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Journal articles on the topic 'Earthquake dynamics'

Author: Grafiati

Published: 10 March 2023

Last updated: 25 July 2025

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1

Gabriel, Alice-Agnes, Thomas Ulrich, Mathilde Marchandon, James Biemiller, and John Rekoske. "3D Dynamic Rupture Modeling of the 6 February 2023, Kahramanmaraş, Turkey Mw 7.8 and 7.7 Earthquake Doublet Using Early Observations." Seismic Record 3, no. 4 (2023): 342–56. http://dx.doi.org/10.1785/0320230028.

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Abstract The 2023 Turkey earthquake sequence involved unexpected ruptures across numerous fault segments. We present 3D dynamic rupture simulations to illuminate the complex dynamics of the earthquake doublet. Our models are constrained by observations available within days of the sequence and deliver timely, mechanically consistent explanations of the unforeseen rupture paths, diverse rupture speeds, multiple slip episodes, heterogeneous fault offsets, locally strong shaking, and fault system interactions. Our simulations link both earthquakes, matching geodetic and seismic observations and r

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2

Lin, Yu Sen, Li Hua Xin, and Min Xiang. "Parameters Analysis of Train Running Performance on High-Speed Bridge during Earthquake." Advanced Materials Research 163-167 (December 2010): 4457–63. http://dx.doi.org/10.4028/www.scientific.net/amr.163-167.4457.

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A model of coupled vehicle-bridge system excited by earthquake and irregular track is established for studying train running performance on high-speed bridge during earthquake, by the methods of bridge structure dynamics and vehicle dynamics. The results indicate that under Qian’an earthquake waves vehicle dynamical responses hardly vary with the increasing-height pier, but vehicle dynamical responses increase evidently while the height of pier is 18m, which the natural vibration frequency is approaching to dominant frequency of earthquake waves. Dynamic responses are linearly increasing with

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3

Tiwari, Ram Krishna, and Harihar Paudyal. "Spatial mapping of b-value and fractal dimension prior to November 8, 2022 Doti Earthquake, Nepal." PLOS ONE 18, no. 8 (2023): e0289673. http://dx.doi.org/10.1371/journal.pone.0289673.

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An earthquake of magnitude 5.6 mb (6.6 ML) hit western Nepal (Doti region) in the wee hours of wednesday morning local time (2:12 AM, 2022.11.08) killing at least six people. Gutenberg-Richter b-value of earthquake distribution and correlation fractal dimension (D2) are estimated for 493 earthquakes with magnitude of completeness 3.6 prior to this earthquake. We consider earthquakes in western Nepal Himalaya and adjoining region (80.0–83.5°E and 27.3–30.5°N) for the period of 1964 to 2022 for the analysis. The b-value 0.68±0.03 implies a high stress zone and the spatial correlation dimension 1

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4

Ventura, Carlos E., W. D. Liam Finn, and Norman D. Schuster. "Seismic response of instrumented structures during the 1994 Northridge, California, earthquake." Canadian Journal of Civil Engineering 22, no. 2 (1995): 316–37. http://dx.doi.org/10.1139/l95-045.

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This paper presents an overview of strong motion records obtained from instrumented structures during the 1994 Northridge earthquake. It describes the behaviour of buildings, bridges, and dams that have been instrumented by the major strong motion instrumentation networks operating in California and highlights important features of the most significant structural motions recorded during the earthquake. The structural damage observed during a reconnaissance visit to the affected areas by the earthquake is correlated with preliminary analyses of the recorded motions. Detailed discussions of the

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Delorey, Andrew A., Kevin Chao, Kazushige Obara, and Paul A. Johnson. "Cascading elastic perturbation in Japan due to the 2012 Mw 8.6 Indian Ocean earthquake." Science Advances 1, no. 9 (2015): e1500468. http://dx.doi.org/10.1126/sciadv.1500468.

