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Littérature scientifique sur le sujet « Earthquake source and dynamics »

Auteur : Grafiati

Publié le 10 mars 2023

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Articles de revues sur le sujet "Earthquake source and dynamics"

VEITCH, STEPHEN A., et MEREDITH NETTLES. « Assessment of glacial-earthquake source parameters ». Journal of Glaciology 63, n^o 241 (octobre 2017) : 867–76. http://dx.doi.org/10.1017/jog.2017.52.

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ABSTRACTGlacial earthquakes are slow earthquakes of magnitude M~5 associated with major calving events at near-grounded marine-terminating glaciers. These globally detectable earthquakes provide information on the grounding state of outlet glaciers and the timing of large calving events. Seismic source modeling of glacial earthquakes provides information on the size and orientation of forces associated with calving events. We compare force orientations estimated using a centroid-single-force technique with the calving-front orientations of the source glaciers at or near the time of earthquake occurrence. We consider earthquakes recorded at four glaciers in Greenland – Kangerdlugssuaq Glacier, Helheim Glacier, Kong Oscar Glacier, and Jakobshavn Isbræ – between 1999 and 2010. We find that the estimated earthquake force orientations accurately represent the orientation of the calving front at the time of the earthquake, and that seismogenic calving events are produced by a preferred section of the calving front, which may change with time. We also find that estimated earthquake locations vary in a manner consistent with changes in calving-front position, though with large scatter. We conclude that changes in glacial-earthquake source parameters reflect true changes in the geometry of the source glaciers, providing a means for identifying changes in glacier geometry and dynamics that complements traditional remote-sensing techniques.

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Yin, Jiuxun, Zefeng Li et Marine A. Denolle. « Source Time Function Clustering Reveals Patterns in Earthquake Dynamics ». Seismological Research Letters 92, n^o 4 (31 mars 2021) : 2343–53. http://dx.doi.org/10.1785/0220200403.

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Abstract We cluster a global database of 3529 Mw>5.5 earthquakes in 1995–2018 based on a dynamic time warping distance between earthquake source time functions (STFs). The clustering exhibits different degrees of complexity of the STF shapes and suggests an association between STF complexity and earthquake source parameters. Most of the thrust events have simple STF shapes across all depths. In contrast, earthquakes with complex STF shapes tend to be located at shallow depths in complicated tectonic regions, exhibit long source duration compared with others of similar magnitude, and tend to have strike-slip mechanisms. With 2D dynamic modeling of dynamic ruptures on heterogeneous fault properties, we find a systematic variation of the simulated STF complexity with frictional properties. Comparison between the observed and synthetic clustering distributions provides useful constraints on frictional properties. In particular, the characteristic slip-weakening distance could be constrained to be short (<0.1 m) and depth dependent if stress drop is in general constant.

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Badea, Lori, Ioan R. Ionescu et Sylvie Wolf. « Schwarz method for earthquake source dynamics ». Journal of Computational Physics 227, n^o 8 (avril 2008) : 3824–48. http://dx.doi.org/10.1016/j.jcp.2007.11.044.

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Madden, E. H., M. Bader, J. Behrens, Y. van Dinther, A.-A. Gabriel, L. Rannabauer, T. Ulrich, C. Uphoff, S. Vater et I. van Zelst. « Linked 3-D modelling of megathrust earthquake-tsunami events : from subduction to tsunami run up ». Geophysical Journal International 224, n^o 1 (10 octobre 2020) : 487–516. http://dx.doi.org/10.1093/gji/ggaa484.

