The reservoir-induced 2023 Heyuan earthquake sequence in Guangdong, China and its geodynamic implications

IF 2.7 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Huimin Guan , Jianshe Lei , Dapeng Zhao , Xiaohui Hu
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Abstract

To better understand the mechanism of the 2023 M4.3 Heyuan earthquake sequence, we relocate the events of this sequence during January to August 2023 and determine a focal mechanism solution of the Heyuan mainshock. A total of 565 events including the mainshock are precisely relocated using the double-difference location method. Our results show that most of the events occurred in the Shijiao-Xingang-Baitian fault zone with focal depths of 7–13 km, and the aftershocks took place above the mainshock hypocenter. This sequence has obvious spatiotemporal distribution features. Before the mainshock, the seismicity was low, but within 1.5 h following the mainshock, the sequence extended toward a shallow depth and bounced back and forth in the east-west direction. Between 1.5 and 8 h after the mainshock, the sequence gradually converged to the Shijiao-Xingang-Baitian fault. After 8 h the sequence gradually extended to the eastern part of the fault. To further ascertain the seismogenic fault, we invert waveform data for the mainshock focal mechanism. Our result shows that the Heyuan earthquake had a left-lateral normal rupture with MW 4.1 and a focal depth of 9.8 km. The strike, dip, and rake angles of nodal plane I are 334°, 64°, and − 58°, whereas those of nodal plane II are 99°, 40°, and − 137°. Among the existing faults in the study area, the strike of nodal plane I is closer to that of the Shijiao-Xingang-Baitian fault, which could be the seismogenic fault. In addition, seismic tomography revealed a high-Vp/Vs anomaly in the Heyuan earthquake area, suggesting that the Xinfengjiang Reservoir infiltration can explain why the aftershocks spread eastward. These results indicate that the 2023 Heyuan earthquake sequence is related to the seepage of the Xingfengjiang Reservoir water leading to the local crustal stress field variation, which is helpful to understand the mechanism of reservoir-induced earthquakes worldwide.

Abstract Image

2023年广东河源水库诱发地震序列及其地球动力学意义
为了更好地理解2023年河源M4.3级地震序列的震源机制,我们对2023年1 - 8月河源M4.3级地震序列进行了重新定位,确定了震源机制解。采用双差定位法对包括主震在内的565个地震事件进行了精确定位。结果表明,地震活动主要发生在石椒-新港-白田断裂带,震源深度为7 ~ 13 km,余震发生在主震震源上方。该序列具有明显的时空分布特征。主震前地震活动性较低,但在主震后1.5 h内,层序向浅层延伸,并沿东西方向来回弹跳。在主震后1.5 ~ 8 h,层序逐渐收敛于石椒-新港-白田断裂。8 h后,层序逐渐向断层东部延伸。为了进一步确定发震断层,我们反演了主震震源机制的波形资料。结果表明,河源地震为左侧正破裂,震级4.1级,震源深度9.8 km。节面I的走向角、倾角和前倾角分别为334°、64°和- 58°,节面II的走向角为99°、40°和- 137°。研究区现有断裂中,节面I走向与石交-新港-白田断裂走向更接近,可能为发震断裂。此外,地震层析成像显示河源震区存在高vp /Vs异常,表明新丰江水库的入渗可以解释余震向东扩散的原因。这些结果表明,2023年河源地震序列与兴峰江水库水渗流导致局部地应力变化有关,有助于认识世界范围内水库诱发地震的机理。
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来源期刊
Tectonophysics
Tectonophysics 地学-地球化学与地球物理
CiteScore
4.90
自引率
6.90%
发文量
300
审稿时长
6 months
期刊介绍: The prime focus of Tectonophysics will be high-impact original research and reviews in the fields of kinematics, structure, composition, and dynamics of the solid arth at all scales. Tectonophysics particularly encourages submission of papers based on the integration of a multitude of geophysical, geological, geochemical, geodynamic, and geotectonic methods
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