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DOI | 10.1016/j.epsl.2020.116528 |
Anomalously low aftershock productivity of the 2019 MW 8.0 energetic intermediate-depth faulting beneath Peru | |
Ye L.; Lay T.; Kanamori H. | |
发表日期 | 2020 |
ISSN | 0012821X |
卷号 | 549 |
英文摘要 | The 26 May 2019 Peru (MW 8.0) earthquake struck within the nearly-horizontal underthrust Nazca plate at depths from ∼110 to 150 km below the upper Amazon, near a steep bend in the plate where it plunges down to a deep earthquake zone. Little prior seismicity occurred in this region, but large intraslab events with similar normal-faulting mechanisms have occurred to the west. The event is situated in a similar slab position to the 2017 Puebla-Morelos, Mexico earthquake, but the remote location resulted in limited loss of life and damage. Back-projection imaging and finite-fault inversion based on teleseismic data suggest a brittle and energetic rupture process with unilateral expansion northward over a 170-km-long zone at a rupture speed, Vr ∼3 km/s, with three normal-faulting patches of up to ∼4.5 m slip. Despite the mainshock size, it produced only three M4.0+ aftershocks within 300 km (one nearby); the aftershock productivity of the 2019 Peru earthquake is very low even among all large intermediate-depth earthquakes, but similar to that for other large Peruvian intraslab events. Comparison of aftershock productivity of the Peru event with that of global large earthquakes in various tectonic settings suggests that the low aftershock productivity can largely be attributed to regionally homogeneous faulting systems and relatively uniform stress state in the flat Peru slab. © 2020 |
关键词 | 2019 Peru earthquakeaftershock productivityflat slabintermediate-depth earthquakesstress heterogeneity |
英文关键词 | Fault slips; Productivity; Back-projection imaging; Deep earthquakes; Finite fault inversions; Intermediate depths; Intermediate-depth earthquakes; Large earthquakes; Mexico earthquake; Tectonic settings; Earthquakes; aftershock; earthquake event; earthquake magnitude; heterogeneity; normal fault; seismic velocity; seismicity; tectonic setting; Peru |
语种 | 英语 |
来源期刊 | Earth and Planetary Science Letters
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/202989 |
作者单位 | Guangdong Provincial Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou, China; Department of Earth and Planetary Sciences, University of California Santa Cruz, Santa Cruz, CA 95064, United States; Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125, United States |
推荐引用方式 GB/T 7714 | Ye L.,Lay T.,Kanamori H.. Anomalously low aftershock productivity of the 2019 MW 8.0 energetic intermediate-depth faulting beneath Peru[J],2020,549. |
APA | Ye L.,Lay T.,&Kanamori H..(2020).Anomalously low aftershock productivity of the 2019 MW 8.0 energetic intermediate-depth faulting beneath Peru.Earth and Planetary Science Letters,549. |
MLA | Ye L.,et al."Anomalously low aftershock productivity of the 2019 MW 8.0 energetic intermediate-depth faulting beneath Peru".Earth and Planetary Science Letters 549(2020). |
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