Regionally adjusted ground motion model: Case study of the ML6.2 (Mw6.4) Petrinja (Croatia) 2020 earthquake

IF 0.5 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Jakov Stanislav Uglešić, Filip Skendrović, Iva Lončar, Snježana Markušić, Davor Stanko
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引用次数: 0

Abstract

In the wake of recent 2020 ML ≥ 5.5 earthquakes in Croatia, Zagreb ML5.5 and Petrinja ML6.2, the insufficient instrumental network as well as the lack of regional ground motion prediction equation (GMPE) were identified as the drawbacks of our engineering community. The former is related to the quality definition of active seismicity (most of the instruments are installed in the southern part of Croatia with fewer installed around Zagreb in the northwestern part of Croatia), and the latter is related to the proper number of strong motion recordings. In Croatia, there is a sparse database of ground motion recordings for moderate earthquakes which makes a well-designed ground motion selecting procedure hardly achievable. Following this, strong motion BSHAP database for empirical estimation of the response spectrum based on Fourier amplitude spectrum and the ground motion duration using Random Vibration Theory approach adjusted to source, propagation, and local site conditions was used. Regionally adjusted ground motion model estimations for the ML6.2 Petrinja 2020 earthquake scenario are comparable with the previously published GMPEs models for this part of Europe and for the Western part of North America. However, model-to-model variability and uncertainties in local GMPE exceeded those of global GMPEs and are influenced by statistically less stable and more limited datasets. Model is applicable for magnitudes up to Mw6.5 and Joyner-Boore distances up to 200 km with usable frequency range between 0.4 and 33 Hz. The presented model is a step forward toward performing hybrid-empirical seismic hazard studies in areas with sparse ground motions such as the region of Croatia.

区域调整地面运动模型:以2020年克罗地亚佩特里尼亚ML6.2 (Mw6.4)地震为例
在最近的2020年克罗地亚ML≥5.5地震,萨格勒布ML5.5和佩特里尼亚ML6.2地震之后,仪器网络不足以及缺乏区域地面运动预测方程(GMPE)被认为是我们工程界的缺点。前者与活跃地震活动的质量定义有关(大多数仪器安装在克罗地亚南部,较少安装在克罗地亚西北部的萨格勒布附近),后者与强震记录的适当数量有关。在克罗地亚,有一个稀疏的中地震地面运动记录数据库,这使得设计良好的地面运动选择程序很难实现。在此基础上,采用基于傅立叶振幅谱和地震动持续时间的强震BSHAP数据库,利用随机振动理论方法对震源、传播和局部场地条件进行了调整,对响应谱进行了经验估计。pepetrinja 2020年ML6.2地震情景的区域调整地面运动模型估计与先前发布的欧洲该地区和北美西部的GMPEs模型相当。然而,本地GMPE的模式间变率和不确定性超过全球GMPE,并受到统计上不太稳定和更有限的数据集的影响。该模型适用于震级不超过Mw6.5,乔伊纳-布尔距离不超过200公里,可用频率范围在0.4至33赫兹之间。提出的模型是在克罗地亚等地震动稀少的地区进行混合经验地震危险性研究的一步。
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来源期刊
Studia Geophysica et Geodaetica
Studia Geophysica et Geodaetica 地学-地球化学与地球物理
CiteScore
1.90
自引率
0.00%
发文量
8
审稿时长
6-12 weeks
期刊介绍: Studia geophysica et geodaetica is an international journal covering all aspects of geophysics, meteorology and climatology, and of geodesy. Published by the Institute of Geophysics of the Academy of Sciences of the Czech Republic, it has a long tradition, being published quarterly since 1956. Studia publishes theoretical and methodological contributions, which are of interest for academia as well as industry. The journal offers fast publication of contributions in regular as well as topical issues.
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