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Since the discovery of extensive earthquake triggering occurring in response to the 1992 Mw (moment magnitude) 7.3 Landers earthquake, it is now well established that seismic waves from earthquakes can trigger other earthquakes, tremor, slow slip, and pore pressure changes. Our contention is that earthquake triggering is one manifestation of a more widespread elastic disturbance that reveals information about Earth’s stress state. Earth’s stress state is central to our understanding of both natural and anthropogenic-induced crustal processes. We show that seismic waves from distant earthquakes

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6

Wu, Gongcheng, Kanghua Zhang, Chonglang Wang, and Xing Li. "Nucleation Mechanism and Rupture Dynamics of Laboratory Earthquakes at Different Loading Rates." Applied Sciences 13, no. 22 (2023): 12243. http://dx.doi.org/10.3390/app132212243.

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The loading rate of tectonic stress is not constant during long-term geotectonic activity and significantly affects the earthquake nucleation and fault rupture process. However, the mechanism underlying the loading rate effect is still unclear. In this study, we conducted a series of experiments to explore the effect of the loading rate on earthquake nucleation and stick–slip characteristics. Through lab experiments, faults were biaxially loaded at varying rates to produce a series of earthquakes (stick–slip events). Both shear strain and fault displacement were monitored during these events.

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7

Sobolev, G. A. "Seismicity dynamics and earthquake predictability." Natural Hazards and Earth System Sciences 11, no. 2 (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 th

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Ramos, Marlon D., Prithvi Thakur, Yihe Huang, Ruth A. Harris, and Kenny J. Ryan. "Working with Dynamic Earthquake Rupture Models: A Practical Guide." Seismological Research Letters 93, no. 4 (2022): 2096–110. http://dx.doi.org/10.1785/0220220022.

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Abstract Dynamic rupture models are physics-based simulations that couple fracture mechanics to wave propagation and are used to explain specific earthquake observations or to generate a suite of predictions to understand the influence of frictional, geometrical, stress, and material parameters. These simulations can model single earthquakes or multiple earthquake cycles. The objective of this article is to provide a self-contained and practical guide for students starting in the field of earthquake dynamics. Senior researchers who are interested in learning the first-order constraints and gen

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9

Jiménez, A., K. F. Tiampo, and A. M. Posadas. "An Ising model for earthquake dynamics." Nonlinear Processes in Geophysics 14, no. 1 (2007): 5–15. http://dx.doi.org/10.5194/npg-14-5-2007.

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Abstract. This paper focuses on extracting the information contained in seismic space-time patterns and their dynamics. The Greek catalog recorded from 1901 to 1999 is analyzed. An Ising Cellular Automata representation technique is developed to reconstruct the history of these patterns. We find that there is strong correlation in the region, and that small earthquakes are very important to the stress transfers. Finally, it is demonstrated that this approach is useful for seismic hazard assessment and intermediate-range earthquake forecasting.

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10

Charpentier, Arthur, and Marilou Durand. "Modeling earthquake dynamics." Journal of Seismology 19, no. 3 (2015): 721–39. http://dx.doi.org/10.1007/s10950-015-9489-9.

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11

Ohsawa, Yukio. "Regional Seismic Information Entropy to Detect Earthquake Activation Precursors." Entropy 20, no. 11 (2018): 861. http://dx.doi.org/10.3390/e20110861.

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A method is presented to detect earthquake precursors from time series data on earthquakes in a target region. The Regional Entropy of Seismic Information (RESI) is an index that represents the average influence of an earthquake in a target region on the diversity of clusters to which earthquake foci are distributed. Based on a simple qualitative model of the dynamics of land crust, it is hypothesized that the saturation that occurs after an increase in RESI precedes the activation of earthquakes. This hypothesis is validated by the earthquake catalog. This temporal change was found to correla

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12

Zimbidis, Alexandros A., Nickolaos E. Frangos, and Athanasios A. Pantelous. "Modeling Earthquake Risk via Extreme Value Theory and Pricing the Respective Catastrophe Bonds." ASTIN Bulletin 37, no. 01 (2007): 163–83. http://dx.doi.org/10.2143/ast.37.1.2020804.