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SUMMARY How does megathrust earthquake rupture govern tsunami behaviour? Recent modelling advances permit evaluation of the influence of 3-D earthquake dynamics on tsunami genesis, propagation, and coastal inundation. Here, we present and explore a virtual laboratory in which the tsunami source arises from 3-D coseismic seafloor displacements generated by a dynamic earthquake rupture model. This is achieved by linking open-source earthquake and tsunami computational models that follow discontinuous Galerkin schemes and are facilitated by highly optimized parallel algorithms and software. We present three scenarios demonstrating the flexibility and capabilities of linked modelling. In the first two scenarios, we use a dynamic earthquake source including time-dependent spontaneous failure along a 3-D planar fault surrounded by homogeneous rock and depth-dependent, near-lithostatic stresses. We investigate how slip to the trench influences tsunami behaviour by simulating one blind and one surface-breaching rupture. The blind rupture scenario exhibits distinct earthquake characteristics (lower slip, shorter rupture duration, lower stress drop, lower rupture speed), but the tsunami is similar to that from the surface-breaching rupture in run-up and length of impacted coastline. The higher tsunami-generating efficiency of the blind rupture may explain how there are differences in earthquake characteristics between the scenarios, but similarities in tsunami inundation patterns. However, the lower seafloor displacements in the blind rupture result in a smaller displaced volume of water leading to a narrower inundation corridor inland from the coast and a 15 per cent smaller inundation area overall. In the third scenario, the 3-D earthquake model is initialized using a seismo-thermo-mechanical geodynamic model simulating both subduction dynamics and seismic cycles. This ensures that the curved fault geometry, heterogeneous stresses and strength and material structure are consistent with each other and with millions of years of modelled deformation in the subduction channel. These conditions lead to a realistic rupture in terms of velocity and stress drop that is blind, but efficiently generates a tsunami. In all scenarios, comparison with the tsunamis sourced by the time-dependent seafloor displacements, using only the time-independent displacements alters tsunami temporal behaviour, resulting in later tsunami arrival at the coast, but faster coastal inundation. In the scenarios with the surface-breaching and subduction-initialized earthquakes, using the time-independent displacements also overpredicts run-up. In the future, the here presented scenarios may be useful for comparison of alternative dynamic earthquake-tsunami modelling approaches or linking choices, and can be readily developed into more complex applications to study how earthquake source dynamics influence tsunami genesis, propagation and inundation.

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Abercrombie, Rachel E. « Resolution and uncertainties in estimates of earthquake stress drop and energy release ». Philosophical Transactions of the Royal Society A : Mathematical, Physical and Engineering Sciences 379, n^o 2196 (15 mars 2021) : 20200131. http://dx.doi.org/10.1098/rsta.2020.0131.

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Our models and understanding of the dynamics of earthquake rupture are based largely on estimates of earthquake source parameters, such as stress drop and radiated seismic energy. Unfortunately, the measurements, especially those of small and moderate-sized earthquakes (magnitude less than about 5 or 6), are not well resolved, containing significant random and potentially systematic uncertainties. The aim of this review is to provide a context in which to understand the challenges involved in estimating these measurements, and to assess the quality and reliability of reported measurements of earthquake source parameters. I also discuss some of the ways progress is being made towards more reliable parameter measurements. At present, whether the earthquake source is entirely self-similar, or not, and which factors and processes control the physics of the rupture remains, at least in the author's opinion, largely unconstrained. Detailed analysis of the best recorded earthquakes, using the increasing quantity and quality of data available, and methods less dependent on simplistic source models is one approach that may help provide better constraints. This article is part of the theme issue ‘Fracture dynamics of solid materials: from particles to the globe’.

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Nakanishi, Hiizu. « Complex Behavior in Earthquake Dynamics ». International Journal of Modern Physics B 12, n^o 03 (30 janvier 1998) : 273–84. http://dx.doi.org/10.1142/s0217979298000211.

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Recent progresses in understanding earthquake dynamics with the aid of a simple spring-block system is reviewed from a physicists' point of view. Dynamical instability due to negative dynamical friction amplifies any perturbation and leads to a chaotic behavior for almost any initial configurations. It is also pointed out that static friction gives another source of the complex behavior which is characteristic to a threshold element system.

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Tinti, E. « A Kinematic Source-Time Function Compatible with Earthquake Dynamics ». Bulletin of the Seismological Society of America 95, n^o 4 (1 août 2005) : 1211–23. http://dx.doi.org/10.1785/0120040177.

