Abstract
This study presents long-period wave propagation simulations of western Sichuan Basin during the 2008 Mw 7.9 Wenchuan, China, earthquake. The simulations utilize a 3D basin model considering unconsolidated Quaternary sediments, and a finite source model inverted from far-field records. The variations of slip amount, rise time, and rake angle of each subfault are directly obtained by inversion. We validate the seismic source and basin velocity models by comparing the synthetic velocity waveforms with observed records at 21 stations inside and outside the basin. Results show that our simulations can reproduce the main features of strong ground motions and seismic damage distributions, as well as high abnormal seismic intensity found at Tangchang town within the basin that are caused by deep and soft deposits. In addition, it is indicated that Sichuan Basin imposed noteworthy influence on wave propagation behaviors inside the basin during this event. First, ground motions are significantly amplified by basin sediments even for long-period waves, with a maximum factor (AF) of more than 8 and 5 for the horizontal and vertical component, respectively. However, no direct relevance between AF and sediment depth can be found. Then, the coupling of low-velocity sediments and interferences of delayed seismic waves radiated from different locations of large fault greatly change the strong ground motion distributions, and lengthen the strong shaking durations. In addition, vertical component ground motions are less affected by basin sediments compared with horizontals. Our study indicates that a higher-resolution source and basin velocity models are necessary for local strong ground motion prediction or seismic hazard analysis in the future, and seismic response of large-scale basins under successive rupture process deserve special attention.
Similar content being viewed by others
Data availability
Data for this study are provided by China Strong Motion Network Centre at Institute of Engineering Mechanics, China Earthquake Administration. Maps were generated using Generic Mapping tools (GMT; Wessel et al. 2013).
References
Anderson JG (2004) Quantitative measure of the goodness-of-fit of synthetic seismograms. 13th World Conf. on Earthquake Engineering Conference Proc. Vancouver, Canada, Paper 243
Anderson JG, Bodin P, Brune JN et al (1986) Strong ground motion from the Michoacan, Mexico. Earthq Sci 233(4768):1043–1049
Bard PY, Bouchon M (1985) The two-dimensional resonance of sediment-filled valleys. Bull Seismol Soc Am 75(2):519–541
Bjerrum LW, Sørensen MB, Atakan K (2010) Strong Ground-motion simulation of the 12 May 2008 Mw 7.9 Wenchuan earthquake, using various slip models. Bull Seism Soc Am 100(5B):2396–2424
Carcione JM, Kosloff D, Kosloff R (1988) Wave propagation simulation in a linear viscoelastic medium. Geophys J Int 95(3):597–611
Chaljub E, Moczo P, Tsuno S et al (2010) Quantitative comparison of four numerical predictions of 3D ground motion in the Grenoble Valley, France. Bull Seism Soc Am 100(4):1427–1455
Chang Y, Zhou H, Yu YX (2012) Strong ground motion simulation of the Wenchuan earthquake. Acta Seismolo Sinica 34(2):224–234 (in Chinese)
Fu L, Li XJ (2017) The kappa model of the Longmenshan region and its application to simulation of strong-ground motion by the Wenchuan Ms8.0 earthquake. Chin J Geophys 60(8):2935–2947 (in Chinese)
Guidotti R, Stupazzini M, Smerzini C et al (2011) Numerical study on the role of basin geometry and kinematic seismic source in 3D ground motion simulation of the 22 February 2011 Mw 6.2 Christchurch earthquake. Seismol Res Lett 82(6):767–782
Guo E, Zhou XY (2010) Study on basin effects of Wenchuan earthquake. J Disaster Prevent Mitig Eng 30(4):459–465 (in Chinese)
Hao M, Xie LL (2007) The isoseismal of seismic intensity for the 9.21 Taiwan Chi-Chi earthquake of 1999. J Harbin Inst Technol 39(2):169–172 (in Chinese)
Hartzell S, Mendoza C, Ramirez-Guzman L et al (2013) Rupture History of the 2008 Mw 7.9 Wenchuan, China, earthquake: evaluation of separate and joint inversions of geodetic, teleseismic, and strong-motion data. Bull Seism Soc Am 103(1):353–370
He YW (1992) The age of formation of the Chengdu basin and features of its early deposits. Geol Review 38(2):149–156 (in Chinese)
Ji C, Hayes G (2008) Source model of the May 12th 2008 Wenchuan earthquake. http://earthquake.usgs.gov/eqcenter/eqarchives/poster/2008/20080512.php
Komatitsch D, Tromp J (1999) Introduction to the spectral element method for three-dimensional seismic wave propagation. Geophys J Int 139(3):806–822
Komatitsch D, Liu Q, Tromp J et al (2004) Simulations of ground motion in the Los Angeles basin based upon the spectral-element method. Bull Seismol Soc Am 94(1):187–206
