Moreover, viscous and plastic material properties are used to simulate pressure solution creep and cataclasis, respectively. Throughout the simulations on a structural
作者: 可忽略    時(shí)間: 2025-3-29 22:05

作者: 上腭    時(shí)間: 2025-3-30 02:24

作者: SEEK    時(shí)間: 2025-3-30 05:27

作者: 軍械庫    時(shí)間: 2025-3-30 11:25
The Cognitive Component of Amusement,the field into various distinct lengthscales, we have also constructed the 2-D maps describing the spatial distributions of the maximum of the wavelet-transformed L.-norm E. (x,y) and its corresponding local wavenumber ...,.,where x and y are the Cartesian coordinates. For geoid anomalies, using a w
作者: 腐蝕    時(shí)間: 2025-3-30 13:30
https://doi.org/10.1007/978-3-319-30779-4han characteristic structural dimensions. For this purpose we derive constitutive relations and apply a computational simulation scheme (a finite-element based particle advection scheme; see MORESI ., 2001) suitable for problems involving very large deformations of layered viscous and viscoelastic r
作者: 一窩小鳥    時(shí)間: 2025-3-30 20:31

作者: installment    時(shí)間: 2025-3-30 21:54
https://doi.org/10.1007/978-3-319-71571-1ake-prone areas such as California and Japan. The installation of the Southern California Integrated Geodetic Network (SCIGN) and the Bay Area Regional Deformation (BARD) network are two examples. As part of the recently proposed Earthscope NSF/GEO/EAR/MRE initiative, the Plate Boundary Observatory
作者: 徹底檢查    時(shí)間: 2025-3-31 03:22
A Pictorial Approach to Molecular Bondinge Benioff strain following a power law timeto-failure relation with a term (t. - t)., where . is the failure time of the large event and observed values of . are close to 0.3. We discuss properties of ASR and related aspects of seismicity patterns associated with several theoretical frameworks. The
作者: FLACK    時(shí)間: 2025-3-31 05:47

作者: Perineum    時(shí)間: 2025-3-31 12:51
A Picture is Worth a Thousand Tablesory activity and quiescence, and aftershock sequences. Although the characteristics of these patterns can be qualitatively described, a systematic quantitative analysis remains elusive. Our research suggests that a new pattern dynamics methodology can be used to define a unique, finite set of seismi
作者: CRUE    時(shí)間: 2025-3-31 15:16

作者: 描述    時(shí)間: 2025-3-31 18:58

作者: 古老    時(shí)間: 2025-3-31 23:08

作者: Intellectual    時(shí)間: 2025-4-1 04:16

作者: esculent    時(shí)間: 2025-4-1 07:35
3-D Simulation of Earthquake Generation Cycles and Evolution of Fault Constitutitve Propertiesress redistribution and fault restrengthening. From a macroscopic point of view, the entire process of earthquake generation cycles should be consistently described by a coupled nonlinear system of a slip-response function, a fault constitutive law and a driving force. On the basis of such a general
作者: mortgage    時(shí)間: 2025-4-1 11:24





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