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Cao, Zelin, Xiaxin Tao, Zhengru Tao et Aiping Tang. « Kinematic Source Modeling for the Synthesis of Broadband Ground Motion Using the f‐k Approach ». Bulletin of the Seismological Society of America 109, n^o 5 (23 juillet 2019) : 1738–57. http://dx.doi.org/10.1785/0120180294.

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Abstract A procedure for building a kinematic source model is proposed in this article for the synthesis of broadband ground motion based on the frequency–wavenumber Green’s function. The spatial distribution of slip on the rupture plane is generated by combining asperity slip with random slip. A set of scaling laws recently updated for the global and local parameters of seismic sources is adopted. To characterize the temporal evolution of slip on the rupture plane, different rupture velocities, and rise times are first generated by considering the correlation with slip, and a source time function obtained by rupture dynamics is selected for each subsource. Then, the entire rupture process is set as the object to jointly determine the rise time and rupture velocity for a given slip distribution under the selection criterion that the entire rupture process should radiate the closest seismic energy to the expected energy. To reduce uncertainty, 30 spatiotemporal rupture processes for an earthquake scenario are realized to select a mean source model. To demonstrate the feasibility of the proposed source modeling approach, two California earthquakes, the Whittier Narrows earthquake and the Loma Prieta earthquake, are chosen as case studies. The performance of the obtained source models shows that our modeling approach is advantageous for estimating the size of the rupture plane, emphasizing the effect of asperity, and considering the correlation between temporal rupture parameters and slip. The bias values between the observed and synthetic pseudospectral accelerations are relatively small compared to those for the methods on the Southern California Earthquake Center broadband platform. The synthetics are further compared with the estimates from regional ground‐motion prediction equations for four scenario earthquakes with moment magnitudes of 6.0, 6.5, 7.0, and 7.5. Finally, the sensitivity of the synthetic motion to various rupture parameters is analyzed.

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Uchida, Naoki, et Roland Bürgmann. « Repeating Earthquakes ». Annual Review of Earth and Planetary Sciences 47, n^o 1 (30 mai 2019) : 305–32. http://dx.doi.org/10.1146/annurev-earth-053018-060119.

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Repeating earthquakes, or repeaters, are identical in location and geometry but occur at different times. They appear to represent recurring seismic energy release from distinct structures such as slip on a fault patch. Repeaters are most commonly found on creeping plate boundary faults, where seismic patches are loaded by surrounding slow slip, and they can be used to track fault creep at depth. Their hosting environments also include volcanoes, subducted slabs, mining-induced fault structures, glaciers, and landslides. While true repeaters should have identical seismic waveforms, small differences in their seismograms can be used to examine subtle changes in source properties or in material properties of the rocks through which the waves propagate. Source studies have documented the presence of smaller slip patches within the rupture areas of larger repeaters, illuminated earthquake triggering mechanisms, and revealed systematic changes in rupture characteristics as a function of loading rate. ▪ Repeating earthquakes are observed in diverse tectonic and nontectonic settings. ▪ Their occurrence patterns provide quantitative information about fault creep, earthquake cycle dynamics, triggering, and predictability. ▪ Their seismic waveform characteristics provide important insights on earthquake source variability and temporal Earth structure changes.

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Sobolev, G. A. « Seismicity dynamics and earthquake predictability ». Natural Hazards and Earth System Sciences 11, n^o 2 (14 février 2011) : 445–58. http://dx.doi.org/10.5194/nhess-11-445-2011.

