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Relevant bibliographies by topics / Earthquake complexity

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Journal articles

Academic literature on the topic 'Earthquake complexity'

Author: Grafiati

Published: 10 March 2023

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Journal articles on the topic "Earthquake complexity"

1

KIKUCHI, Masayuki. "Complexity of Earthquake Source Processes." Zisin (Journal of the Seismological Society of Japan. 2nd ser.) 44, Supplement (1991): 301–14. http://dx.doi.org/10.4294/zisin1948.44.supplement_301.

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2

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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3

Vallianatos, F., G. Michas, G. Papadakis, and A. Tzanis. "Evidence of non-extensivity in the seismicity observed during the 2011–2012 unrest at the Santorini volcanic complex, Greece." Natural Hazards and Earth System Sciences 13, no. 1 (2013): 177–85. http://dx.doi.org/10.5194/nhess-13-177-2013.

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Abstract. During the period of October 2011–January 2012, an increase of earthquake activity has been observed in the volcanic complex of Santorini Island, Greece. Herein, the magnitude distribution of earthquakes as well as the temporal distribution of seismicity are studied. The statistics of both parameters exhibit complexity that is evident in the frequency-magnitude distribution and the inter-event time distribution, respectively. Because of this, we have used the analysis framework of non-extensive statistical physics (NESP), which seems suitable for studying complex systems. The observe

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4

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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5

Ando, R., and T. Yamashita. "Fault Zone Complexity and Earthquake Ruptures." Scientific Drilling SpecialIssue (November 1, 2007): 27–28. http://dx.doi.org/10.5194/sd-specialissue-27-2007.

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6

Rice, J. R., and Y. Ben-Zion. "Slip complexity in earthquake fault models." Proceedings of the National Academy of Sciences 93, no. 9 (1996): 3811–18. http://dx.doi.org/10.1073/pnas.93.9.3811.

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7

Barnhart, William D., Gavin P. Hayes, and David J. Wald. "Global Earthquake Response with Imaging Geodesy: Recent Examples from the USGS NEIC." Remote Sensing 11, no. 11 (2019): 1357. http://dx.doi.org/10.3390/rs11111357.

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The U.S. Geological Survey National Earthquake Information Center leads real-time efforts to provide rapid and accurate assessments of the impacts of global earthquakes, including estimates of ground shaking, ground failure, and the resulting human impacts. These efforts primarily rely on analysis of the seismic wavefield to characterize the source of the earthquake, which in turn informs a suite of disaster response products such as ShakeMap and PAGER. In recent years, the proliferation of rapidly acquired and openly available in-situ and remotely sensed geodetic observations has opened new a

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8

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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9

BHATTACHARYA, S. N., K. C. SINHA RAY, and H. N. SRIVASTAVA. "Large fractal dimension of chaotic at tractor for earthquake sequence near Nurek reservoir." MAUSAM 46, no. 2 (2022): 187–92. http://dx.doi.org/10.54302/mausam.v46i2.3227.

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Fractal dimension of the chaotic attractor for earthquake sequence in Nurek dam based on 22.000 earthquakes detected during the period 1976-87 has been studied for this total period of observations as well as for the period from December 1977 to December 1987. The second period excluded increased seismic activity during second stage of filling the reservoir. Large fractal dimensions of the chaotic at tractor of 8.3 and 7.3 were found for the respective period which suggests the complexity of earthquake .dynamics in this region as compared to Koyna reservoir.

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10

Quintanar, Luis, J. Yamamoto, and Z. Jiménez. "Source mechanism of two 1994 intermediate-depth-focus earthquakes in Guerrero, Mexico." Bulletin of the Seismological Society of America 89, no. 4 (1999): 1004–18. http://dx.doi.org/10.1785/bssa0890041004.

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Abstract In May and December 1994, two medium-size, intermediate-depth-focus earthquakes occurred in Guerrero, Mexico, eastward of the rupture area of the great Michoacan earthquake of September 19, 1985. Even though these are not major earthquakes (∼6.4 Mw), they were widely felt through central and southern Mexico, with minor damage at Zihuatanejo and Acapulco, located along the Pacific coast, and Mexico City. Both earthquakes, separated by ∼100 km, have similar focal depths and magnitudes, however, their focal mechanisms, based upon the polarities of first arrivals, show some differences. T

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