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Rupture Process of the 2008 Wenchuan, China, Earthquake: A Review

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Earthquake and Disaster Risk: Decade Retrospective of the Wenchuan Earthquake

Abstract

The May 12, 2008, Wenchuan earthquake (MW 7.9, MS 8.1) is the largest continental intraplate event to strike globally in the last 60 years. It caused great destruction and loss of life along the steep eastern margin of the Tibetan Plateau, adjacent to the Sichuan Basin. The event ruptured multiple faults with a mix of thrust- and right-lateral strike-slip faulting along the northeast-trending Longmen Shan thrust belt, with an overall oblique compressional deformation. Surface displacements of up to ~11 m, the distribution of thousands of aftershocks and landslides, geodetic observations, and seismic wave imaging indicate a total rupture extent of ~280 km, extending unilaterally northeastward from the hypocenter. The primary slip has a patchy distribution along the segmented out-of-sequence Beichuan fault, with large-slip patches in the region from Yingxiu to Xiaoyudong, near Beichuan, and near Nanba. The southwestern segment near Yingxiu, where the hanging wall is comprised of the high seismic velocity Pengguan massif, has primarily thrust displacement with minor right-lateral component. Strongly oblique slip occurred near Beichuan and progressively more steeply dipping right-lateral strike-slip dominates toward the northeast. The large-slip patches are less than 10 km deep, but slip extends deeper in the southwestern region and the fault appears to have listric extension into a mid-crustal décollement with shallow dip below 20 km depth. The rupture expanded with an average rupture velocity of ~2.8 ± 0.2 km/s along this segmented fault zone with a total rupture duration of ~110 s, with faster rupture speed in the northeastern region, possibly being supershear. Most aftershocks are concentrated from 10 to 20 km deep, below the large-slip zones. Predominantly thrust slip with vertical offset of ~3.5 m occurred at shallow depth along ~72 km of the imbricate Pengguan fault located 6–7 km to the southeast of the southern Beichuan fault. Shallower dip of the Pengguan fault may cause it to converge with the Beichuan fault at depth, and/or to flatten into the same mid-crustal décollement. Oblique compressional left-lateral slip occurred on the short conjugate southward-dipping Xiaoyudong fault, connecting the two range-parallel faults. The moment-scaled radiated energy of the Wenchuan event is higher than for typical interplate thrust faulting, likely contributing to the extensive damage.

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Change history

  • 27 June 2019

    In the original version of the book, the following belated corrections are to be incorporated.

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Acknowledgements

All seismological data used in finite-fault inversions by the author were obtained from the Incorporated Research Institutions for Seismology (IRIS) data management service (DMS) (https://www.iris.edu/hq/). Editor Yong-Gang Li provides helpful comments on the manuscript. The author’s research on earthquake processes is supported by the U.S. National Science Foundation grant EAR1802364. This chapter was prepared following the International Conference for the Decade Memory of the Wenchuan Earthquake (4th International Conference on Continental Earthquakes), May 12–14, 2018 in Chengdu, China. The author’s participation in that excellent conference was supported by the China Earthquake Administration.

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Lay, T. (2019). Rupture Process of the 2008 Wenchuan, China, Earthquake: A Review. In: Li, YG. (eds) Earthquake and Disaster Risk: Decade Retrospective of the Wenchuan Earthquake. Springer, Singapore. https://doi.org/10.1007/978-981-13-8015-0_2

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