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Abstract. Many factors complicate earthquake sequences, including the heterogeneity and self-similarity of the geological medium, the hierarchical structure of faults and stresses, and small-scale variations in the stresses from different sources. A seismic process is a type of nonlinear dissipative system demonstrating opposing trends towards order and chaos. Transitions from equilibrium to unstable equilibrium and local dynamic instability appear when there is an inflow of energy; reverse transitions appear when energy is dissipating. Several metastable areas of a different scale exist in the seismically active region before an earthquake. Some earthquakes are preceded by precursory phenomena of a different scale in space and time. These include long-term activation, seismic quiescence, foreshocks in the broad and narrow sense, hidden periodical vibrations, effects of the synchronization of seismic activity, and others. Such phenomena indicate that the dynamic system of lithosphere is moving to a new state – catastrophe. A number of examples of medium-term and short-term precursors is shown in this paper. However, no precursors identified to date are clear and unambiguous: the percentage of missed targets and false alarms is high. The weak fluctuations from outer and internal sources play a great role on the eve of an earthquake and the occurrence time of the future event depends on the collective behavior of triggers. The main task is to improve the methods of metastable zone detection and probabilistic forecasting.

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Thèses sur le sujet "Earthquake source and dynamics"

Twardzik, Cedric. « Study of the earthquake source process and seismic hazards ». Thesis, University of Oxford, 2014. http://ora.ox.ac.uk/objects/uuid:c2553a3f-f6ce-46a0-9c47-d68f5957cdac.

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To obtain the rupture history of the Parkfield, California, earthquake, we perform 12 kinematic inversions using elliptical sub-faults. The preferred model has a seismic moment of 1.21 x 10^18 Nm, distributed on two distinct ellipses. The average rupture speed is ~2.7 km/s. The good spatial agreement with previous large earthquakes and aftershocks in the region, suggests the presence of permanent asperities that break during large earthquakes. We investigate our inversion method with several tests. We demonstrate its capability to retrieve the rupture process. We show that the convergence of the inversion is controlled by the space-time location of the rupture front. Additional inversions show that our procedure is not highly influenced by high-frequency signal, while we observe high sensitivity to the waveforms duration. After considering kinematic inversion, we present a full dynamic inversion for the Parkfield earthquake using elliptical sub-faults. The best fitting model has a seismic moment of 1.18 x 10^18 Nm, distributed on one ellipse. The rupture speed is ~2.8 km/s. Inside the parameter-space, the models are distributed according the rupture speed and final seismic moment, defining a optimal region where models fit correctly the data. Furthermore, to make the preferred kinematic model both dynamically correct while fitting the data, we show it is necessary to connect the two ellipses. This is done by adopting a new approach that uses b-spline curves. Finally, we relocate earthquakes in the vicinity of the Darfield, New-Zealand earthquake. 40 years prior to the earthquake, where there is the possibility of earthquake migration towards its epicentral region. Once it triggers the 2010-2011 earthquake sequence, we observe earthquakes migrating inside regions of stress increase. We also observe a stress increase on a large seismic gap of the Alpine Fault, as well as on some portions of the Canterbury Plains that remain today seismically quiet.

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Horikawa, Haruo. « Inversion for dynamic source parameters : Application to the 1990 Izu-Oshima, Japan, earthquake ». 京都大学 (Kyoto University), 1997. http://hdl.handle.net/2433/202443.

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Zhang, Wenbo. « Study on Dynamic Rupture Process and Near-Source Strong Motion Simulation - Case of the 1999 Chi-Chi, Taiwan, Earthquake ». 京都大学 (Kyoto University), 2003. http://hdl.handle.net/2433/149083.

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Kyoto University (京都大学)
0048
新制・課程博士
博士(理学)
甲第9962号
理博第2623号
新制||理||1337(附属図書館)
UT51-2003-H383
京都大学大学院理学研究科地球惑星科学専攻
(主査)教授入倉孝次郎, 教授 Mori James J., 教授岡田篤正
学位規則第4条第1項該当

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Chen, Shengzao. « Global comparisons of earthquake source spectra ». Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/NQ58253.pdf.

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Chen, Shengzao Carleton University Dissertation Earth Sciences. « Global comparisons of earthquake source spectra ». Ottawa, 2000.

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Shomali, Z. Hossein. « Dynamic Source Models of Icelandic Earthquakes and Teleseismic Tomograhy along the TOR array ». Doctoral thesis, Uppsala University, Department of Earth Sciences, 2001. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-1451.