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The aim of the paper is twofold. Firstly, to analyze the historical data of the earthquakes in the boarder area of Greece and then to produce a reliable model for the risk dynamics of the magnitude of the earthquakes, using advanced techniques from the Extreme Value Theory. Secondly, to discuss briefly the relevant theory of incomplete markets and price earthquake catastrophe bonds, combining the model found for the earthquake risk and an appropriate model for the interest rate dynamics in an incomplete market framework. The paper ends by providing some numerical results using Monte Carlo simu

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Zimbidis, Alexandros A., Nickolaos E. Frangos, and Athanasios A. Pantelous. "Modeling Earthquake Risk via Extreme Value Theory and Pricing the Respective Catastrophe Bonds." ASTIN Bulletin 37, no. 1 (2007): 163–83. http://dx.doi.org/10.1017/s0515036100014793.

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The aim of the paper is twofold. Firstly, to analyze the historical data of the earthquakes in the boarder area of Greece and then to produce a reliable model for the risk dynamics of the magnitude of the earthquakes, using advanced techniques from the Extreme Value Theory. Secondly, to discuss briefly the relevant theory of incomplete markets and price earthquake catastrophe bonds, combining the model found for the earthquake risk and an appropriate model for the interest rate dynamics in an incomplete market framework. The paper ends by providing some numerical results using Monte Carlo simu

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14

Zhang, J., F. Gao, H. Yu, and X. Zhao. "Use of an orthogonal parallel robot with redundant actuation as an earthquake simulator and its experiments." Proceedings of the Institution of Mechanical Engineers, Part C: Journal of Mechanical Engineering Science 226, no. 1 (2011): 257–72. http://dx.doi.org/10.1177/0954406211413050.

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In this article, an orthogonal 6-degree-of-freedom (DOF) parallel robot with redundant actuation is studied as an earthquake motion simulator. Taking the practical simulation of earthquake waves into consideration, the general characteristics of natural earthquakes are analysed and complexity and variety of seismic waves, three-dimensional and multi-DOF movement, and strong devastating force are regarded as the three obvious features in this article. Based on the characteristics of this orthogonal 6-DOF parallel robot with redundant actuation and the features of earthquakes, the feasibility of

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15

Zöller, G., and S. Hainzl. "Detecting premonitory seismicity patterns based on critical point dynamics." Natural Hazards and Earth System Sciences 1, no. 1/2 (2001): 93–98. http://dx.doi.org/10.5194/nhess-1-93-2001.

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Abstract. We test the hypothesis that critical point dynamics precedes strong earthquakes in a region surrounding the future hypocenter. Therefore, we search systematically for regions obeying critical point dynamics in terms of a growing spatial correlation length (GCL). The question of whether or not these spatial patterns are correlated with future seismicity is crucial for the problem of predictability. The analysis is conducted for earthquakes with M > 6.5 in California. As a result, we observe that GCL patterns are correlated with the distribution of future seismicity. In particular,

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16

Rosenau, Matthias, Fabio Corbi, and Stephane Dominguez. "Analogue earthquakes and seismic cycles: experimental modelling across timescales." Solid Earth 8, no. 3 (2017): 597–635. http://dx.doi.org/10.5194/se-8-597-2017.

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Abstract. Earth deformation is a multi-scale process ranging from seconds (seismic deformation) to millions of years (tectonic deformation). Bridging short- and long-term deformation and developing seismotectonic models has been a challenge in experimental tectonics for more than a century. Since the formulation of Reid's elastic rebound theory 100 years ago, laboratory mechanical models combining frictional and elastic elements have been used to study the dynamics of earthquakes. In the last decade, with the advent of high-resolution monitoring techniques and new rock analogue materials, labo

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17

Chugh, Ashok K., and J. Lawrence Von Thun. "Pore pressure response analysis for earthquakes." Canadian Geotechnical Journal 22, no. 4 (1985): 466–76. http://dx.doi.org/10.1139/t85-066.

