A zoning model for seismic hazard analysis of Finland and adjacent areas: A fusion of seismological and geological data

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Tectonophysics Pub Date : 2025-06-18 Epub Date: 2025-04-21 DOI:10.1016/j.tecto.2025.230757
Päivi Mäntyniemi , Ludovic Fülöp , Kati Oinonen , Niina Junno , Emilia Kosonen , Annakaisa Korja
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Abstract

We present a new seismic zoning model for the territory of Finland and adjacent areas in northern Europe for the purpose of seismic hazard mapping. The target region, mostly situated in the stable continental region of the Fennoscandian Shield, exhibits predominantly earthquakes below moment magnitude 3.0. We have delineated area seismic source zones by fusing seismological, geological, and geophysical data, and tectonic boundaries. The approach is warranted to find sufficient argumentation on the zoning due to the poor to non-existent seismicity data in the eastern and southeastern part of our target region. We have addressed the subjectivity included in delineation of zone boundaries by combining the preliminary delineations of four expert groups into a model with three levels of details: macro-, meso- and microlevel. We compare the new microlevel zoning with the regional zoning models of 2015 and 2016 and all the three zonings with the respective zonings of the 2020 European Seismic Hazard Model. We argue that the new zoning model SZ2025FI provides a sufficient basis for seismic hazard mapping on national and regional scales, as well as European and global mapping initiatives.
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芬兰及其邻近地区地震灾害分析的分区模型:地震和地质数据的融合
我们提出了一个新的地震区划模型为芬兰和邻近地区的领土在北欧地震灾害测绘的目的。目标区域主要位于芬诺斯坎地盾的稳定大陆区域,主要表现为3.0级以下的地震。我们通过融合地震、地质和地球物理数据以及构造边界,划定了区域震源带。由于我们目标区域的东部和东南部地震活动数据贫乏或不存在,该方法有理由找到关于分区的充分论证。我们通过将四个专家组的初步划定结合到一个具有宏观、中观和微观三个层次细节的模型中,解决了区域边界划定中包含的主观性。我们将新的微观区划与2015年和2016年的区域区划模型进行了比较,并将这三个区划与2020年欧洲地震灾害模型的各自区划进行了比较。我们认为,新的分区模型SZ2025FI为国家和区域尺度的地震灾害制图以及欧洲和全球制图倡议提供了充分的基础。
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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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