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This thesis describes new inversion-oriented methodological developments and their seismological applications. In the first study presented the dynamic source parameters of some local Icelandic earthquakes are studied by employing a time domain moment tensor inversion method. A windowing method for direct P and S phases was used and the inversion was performed for frequencies lower than the associated corner frequency under the double-couple constraint. The inversion algorithm could determine the dynamic source parameters correctly, even under conditions of poor azimuthal coverage. The second study deals with a new method for calculating the empirical Green's function based on inversion of earthquake radiation patterns. The resulting Green's functions then may contain both body and surface waves. The validity of the method was then confirmed by applying the method to some Icelandic earthquakes. The lithosphere-asthenosphere transition along the TOR array is investigated in the last two studies. Separate and simultaneous teleseismic P and S relative arrival-time residuals were inverted via different methods (a singular value decomposition and a quadratic programming method) to investigate the reliability and the resolution of the model. The data were corrected a priori for the effect of travel-time perturbations due to crustal structure. The results indicate that the transition between thinner lithosphere in Germany to the thicker Baltic Shield in Sweden occurs in two sharp and steep steps. A sharp and steep subcrustal boundary is found below the Tornquist Zone, with a less significant transition below the Elbe Lineament. The lithospheric structure appears to be about 120 km thick under the Tornquist Zone, increasing to more than 200 km beneath the Baltic Shield.

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Shomali, Z. Hossein. « Dynamic source models of Icelandic earthquakes and teleseismic tomography along the TOR array / ». Uppsala : Acta Universitatis Upsaliensis : Univ.-bibl. [distributör], 2001. http://publications.uu.se/theses/91-554-5098-9/.

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Xia, Kaiwen Rosakis Ares J. « Laboratory investigations of earthquake dynamics / ». Diss., Pasadena, Calif. : California Institute of Technology, 2005. http://resolver.caltech.edu/CaltechETD:etd-02262005-161824.

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Hjörleifsdóttir, Vala Simons Mark Tromp Jeroen. « Earthquake source characterization using 3D numerical modeling / ». Diss., Pasadena, Calif. : California Institute of Technology, 2007. http://resolver.caltech.edu/CaltechETD:etd-03212007-170259.

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Donner, Stefanie, Manfred Strecker, Dirk Rößler, Abdolreza Ghods, Frank Krüger, Angela Landgraf et Paolo Ballato. « Earthquake source models for earthquakes in Northern Iran ». Universität Potsdam, 2009. http://opus.kobv.de/ubp/volltexte/2009/3258/.

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The complex system of strike-slip and thrust faults in the Alborz Mountains, Northern Iran, are not well understood yet. Mainly structural and geomorphic data are available so far. As a more extensive base for seismotectonic studies and seismic hazard analysis we plan to do a comprehensive seismic moment tensor study also from smaller magnitudes (M < 4.5) by developing a new algorithm. Here, we present first preliminary results.

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Livres sur le sujet "Earthquake source and dynamics"

Das, Shamita, John Boatwright et Christopher H. Scholz, dir. Earthquake Source Mechanics. Washington, D. C. : American Geophysical Union, 1986. http://dx.doi.org/10.1029/gm037.

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Shamita, Das, Boatwright John et Scholz C. H, dir. Earthquake source mechanics. Washington, D.C : American Geophysical Union, 1986.

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Takeshi, Mikumo, dir. Earthquake source physics and earthquake precursors. Amsterdam : Elsevier, 1992.

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Shamita, Das, et Kostrov B. V, dir. Principles of earthquake source mechanics. Cambridge, England : Cambridge University Press, 1988.

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Adimoolam, Boominathan, et Subhadeep Banerjee, dir. Soil Dynamics and Earthquake Geotechnical Engineering. Singapore : Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-0562-7.

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Manolis, Papadrakakis, dir. Computational structural dynamics and earthquake engineering. Boca Raton : CRC Press, 2009.