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Modifications and extensions made to the computer programs APOLLO and GADFLEA for studying the generation and dissipation of pore water pressure in soil deposits under earthquake loading are presented. The revised versions of these computer programs permit a fuller use of the analytically estimated site-specific earthquake response of soil deposits. These changes do not, however, alter the basic formulation of the problem and the solution strategies implemented in the computer programs APOLLO and GADFLEA. It is argued that the dynamic pore pressure response results obtained through these progr

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18

Vasudevan, K., M. Cavers, and A. Ware. "Earthquake sequencing: chimera states with Kuramoto model dynamics on directed graphs." Nonlinear Processes in Geophysics 22, no. 5 (2015): 499–512. http://dx.doi.org/10.5194/npg-22-499-2015.

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Abstract. Earthquake sequencing studies allow us to investigate empirical relationships among spatio-temporal parameters describing the complexity of earthquake properties. We have recently studied the relevance of Markov chain models to draw information from global earthquake catalogues. In these studies, we considered directed graphs as graph theoretic representations of the Markov chain model and analyzed their properties. Here, we look at earthquake sequencing itself as a directed graph. In general, earthquakes are occurrences resulting from significant stress interactions among faults. As

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Vasudevan, K., M. Cavers, and A. Ware. "Earthquake sequencing: Chimera states with Kuramoto model dynamics on directed graphs." Nonlinear Processes in Geophysics Discussions 2, no. 1 (2015): 361–98. http://dx.doi.org/10.5194/npgd-2-361-2015.

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Abstract. Earthquake sequencing studies allow us to investigate empirical relationships among spatio-temporal parameters describing the complexity of earthquake properties. We have recently studied the relevance of Markov chain models to draw information from global earthquake catalogues. In these studies, we considered directed graphs as graph theoretic representations of the Markov chain model, and analyzed their properties. Here, we look at earthquake sequencing itself as a directed graph. In general, earthquakes are occurrences resulting from significant stress-interactions among faults. A

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20

Febriani, Dewi, and Siti Rohmah Nurhayati. "Description of the dynamics of the resilience of people victims of the 2018 North Lombok earthquake." IOP Conference Series: Earth and Environmental Science 884, no. 1 (2021): 012040. http://dx.doi.org/10.1088/1755-1315/884/1/012040.

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Abstract Before the earthquake struck lombok island on July 26, 2018, with a magnitude of 6.4 SR and on August 5, 2018 with a magnitude of 7.0 SR, it turned out that the history of earthquakes in Lombok had occurred 7 times from 1856 to 2013 with different strengths. So it can be concluded that lombok island is classified as a disaster prone area. Earthquakes include geological disasters that leave major impacts on lives, economies, infrastructure, the environment as well as psychological impacts. This research aims to describe the dynamics of the resilience of the victims of the 2018 North Lo

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21

Yin, Jiuxun, Zefeng Li, and Marine A. Denolle. "Source Time Function Clustering Reveals Patterns in Earthquake Dynamics." Seismological Research Letters 92, no. 4 (2021): 2343–53. http://dx.doi.org/10.1785/0220200403.

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Abstract We cluster a global database of 3529 Mw&gt;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 ten

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22

Rakuasa, Heinrich, S. Supriatna, A. Karsidi, A. Rifai, M. P. Tambunan, and A. Poniman K. "Spatial Dynamics Model of Earthquake Prone Area in Ambon City." IOP Conference Series: Earth and Environmental Science 1039, no. 1 (2022): 012057. http://dx.doi.org/10.1088/1755-1315/1039/1/012057.

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Abstract Ambon City has limitations in the development of residential areas because it is in an area prone to earthquake disasters, This is because Ambon City is in a very active tectonic area and 65% of settlement land / land built in Ambon City is in an active and weak fault zone and if there is a plate movement there will be an earthquake along the weak zone. One of the first steps to the effort to stigmatize disasters is to estimate how large the area of settlements that have been analyzed using cellular automata markov-chain located in earthquake-prone areas. This study aims to analyze ch

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23

Gotoh, K., M. Hayakawa, and N. Smirnova. "Fractal analysis of the ULF geomagnetic data obtained at Izu Peninsula, Japan in relation to the nearby earthquake swarm of June–August 2000." Natural Hazards and Earth System Sciences 3, no. 3/4 (2003): 229–36. http://dx.doi.org/10.5194/nhess-3-229-2003.

