The evolution process between the earthquake swarm beneath the Noto Peninsula,central Japan and the 2024 M 7.6 Noto Hanto earthquake sequence  

作　　者：Zhigang Peng Xinglin Lei Qing-Yu Wang Dun Wang Phuc Mach Dongdong Yao Aitaro Kato Kazushige Obara Michel Campillo 

机构地区：[1]School of Earth and Atomospheric Sciences,Georgia Institute of Technology,Atlanta,GA,30332,United States [2]Geological Survey of Japan,National Institute of Advanced Industrial Science and Technology,Tsukuba,Ibaraki,305-8567,Japan [3]Universite Grenoble Alpes,University Savoie Mont Blanc,CNRS,IRD,University Gustave Eiffel,ISTerre,Grenoble,38000,France [4]Chinese University of Geosciences,Wuhan,Hubei,430074,China [5]Earthquake Research Institute,University of Tokyo,Bunkyo City,Tokyo,113-0032,Japan

出　　处：《Earthquake Research Advances》2025年第1期10-21,共12页地震研究进展(英文)

基　　金：partially supported by U.S.National Science Foundation grants EAR1925965 and RISE-2425889;support from the European Research Council under the European Union Horizon 2020 research and innovation program(grant agreement no.742335,FIMAGE)。

摘　　要：Several physical mechanisms of earthquake nucleation,such as pre-slip,cascade triggering,aseismic slip,and fluid-driven models,have been proposed.However,it is still not clear which model plays the most important role in driving foreshocks and mainshock nucleation for given cases.In this study,we focus on the relationship between an intensive earthquake swarm that started beneath the Noto Peninsula in Central Japan since November 2020 and the nucleation of the 2024 M 7.6 Noto Hanto earthquake.We relocate earthquakes listed in the standard Japan Meteorological Agency(JMA)catalog since 2018 with the double-different relocation method.Relocated seismicity revealed that the 2024 M 7.6 mainshock likely ruptured a thrust fault above a parallel fault where the M 6.5 Suzu earthquake occurred in May 2023.We find possible along-strike and along-dip expansion of seismicity in the first few months at the beginning of the swarm sequence,while no obvious migration pattern in the last few days before the M 7.6 mainshock was observed.Several smaller events occurred in between the M 5.5 and M 4.6 foreshocks that occurred about 4min and 2 min before the M 7.6 mainshock.The Coulomb stress changes from the M 5.5 foreshock were negative at the hypocenter of the M 7.6 mainshock,which is inconsistent with a simple cascade triggering model.Moreover,an M 5.9 foreshock was identified in the JMA catalog 14 s before the mainshock.Results from backprojection of high-frequency teleseismic P waves show a prolonged initial rupture process near the mainshock hypocenter lasting for~25 s,before propagating bilaterally outward.Our results suggest a complex evolution process linking the earthquake swarm to the nucleation of the M 7.6 mainshock at a region of complex structures associated with the bend of a mapped large-scale reverse fault.A combination of fluid migration,aseismic slip and elastic stress triggering likely work in concert to drive both the prolonged earthquake swarm and the nucleation of the M 7.6 mainshock.

关 键 词：EARTHQUAKE BENEATH EVOLUTION 

分 类 号：P31[天文地球—固体地球物理学]