中国云南省小地震临时观测资料中的近震源地动衰减特征

Hongrui Li, Hongwei Wang, R. Wen, Yefei Ren, Guoliang Lin, Jianwen Cui, Ying Zhou
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摘要

中国西南地区云南省的临时强震观测,从2008年至2018年的多次小地震中获得了一批宝贵的近源记录。基于云南省198次ML=2.0-4.3的小地震中,56个临时强震观测站获得的546个R=4-35km的经过良好处理的强震记录,我们建立了周期为0.1-2.0s的峰值地加速度和峰值谱加速度(PSA)的地动衰减模型,研究了小地震近源地动的衰减特征。我们的模型包括以 M 的二次函数形式表示的源项、与震级相关的几何扩展项以及水平地面运动的局部场地效应。我们的模型所预测的中值可以很好地描述在小型事件中观测到的近源地动的距离衰减。本研究的衰减模型很好地体现了几何扩展与震级和振荡周期的关系,即震级越大、周期越长,几何扩展越弱。我们的模型与 Sun19 模型(用于云南景谷地震序列中的小型余震)和 Zhang22 模型(用于中国西部中大型地震)进行了比较。与 Sun19 模型相比,我们的模型显示出较弱的距离衰减率和较弱的震源效应。同样,与 Zhang22 模型相比,我们的模型中周期大于 0.5 秒的 PSAs 的几何扩展较弱。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Attenuation Characteristics of Near-Source Ground Motions from Temporary Observations of Small Earthquakes in Yunnan Province, China
The temporary strong-motion observation in Yunnan Province, southwestern China, has obtained a valuable batch of near-source recordings from many small earthquakes from 2008 to 2018. Based on the 546 well-processed strong-motion recordings with R = 4–35 km, which were obtained at 56 temporary strong-motion stations in 198 small earthquakes with ML=2.0–4.3 in Yunnan Province, we established ground-motion attenuation models for peak ground acceleration and peak spectral accelerations (PSAs) at periods of 0.1–2.0 s and investigated the attenuation characteristics of the near-source ground motions of small events. Our model includes the source term represented by the quadratic functional form of M, the magnitude-dependent geometrical spreading term, and the local site effects on the horizontal ground motions. The predicted medians by our model can well describe the distance attenuation of the near-source ground motion observed in the small events. The attenuation model in this study well represents the dependence of geometrical spreading on both the magnitude and the oscillator period that is the larger the magnitude and the longer the period, the weaker the geometrical spreading. Our model was compared with the Sun19 model for small aftershocks in the Jinggu, Yunnan Province earthquake sequence and the Zhang22 model for moderate-to-large earthquakes in western China. Our model shows the weaker attenuation rate with distance and the weaker source effects, compared with the Sun19 model. Similarly, there is the weaker geometrical spreading for PSAs at periods greater than 0.5 s in our model than in the Zhang22 model.
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