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Abstract. In our recent papers we applied fractal methods to extract the earthquake precursory signatures from scaling characteristics of the ULF geomagnetic data, obtained in a seismic active region of Guam Island during the large earthquake of 8 August 1993. We found specific dynamics of their fractal characteristics (spectral exponents and fractal dimensions) before the earthquake: appearance of the flicker-noise signatures and increase of the time series fractal dimension. Here we analyze ULF geomagnetic data obtained in a seismic active region of Izu Peninsula, Japan during a swarm of the

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Kearse, Jesse, Yoshihiro Kaneko, Tim Little, and Russ Van Dissen. "Curved slickenlines preserve direction of rupture propagation." Geology 47, no. 9 (2019): 838–42. http://dx.doi.org/10.1130/g46563.1.

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Abstract Slip-parallel grooves (striations) on fault surfaces are considered a robust indicator of fault slip direction, yet their potential for recording aspects of earthquake rupture dynamics has received little attention. During the 2016 Kaikōura earthquake (South Island, New Zealand), >10 m of dextral strike-slip on the steeply dipping Kekerengu fault exhumed >200 m2 of fresh fault exposure (free faces) where it crossed bedrock canyons. Inscribed upon these surfaces, we observed individual striae up to 6 m long, all of which had formed during the earthquake. These were typically curv

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Madden, E. H., M. Bader, J. Behrens, et al. "Linked 3-D modelling of megathrust earthquake-tsunami events: from subduction to tsunami run up." Geophysical Journal International 224, no. 1 (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 pr

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Chen, Jiemin, Zelin Yan, Linfeng Xu, Zhixin Liu, Yan Liu, and Jiawei Tian. "The Nonlinear Time Sequence Analysis in the Alpine-Himalayan Earthquake Zone." E3S Web of Conferences 299 (2021): 02001. http://dx.doi.org/10.1051/e3sconf/202129902001.

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The characteristics of the earthquake activity in the Eurasian earthquake zone, which is the second largest earthquake zone in the world, was investigated by researchers. The earthquake activity of the Eurasian earthquake zone was analysed in various disciplines, such as earth dynamics, rock mechanics, geology and tectonics. The emergence of fractal theory provided a new direction in exploring the characteristics of the earthquake activity in the Eurasian earthquake zone. This study processed the data on the earthquake activity in the Eurasian earthquake zone by self-similarity method and scal

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Nazarov, Yuriy P., and Vladimir I. Travush. "LONG-PERIOD SEISMIC IMPACTS AND IT AFFECTING ON THE STRENGTH OF HIGH-RISE BUILDINGS CONSTRUCTIONS." International Journal for Computational Civil and Structural Engineering 14, no. 4 (2018): 14–26. http://dx.doi.org/10.22337/2587-9618-2018-14-4-14-26.

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Currently, in all building codes, the diagrams of dynamics coefficient are limited to a maximum natural oscillation period of 1.8 s. However, this range is clearly not enough for the calculation of constructions of high-rise structures with characteristic basic periods of about 4-5 s and more. This article analyzes the available seis-mological data presented in the Center for Engineering Strong Motion Data (CESMD) database. The spectra of Tolioku earthquakes (Tohoku earthquake. Japan. March 11. 2011) and Emberley (New Zealand Earthquake. New Zealand. November 13, 2016) were studied, and dynami

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Johnson, Paul A., and Chris W. Johnson. "Earthquake fault slip and nonlinear dynamics." Journal of the Acoustical Society of America 153, no. 3_supplement (2023): A203. http://dx.doi.org/10.1121/10.0018661.