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International Conference on Soil Dynamics and Earthquake Engineering (7th 1995 Crete, Greece). Soil dynamics and earthquake engineering VII. Sous la direction de Cakmak A. S et Brebbia C. A. Southampton : Computational Mechanics Publications, 1995.

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S, Cakmak A., Brebbia C. A et International Conference on Soil Dynamics and Earthquake Engineering (6th : 1993 : Bath, England), dir. Soil dynamics and earthquake engineering VI. Southampton : Computational Mechanics Publications, 1992.

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Manolis, G. D. Stochastic structural dynamics in earthquake engineering. Southampton : WITPress, 2001.

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Universität Karlsruhe. Institut für Bodenmechanik und Felsmechanik. et Deutsche Forschungsgemeinschaft, dir. Soil dynamics and earthquake engineering V. Southampton, UK : Computational Mechanics Publications, 1991.

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Chapitres de livres sur le sujet "Earthquake source and dynamics"

Spudich, Paul, et David Oppenheimer. « Dense Seismograph Array Observations of Earthquake Rupture Dynamics ». Dans Earthquake Source Mechanics, 285–96. Washington, D. C. : American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm037p0285.

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Okubo, Paul G., et James H. Dieterich. « State Variable Fault Constitutive Relations for Dynamic Slip ». Dans Earthquake Source Mechanics, 25–35. Washington, D. C. : American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm037p0025.

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Zhang, Ruichong, Yan Yong et Y. K. Lin. « Stochastic Earthquake Modeling with Discretized Line Source ». Dans Stochastic Structural Dynamics 1, 285–312. Berlin, Heidelberg : Springer Berlin Heidelberg, 1991. http://dx.doi.org/10.1007/978-3-642-84531-4_15.

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Ohnaka, Mitiyasu, Yasuto Kuwahara, Kiyohiko Yamamoto et Tomowo Hirasawa. « Dynamic Breakdown Processes and the Generating Mechanism for High-Frequency Elastic Radiation During Stick-Slip Instabilities ». Dans Earthquake Source Mechanics, 13–24. Washington, D. C. : American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm037p0013.

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Boatwright, John, et Howard Quin. « The Seismic Radiation from a 3-D Dynamic Model of a Complex Rupture Process. Part I : Confined Ruptures ». Dans Earthquake Source Mechanics, 97–109. Washington, D. C. : American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm037p0097.

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Kilgore, Brian D., Art McGarr, Nicholas M. Beeler et David A. Lockner. « Earthquake Source Properties From Instrumented Laboratory Stick-Slip ». Dans Fault Zone Dynamic Processes, 151–69. Hoboken, NJ, USA : John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781119156895.ch8.

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Sigtryggsdóttir, Fjóla G., et Jónas Th Snæbjörnsson. « Systematic Methodology for Planning and Evaluation of a Multi-source Geohazard Monitoring System. Application of a Reusable Template ». Dans Proceedings of the International Conference on Earthquake Engineering and Structural Dynamics, 385–401. Cham : Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-78187-7_29.

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Tsuda, Kenichi, Satoshi Iwase, Hiroaki Uratani, Sachio Ogawa, Takahide Watanabe, Jun’ichi Miyakoshi et Jean Paul Ampuero. « Dynamic Rupture Simulations Based on the Characterized Source Model of the 2011 Tohoku Earthquake ». Dans Pageoph Topical Volumes, 33–44. Cham : Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-72709-7_4.

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Soloviev, A. A., I. A. Vorobieva et G. F. Panza. « Modelling of Block Structure Dynamics for the Vrancea Region : Source Mechanisms of the Synthetic Earthquakes ». Dans Seismic Hazard of the Circum-Pannonian Region, 97–110. Basel : Birkhäuser Basel, 2000. http://dx.doi.org/10.1007/978-3-0348-8415-0_6.

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Madariaga, Raul. « Earthquake Source Theory ». Dans Encyclopedia of Solid Earth Geophysics, 1–5. Cham : Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-10475-7_62-1.

