Simultaneous rupture propagation through fault bifurcation of the 2021 Mw7.4 Maduo earthquake
Fault geometric complexity plays a critical role in earthquake rupture dimension. Fault bifurcations are commonly observed in earthquake geology, yet, robust kinematic rupture processes on bifurcated fault branches are largely missing, limiting our understanding of rupture dynamics and seismic hazar...
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sg-ntu-dr.10356-1707652024-01-25T09:20:03Z Simultaneous rupture propagation through fault bifurcation of the 2021 Mw7.4 Maduo earthquake Wei, Shengji Zeng, Hongyu Shi, Qibin Liu, Jihong Luo, Heng Hu, Wan Lin Li, Yu Wang, Weitao Ma, Zhangfeng Liu-Zeng, Jing Wang, Teng Asian School of the Environment Earth Observatory of Singapore Science::Geology Maduo Earthquake Backprojections Fault geometric complexity plays a critical role in earthquake rupture dimension. Fault bifurcations are commonly observed in earthquake geology, yet, robust kinematic rupture processes on bifurcated fault branches are largely missing, limiting our understanding of rupture dynamics and seismic hazard. Here, we holistically study the fault geometry and bilateral rupture of the 2021 Mw7.4 Maduo, China earthquake, that shows clear fault bifurcation near its eastern terminal. We integrate space geodesy imaging, back-projection of high-frequency teleseismic array waveforms, multiple point source and finite fault inversions, and constrain in detail the rupture process, in particular, through its fault bifurcation. Our models reveal a stable rupture speed of ∼2.5 km/s throughout the entire rupture and a simultaneous rupture through fault branches bifurcated at 20°. The rupture on bifurcated faults radiated more high-frequency waves, especially from the stopping phases. The stopping phase on the southern branch likely stopped the rupture on the northern branch. Ministry of Education (MOE) National Research Foundation (NRF) Published version This research was supported by Singapore MOE project (MOE2019–T2–1–182) and the Earth Observatory of Singapore via its funding from the National Research Foundation Singapore and the Singapore Ministry of Education under the Research Centers of Excellence initiative. 2023-10-07T13:28:35Z 2023-10-07T13:28:35Z 2022 Journal Article Wei, S., Zeng, H., Shi, Q., Liu, J., Luo, H., Hu, W. L., Li, Y., Wang, W., Ma, Z., Liu-Zeng, J. & Wang, T. (2022). Simultaneous rupture propagation through fault bifurcation of the 2021 Mw7.4 Maduo earthquake. Geophysical Research Letters, 49(21), e2022GL100283-. https://dx.doi.org/10.1029/2022GL100283 0094-8276 https://hdl.handle.net/10356/170765 10.1029/2022GL100283 2-s2.0-85141939583 21 49 e2022GL100283 en MOE2019–T2–1–182 Geophysical Research Letters 10.21979/N9/NOKYXP © 2022 American Geophysical Union. All rights reserved. This article may be downloaded for personal use only. Any other use requires prior permission of the copyright holder. The Version of Record is available online at http://doi.org/10.1029/2022GL100283. application/pdf |
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Science::Geology Maduo Earthquake Backprojections Wei, Shengji Zeng, Hongyu Shi, Qibin Liu, Jihong Luo, Heng Hu, Wan Lin Li, Yu Wang, Weitao Ma, Zhangfeng Liu-Zeng, Jing Wang, Teng Simultaneous rupture propagation through fault bifurcation of the 2021 Mw7.4 Maduo earthquake |
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Fault geometric complexity plays a critical role in earthquake rupture dimension. Fault bifurcations are commonly observed in earthquake geology, yet, robust kinematic rupture processes on bifurcated fault branches are largely missing, limiting our understanding of rupture dynamics and seismic hazard. Here, we holistically study the fault geometry and bilateral rupture of the 2021 Mw7.4 Maduo, China earthquake, that shows clear fault bifurcation near its eastern terminal. We integrate space geodesy imaging, back-projection of high-frequency teleseismic array waveforms, multiple point source and finite fault inversions, and constrain in detail the rupture process, in particular, through its fault bifurcation. Our models reveal a stable rupture speed of ∼2.5 km/s throughout the entire rupture and a simultaneous rupture through fault branches bifurcated at 20°. The rupture on bifurcated faults radiated more high-frequency waves, especially from the stopping phases. The stopping phase on the southern branch likely stopped the rupture on the northern branch. |
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Asian School of the Environment |
author_facet |
Asian School of the Environment Wei, Shengji Zeng, Hongyu Shi, Qibin Liu, Jihong Luo, Heng Hu, Wan Lin Li, Yu Wang, Weitao Ma, Zhangfeng Liu-Zeng, Jing Wang, Teng |
format |
Article |
author |
Wei, Shengji Zeng, Hongyu Shi, Qibin Liu, Jihong Luo, Heng Hu, Wan Lin Li, Yu Wang, Weitao Ma, Zhangfeng Liu-Zeng, Jing Wang, Teng |
author_sort |
Wei, Shengji |
title |
Simultaneous rupture propagation through fault bifurcation of the 2021 Mw7.4 Maduo earthquake |
title_short |
Simultaneous rupture propagation through fault bifurcation of the 2021 Mw7.4 Maduo earthquake |
title_full |
Simultaneous rupture propagation through fault bifurcation of the 2021 Mw7.4 Maduo earthquake |
title_fullStr |
Simultaneous rupture propagation through fault bifurcation of the 2021 Mw7.4 Maduo earthquake |
title_full_unstemmed |
Simultaneous rupture propagation through fault bifurcation of the 2021 Mw7.4 Maduo earthquake |
title_sort |
simultaneous rupture propagation through fault bifurcation of the 2021 mw7.4 maduo earthquake |
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2023 |
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https://hdl.handle.net/10356/170765 |
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1789483050555408384 |