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Earthquake fault slip under shear forcing can be envisioned as a nonlinear dynamical process dominated by a single slip plane. In contrast, nonlinear behavior in Earth materials (e.g., rock) is driven by a strain-induced ensemble activation and slip of a large number of distributed features—cracks and grain boundary slip across many scales in the volume. The bulk recovery of a fault post-failure and that of a rock sample post dynamic or static forcing (”aging” or the “slow dynamics”) is very similar with approximate log(time) dependence for much of the recovery. In our work, we analyze large a

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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, no. 2196 (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 e

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Saito, Tatsuhiko, and Tatsuya Kubota. "Tsunami Modeling for the Deep Sea and Inside Focal Areas." Annual Review of Earth and Planetary Sciences 48, no. 1 (2020): 121–45. http://dx.doi.org/10.1146/annurev-earth-071719-054845.

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This article reviews tsunami modeling and its relation to recent developments of deep-ocean observations. Unlike near-coast observations, deep-ocean observations have enabled the capture of short-wavelength dispersive tsunamis and reflected waves from the coast. By analyzing these waves, researchers can estimate tsunami sources and earthquake slip distributions more reliably with higher spatial resolution. In addition, fractional tsunami speed reduction due to the elasticity of the Earth medium is now clearly detected. Densely and widely distributed tsunami sensors make it possible to observe

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VEITCH, STEPHEN A., and MEREDITH NETTLES. "Assessment of glacial-earthquake source parameters." Journal of Glaciology 63, no. 241 (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

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Carlson, J. M., J. S. Langer, and B. E. Shaw. "Dynamics of earthquake faults." Reviews of Modern Physics 66, no. 2 (1994): 657–70. http://dx.doi.org/10.1103/revmodphys.66.657.

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Zahariev, E. V. "Earthquake dynamic response of large flexible multibody systems." Mechanical Sciences 4, no. 1 (2013): 131–37. http://dx.doi.org/10.5194/ms-4-131-2013.

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Abstract. In the paper dynamics of large flexible structures imposed on earthquakes and high amplitude vibrations is regarded. Precise dynamic equations of flexible systems are the basis for reliable motion simulation and analysis of loading of the design scheme elements. Generalized Newton–Euler dynamic equations for rigid and flexible bodies are applied. The basement compulsory motion realized because of earthquake or wave propagation is presented in the dynamic equations as reonomic constraints. The dynamic equations, algebraic equations and reonomic constraints compile a system of differen

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SRIVASTAVA, H. N., S. N. BHATTACHARYA, D. T. RAO, and S. SRIVASTAVA. "Strange attractor in earthquake swarms near Valsad (Gujarat), India." MAUSAM 58, no. 4 (2021): 543–50. http://dx.doi.org/10.54302/mausam.v58i4.1439.

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Valsad district in south Gujarat near the western coast of the peninsular India experienced earthquake swarms since early February 1986. Seismic monitoring through a network of micro earthquake seismographs showed a well concentrated seismic activity over an area of 7 × 10 km2 with the depth of foci extending from 1 to 15 km. A total number of 21,830 earthquakes were recorded during March 1986 to June 1988. The daily frequency of earthquakes for this period was utilized to examine deterministic chaos through evaluation of dimension of strange attractor and Lyapunov exponent. The low dimension

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Danish, Aamar, Naveed Ahmad, and M. Usama Salim. "Manufacturing and Performance of an Economical 1-D Shake Table." Civil Engineering Journal 5, no. 9 (2019): 2019–28. http://dx.doi.org/10.28991/cej-2019-03091390.

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The researchers and engineers encountered many problems to precisely replicate earthquake waves. Earthquakes are one of the nature's worst catastrophes and are still unpredictable. Statistical research has shown that the earthquakes have increased in frequency in recent years and have become a major concern for the world especially for those countries which are located on the fault lines such as Japan, Bangladesh and Pakistan. So, it was imperative to device a mechanism to check earthquake response and apply some necessary mitigations for the safety of humanity. After many years of research an

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Erickson, Brittany A., Junle Jiang, Michael Barall, et al. "The Community Code Verification Exercise for Simulating Sequences of Earthquakes and Aseismic Slip (SEAS)." Seismological Research Letters 91, no. 2A (2020): 874–90. http://dx.doi.org/10.1785/0220190248.