Kristeková M, Kristek J, Moczo P et al (2006) Misfit CRITERIA for quantitative comparison of seismograms. Bull Seism Soc Am 96(5):1836–1850
Lin XD, Ge HK, Xu P et al (2013) Near field full waveform inversion: Lushan magnitude 7.0 earthquake and its aftershock moment tensor. Chin J Geophys 56(12):4037–4047 (in Chinese)
Liu QF, Yu YY, Yin DY et al (2018) Simulations of strong motion in the Weihe basin during the Wenchuan earthquake by spectral element method. Geophys J Int 215(2):978–995
Luo et al (1981) Compilation of Sichuan earthquake data. Sichuan people’s publishing house
Maufroy E, Chaljub E, Hollender F et al (2015) Earthquake ground motion in the Mygdonian basin, Greece: The E2VP verification and validation of 3D numerical simulation up to 4 Hz. Bull Seism Soc Am 105(3):1398–1418
Meng LY, Shi BP (2011) Near-fault strong ground motion simulation of the May 12, 2008, Mw 7.9 Wenchuan earthquake by dynamical composite source model. Chin J Geophys 54(4):1010–1027 (in Chinese)
Meng GJ, Su XN, Wang Z et al (2018) Joint inversion of the rupture process of the 2008 Wenchuan Ms8.0 earthquake from 1 Hz GPS, strong motion and teleseismic data. Earthquake 38(2):11–27 (in Chinese)
Nakamura T, Tsuboi S, Kaneda Y et al (2010) Rupture process of the 2008 Wenchuan, China earthquake inferred from teleseismic waveform inversion and forward modeling of broadband seismic waves. Tectonophysics 491(1):72–84
Sato T, Helmberger DV, Somerville PG et al (1998) Estimates of regional and local strong motions during the great 1923 Kanto, Japan, earthquake (Ms 8.2). Part 1: source estimation of a calibration event and modeling of wave propagation paths. Bull Seism Soc Am 88(1):183–205
Taborda R, Bielak J (2014) Ground-motion simulation and validation of the 2008 Chino Hills, California, earthquake using different velocity models. Bull Seism Soc Am 104(4):1876–1898
Taborda R, Azizzadeh-Roodpish S, Khoshnevis N et al (2016) Evaluation of the southern California seismic velocity models through simulation of recorded events. Geophys J Int 205(3):1342–1364
Wang P, Liu J (2014) The role of the transverse structure in reverse-type earthquake rupture propagation: a case study on the Xiaoyudong fault in the Wenchuan earthquake. Chin J Geophys 57(10):3296–3307 (in Chinese)
Wang WM, Zhao LF, Li J et al (2008) Rupture process of the Ms 8.0 Wenchuan earthquake of Sichuan, China. Chin J Geophys 51(5):1403–1410 (in Chinese)
Wessel P, Smith WHF, Scharroo R et al (2013) Generic mapping tools: improved version released. Eos Trans AGU 94:409–410
Xu SS, Deng TG, Du PS et al (2008) Investigation on the seismic disasters in the region of Chengdu city caused by the Ms8.0 Wenchuan earthquake. Earthq Res Sichuan 4:12–19
Yao XD, Zhang WB, Yu XW (2015) Simulation of near-field strong ground motion caused by the 2008 Ms8.0 Wenchuan earthquake. Chin J Geophys 58(3):886–903 (in Chinese)
Yoshimoto K, Takemura S (2014) A study on the predominant period of long-period ground motions in the Kanto Basin, Japan. Earth Planets Space 66(1):1–7
Yu YY, Ding HP, Liu QF (2017) Three-dimensional simulations of strong ground motion in the Sichuan basin during the Wenchuan earthquake. Bull Earthq Eng 15(11):4661–4679
Yuan YF (2008) Loss assessment of Wenchuan earthquake. J Earthq Eng Eng Vib 28(5):10–19 (in Chinese)
Zhang YG, Yang GZ (1983) Determination of Q-value by the coda wave for a portion of the Sichuan province. Acta Seismol Sin 5(3):304–312 (in Chinese)
Zhang W, Shen Y, Chen XF (2008) Numerical simulation of strong ground motion for the M s8.0 Wenchuan earthquake of 12 May 2008. Sci China Ser D Earth Sci 51(12):1673–1682
Zhao CP, Chen ZL, Hua W et al (2011) Study on source parameters of small to moderate earthquakes in the main seismic active regions. China Mainland Chin J Geophys 54(6):1478–1489 (in Chinese)
Zhao YJ, Zhang GH, Shan XJ et al (2018) Numerical simulation of the strong ground motion of the 2008 Wenchuan earthquake incorporated with topography and barrier rupture model. Chin J Geophys 61(5):1853–1862 (in Chinese)
Zhu GS (2013) Strong ground motion simulation by finite difference method. University of Science and Technology of China
Acknowledgements
This research is supported by the Scientific Research Fund of Institute of Engineering Mechanics, China Earthquake Administration (Grant No. 2021EEEVL0001), and the National Natural Science Foundation of China under Grant No. 51808371.
Author information
Authors and Affiliations
Corresponding authors
Rights and permissions
Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
About this article
Cite this article
Liu, Q., Yu, Y. & Ding, H. Long-Period Ground Motion Simulation of the 2008 Mw7.9 Wenchuan Earthquake Considering the Western Sichuan Basin. Iran J Sci Technol Trans Civ Eng 48, 169–183 (2024). https://doi.org/10.1007/s40996-023-01141-7
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s40996-023-01141-7