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Actes de conférences sur le sujet "Earthquake source and dynamics"

Rowshandel, Badie. « Capturing and PSHA Implementation of Spatial Variability of Near-Source Ground Motion Hazard ». Dans Geotechnical Earthquake Engineering and Soil Dynamics V. Reston, VA : American Society of Civil Engineers, 2018. http://dx.doi.org/10.1061/9780784481462.006.

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Baker, Jack W., et Abhineet Gupta. « Incorporating Induced Seismicity Source Models and Ground Motion Predictions to Forecast Dynamic Regional Risk ». Dans Geotechnical Earthquake Engineering and Soil Dynamics V. Reston, VA : American Society of Civil Engineers, 2018. http://dx.doi.org/10.1061/9780784481462.003.

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Greenwood, William W., Hao Zhou, Dimitrios Zekkos et Jerome P. Lynch. « Experiments Using a UAV-Deployed Impulsive Source for Multichannel Analysis of Surface Waves Testing ». Dans Geotechnical Earthquake Engineering and Soil Dynamics V. Reston, VA : American Society of Civil Engineers, 2018. http://dx.doi.org/10.1061/9780784481486.046.

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Baltzopoulos, Georgios, Dimitrios Vamvatsikos et Iunio Iervolino. « NEAR -SOURCE PULSE-LIKE SEISMIC DEMAND FOR MULTI-LINEAR BACKBONE OSCILLATORS ». Dans 5th International Conference on Computational Methods in Structural Dynamics and Earthquake Engineering Methods in Structural Dynamics and Earthquake Engineering. Athens : Institute of Structural Analysis and Antiseismic Research School of Civil Engineering National Technical University of Athens (NTUA) Greece, 2015. http://dx.doi.org/10.7712/120115.3476.704.

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Fioriti, Vincenzo, Ivan Roselli et Gerardo De Canio. « MODAL IDENTIFICATION FROM MOTION MAGNIFICATION OF ANCIENT MONUMENTS SUPPORTED BY BLIND SOURCE SEPARATION ALGORITHMS ». Dans 7th International Conference on Computational Methods in Structural Dynamics and Earthquake Engineering Methods in Structural Dynamics and Earthquake Engineering. Athens : Institute of Structural Analysis and Antiseismic Research School of Civil Engineering National Technical University of Athens (NTUA) Greece, 2019. http://dx.doi.org/10.7712/120119.7192.19033.

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Bouckaert, Igor, Michele Godio et João Pacheco de Almeida. « LARGE-DISPLACEMENT RESPONSE OF UNREINFORCED MASONRY STRUCTURES : COMPARISON BETWEEN ANALYTICAL SOLUTIONS AND DEM MODELS INCLUDING OPEN-SOURCE SOFTWARE ». Dans 8th International Conference on Computational Methods in Structural Dynamics and Earthquake Engineering Methods in Structural Dynamics and Earthquake Engineering. Athens : Institute of Structural Analysis and Antiseismic Research National Technical University of Athens, 2021. http://dx.doi.org/10.7712/120121.8788.19942.

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Carlton, Brian D., Elin Skurtveit, Bahman Bohloli, Kuvvet Atakan, Emily Dondzila et Amir M. Kaynia. « Probabilistic Seismic Hazard Analysis for Offshore Bangladesh Including Fault Sources ». Dans Geotechnical Earthquake Engineering and Soil Dynamics V. Reston, VA : American Society of Civil Engineers, 2018. http://dx.doi.org/10.1061/9780784481462.015.

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Psycharis, I., M. Fragiadakis et I. Stefanou. « SEISMIC RELIABILITY ASSESSMENT OF CLASSICAL COLUMNS SUBJECTED TO NEAR SOURCE GROUND MOTIONS ». Dans 4th International Conference on Computational Methods in Structural Dynamics and Earthquake Engineering. Athens : Institute of Structural Analysis and Antiseismic Research School of Civil Engineering National Technical University of Athens (NTUA) Greece, 2014. http://dx.doi.org/10.7712/120113.4622.c1442.