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Abstract Numerical simulations of sequences of earthquakes and aseismic slip (SEAS) have made great progress over past decades to address important questions in earthquake physics. However, significant challenges in SEAS modeling remain in resolving multiscale interactions between earthquake nucleation, dynamic rupture, and aseismic slip, and understanding physical factors controlling observables such as seismicity and ground deformation. The increasing complexity of SEAS modeling calls for extensive efforts to verify codes and advance these simulations with rigor, reproducibility, and broaden

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Lu, Yin, Nadav Wetzler, Nicolas Waldmann, Amotz Agnon, Glenn P. Biasi, and Shmuel Marco. "A 220,000-year-long continuous large earthquake record on a slow-slipping plate boundary." Science Advances 6, no. 48 (2020): eaba4170. http://dx.doi.org/10.1126/sciadv.aba4170.

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Large earthquakes (magnitude ≥ 7.0) are rare, especially along slow-slipping plate boundaries. Lack of large earthquakes in the instrumental record enlarges uncertainty of the recurrence time; the recurrence of large earthquakes is generally determined by extrapolation according to a magnitude-frequency relation. We enhance the seismological catalog of the Dead Sea Fault Zone by including a 220,000-year-long continuous large earthquake record based on seismites from the Dead Sea center. We constrain seismic shaking intensities via computational fluid dynamics modeling and invert them for earth

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Al-Nammari, Fatima M. "Long-Term Recovery of Historic Buildings." International Journal of Mass Emergencies & Disasters 26, no. 1 (2008): 40–63. http://dx.doi.org/10.1177/028072700802600103.

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This paper explores the long-term earthquake recovery of historic buildings. The inquiry examines the dynamics of recovery from the 1989 Loma Prieta earthquake for three NGO and public buildings, and identifies the variables that influenced it. The investigation indicates that long-term earthquake recovery for historic buildings is challenging, dynamic, and can be improved. There are several variables that influence the complexity of the recovery but, complications in earthquake recovery can be reduced through pre-incident recovery planning. The inquiry also illustrates that recovery dynamics

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Dieterich, J. H. "Earthquake simulations with time-dependent nucleation and long-range interactions." Nonlinear Processes in Geophysics 2, no. 3/4 (1995): 109–20. http://dx.doi.org/10.5194/npg-2-109-1995.

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Abstract. A model for rapid simulation of earthquake sequences is introduced which incorporates long-range elastic interactions among fault elements and time-dependent earthquake nucleation inferred from experimentally derived rate- and state-dependent fault constitutive properties. The model consists of a planar two-dimensional fault surface which is periodic in both the x- and y-directions. Elastic interactions among fault elements are represented by an array of elastic dislocations. Approximate solutions for earthquake nucleation and dynamics of earthquake slip are introduced which permit c

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Sharma, Ajanta, and Farha Zaman. "The Great Assam Earthquake of 1950: A Historical Review." Senhri Journal of Multidisciplinary Studies 4, no. 1 (2019): 1–10. http://dx.doi.org/10.36110/sjms.2019.04.01.001.

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Northeast India is prone to major earthquake events due to its geographical and tectonic settings. Recurrence of the earthquakes in this part of India is frequent and associated with devastating events. Earthquake scenario in the region is very dangerous as the unplanned settlements with rise in population increased the vulnerability of human life. To understand such a risk and variability in human life and changes in natural dynamics; it is essential to know and study the past earthquake events. In northeast India, the last most devastating earthquake was the great Assam earthquake of 15th Au

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Stiros, Stathis C. "Intensities of ancient earthquakes, earthquake magnitude and soil dynamics effects. Evidence from the 1750 Croatia earthquake." Geodesy and Geodynamics 10, no. 4 (2019): 339–45. http://dx.doi.org/10.1016/j.geog.2018.03.005.

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Efstathiou, A., A. Tzanis, and F. Vallianatos. "ON THE NATURE AND DYNAMICS OF THE SEISMOGENETIC SYSTEM OF SOUTH CALIFORNIA, USA: AN ANALYSIS BASED ON NON-EXTENSIVE STATISTICAL PHYSICS." Bulletin of the Geological Society of Greece 50, no. 3 (2017): 1329. http://dx.doi.org/10.12681/bgsg.11839.

