The slow self-arresting nature of low-frequency earthquakes

Xueting Wei; Jiankuan Xu; Yuxiang Liu; Xiaofei Chen

doi:10.1038/s41467-021-25823-w

The slow self-arresting nature of low-frequency earthquakes

Nat Commun. 2021 Sep 15;12(1):5464. doi: 10.1038/s41467-021-25823-w.

Authors

Xueting Wei^{1

2}, Jiankuan Xu^{2

3}, Yuxiang Liu^{1

2}, Xiaofei Chen^{4

5}

Affiliations

¹ School of Earth and Space Sciences, University of Science and Technology of China, 230026, Hefei, China.
² Department of Earth and Space Sciences, Southern University of Science and Technology, 518055, Shenzhen, China.
³ Academy for Advanced Interdisciplinary Studies, Southern University of Science and Technology, 518055, Shenzhen, China.
⁴ Department of Earth and Space Sciences, Southern University of Science and Technology, 518055, Shenzhen, China. chenxf@sustech.edu.cn.
⁵ Shenzhen Key Laboratory of Deep Offshore Oil and Gas Exploration Technology, Southern University of Science and Technology, 518055, Shenzhen, China. chenxf@sustech.edu.cn.

Abstract

Low-frequency earthquakes are a series of recurring small earthquakes that are thought to compose tectonic tremors. Compared with regular earthquakes of the same magnitude, low-frequency earthquakes have longer source durations and smaller stress drops and slip rates. The mechanism that drives their unusual type of stress accumulation and release processes is unknown. Here, we use phase diagrams of rupture dynamics to explore the connection between low-frequency earthquakes and regular earthquakes. By comparing the source parameters of low-frequency earthquakes from 2001 to 2016 in Parkfield, on the San Andreas Fault, with those from numerical simulations, we conclude that low-frequency earthquakes are earthquakes that self-arrest within the rupture patch without any introduced interference. We also explain the scaling property of low-frequency earthquakes. Our findings suggest a framework for fault deformation in which nucleation asperities can release stress through slow self-arrest processes.

Abstract

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