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Baltzopoulos, G., E. Chioccarelli et I. Iervolino. « ACCOUNTING FOR NEAR-SOURCE EFFECTS IN THE DISPLACEMENT COEFFICIENT METHOD FOR SEISMIC STRUCTURAL ASSESSMENT ». Dans 4th International Conference on Computational Methods in Structural Dynamics and Earthquake Engineering. Athens : Institute of Structural Analysis and Antiseismic Research School of Civil Engineering National Technical University of Athens (NTUA) Greece, 2014. http://dx.doi.org/10.7712/120113.4509.c1017.

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Baltzopoulos, Georgios, Eugenio Chioccarelli et Iunio Iervolino. « Accounting for Near-Source Effects in the Displacement Coefficient Method for Seismic Structural Assessment ». Dans 4th International Conference on Computational Methods in Structural Dynamics and Earthquake Engineering. Athens : ECCOMAS, 2013. http://dx.doi.org/10.7712/compdyn-2013.1017.

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Rapports d'organisations sur le sujet "Earthquake source and dynamics"

Okubo, Kurama, Esteban Rougier et Harsha Bhat Suresh. Source time functions inferred from dynamic earthquake rupture modeling on Jordan – Kekerengu – Papatea fault system, the 2016 Mw 7.8 Kaikoura earthquake. Office of Scientific and Technical Information (OSTI), mars 2019. http://dx.doi.org/10.2172/1499301.

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Pitarka, Arben, Atsundo Mampo et H. Kawase. Collaborative study on "Earthquake Ground Motion Simulation Using Rupture Dynamics". Office of Scientific and Technical Information (OSTI), mars 2018. http://dx.doi.org/10.2172/1438604.

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Pitarka, Arben, Jikai Sun et Hiroshi Kawase. Collaborative study on Earthquake Ground Motion Simulation Using Rupture Dynamics. Office of Scientific and Technical Information (OSTI), mars 2019. http://dx.doi.org/10.2172/1512610.

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Mayeda, K., S. Felker, R. Gok, J. O'Boyle, W. Walter et S. Ruppert. LDRD LW Project Final Report:Resolving the Earthquake Source Scaling Problem. Office of Scientific and Technical Information (OSTI), février 2004. http://dx.doi.org/10.2172/15013992.

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Bent, A. L. Source parameters of the 1963 Mw 6.1 Baffin Island earthquake. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205317.

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Foxall, B. Southern California Earthquake Center - SCEC1 : Final Report Summary Alternative Earthquake Source Characterization for the Los Angeles Region. Office of Scientific and Technical Information (OSTI), février 2003. http://dx.doi.org/10.2172/15004050.

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Baer, T., N. Berrah, C. Fadley, C. B. Moore, D. M. Neumark, C. Y. Ng, B. Ruscic, N. V. Smith, A. G. Suits et A. M. Wodtke. Chemical Dynamics at the Advanced Light Source. Office of Scientific and Technical Information (OSTI), février 1999. http://dx.doi.org/10.2172/6536.

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Yocky, David. Source Physics Experiment : Rock Valley Interferometric Synthetic Aperture RADAR Earthquake Detection Study. Office of Scientific and Technical Information (OSTI), septembre 2021. http://dx.doi.org/10.2172/1821315.

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Pitarka, Arben. Strong Ground Motion Simulations of the M7.1 Kumamoto, Japan Earthquake Using Characterized Heterogeneous Source Models. Office of Scientific and Technical Information (OSTI), mars 2018. http://dx.doi.org/10.2172/1430931.

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Siders, C., J. Crane, V. Semenov, S. Betts, B. Kozioziemski, K. Wharton, S. Wilks et al. High Brightness, Laser-Driven X-ray Source for Nanoscale Metrology and Femtosecond Dynamics. Office of Scientific and Technical Information (OSTI), février 2007. http://dx.doi.org/10.2172/902319.

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