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We examine the nature of the seismogenetic system in South California, USA, by searching for evidence of non-extensivity in the earthquake record. We attempt to determine whether earthquakes are generated by a self-excited Poisson process, in which case they obey Boltzmann-Gibbs thermodynamics, or by a Critical process, in which long-range interactions in non-equilibrium statesare expected (correlation) and the thermodynamics deviate from the Boltzmann-Gibbs formalism. Emphasis is given to background earthquakes since it is generally agreed that aftershock sequences comprise correlated sets. A

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Tian, Yun, Linfeng Wang, Honghua Jin, and Biao Zeng. "Dynamic Response of Seismic Dangerous Rock Based on PFC and Dynamics." Advances in Civil Engineering 2020 (October 31, 2020): 1–19. http://dx.doi.org/10.1155/2020/8846130.

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Rock slope instability by earthquakes results in substantial economic and property losses. The calculation method of interlayer load and stability coefficient of horizontal complex layered rock slopes in high-intensity areas is established from material mechanics, fracture mechanics, and dynamics. The stability of horizontal layered dangerous rock is calculated after combining it with PFC simulation technology to verify the rationality of the calculation in the Wenchuan area of Sichuan Province. The dynamic response characteristics of dangerous rocks under different weathering degrees are also

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Tian, Xue, Xinyu Ma, Maowei Huang, et al. "Spatiotemporal Dynamic Characteristics of Land Use in the Typical Watershed of Wenchuan Earthquake-Affected Areas—A Case Study in the Longxi River Basin." Sustainability 14, no. 23 (2022): 15937. http://dx.doi.org/10.3390/su142315937.

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Major earthquakes cause serious damage to ecosystem structure and function through their huge destructive force and subsequent geohazards. Understanding the characteristics of post-earthquake land use change is of great interest to assess the effects of ecological restoration in earthquake-affected areas. However, little is known about the consequences of land use change on a small scale due to incomplete, non-comprehensive, and sparse research data. Here, we used remote-sensing images to study the land use change characteristics of the Longxi River before and after the Wenchuan earthquake by

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FUKUYAMA, Eiichi. "Parameters for Earthquake Rupture Dynamics." Zisin (Journal of the Seismological Society of Japan. 2nd ser.) 61, Supplement (2009): 309–14. http://dx.doi.org/10.4294/zisin.61.309.

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Chelidze, Tamaz, and Teimuraz Matcharashvili. "Electromagnetic control of earthquake dynamics?" Computers & Geosciences 29, no. 5 (2003): 587–93. http://dx.doi.org/10.1016/s0098-3004(03)00040-2.

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Nakanishi, Hiizu. "Complex Behavior in Earthquake Dynamics." International Journal of Modern Physics B 12, no. 03 (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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Bonham-Carter, Graeme. "Soil dynamics and earthquake engineering." Computers & Geosciences 17, no. 4 (1991): 594. http://dx.doi.org/10.1016/0098-3004(91)90119-x.

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Aldrighetti, Silvia, Giorgio Pennacchioni, and Giulio Di Toro. "Earthquake dynamics from pseudotachylyte microstructure." Earth and Planetary Science Letters 663 (August 2025): 119424. https://doi.org/10.1016/j.epsl.2025.119424.

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Olsen-Kettle, Louise, Hans Mühlhaus, and Christian Baillard. "A study of localization limiters and mesh dependency in earthquake rupture." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 368, no. 1910 (2010): 119–30. http://dx.doi.org/10.1098/rsta.2009.0190.

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No complete physically consistent model of earthquake rupture exists that can fully describe the rich hierarchy of scale dependencies and nonlinearities associated with earthquakes. We study mesh sensitivity in numerical models of earthquake rupture and demonstrate that this mesh sensitivity may provide hidden clues to the underlying physics generating the rich dynamics associated with earthquake rupture. We focus on unstable slip events that occur in earthquakes when rupture is associated with frictional weakening of the fault. Attempts to simulate these phenomena directly by introducing the

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