Surface deformations of the 6 February 2023 earthquake sequence, eastern Türkiye

被引:29
|
作者
Meng, Jiannan [1 ,2 ]
Kusky, Timothy [1 ,2 ,3 ]
Mooney, Walter D. [4 ]
Bozkurt, Erdin [3 ]
Bodur, Mehmet Nuri [5 ]
Wang, Lu [1 ]
机构
[1] China Univ Geosci, Ctr Global Tecton, Sch Earth Sci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
[2] China Univ Geosci, Badong Natl Observ & Res Stn Geohazards, Wuhan 430074, Peoples R China
[3] Middle East Tech Univ, Dept Geol Engn, TR-06800 Ankara, Turkiye
[4] US Geol Survey, Menlo Pk, CA 94025 USA
[5] Hakkari Univ, Fac Civil Engn, TR-30000 Hakkari, Turkiye
基金
中国国家自然科学基金;
关键词
STRIKE-SLIP FAULTS; POINT MEASUREMENTS; RUPTURE; ZONES; CALIFORNIA; MAGNITUDE; TECTONICS; EVOLUTION; INVERSION;
D O I
10.1126/science.adj3770
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Two powerful earthquakes struck T & uuml;rkiye on 6 February 2023. The initial rupture was on the Dead Sea fault zone, yet maximum displacements and energy release [moment magnitude (M-w) 7.8] occurred 24 seconds later when rupture transferred to the East Anatolian fault zone (EAFZ). More than 7 hours later, a M-w 4.5 aftershock at the junction of the EAFZ with the east-west striking & Ccedil;ardak-S & uuml;rg & uuml; fault was followed 86 minutes later by the second large (M-w 7.5) earthquake, suggesting a causal relationship. We provide quantitative ground and aerial documentation of surface offsets and kinematics from the slipped faults, providing important data on surface deformation during large continental strike-slip earthquakes, rupture propagation mechanisms, and how slip may be transferred between complex fault systems. We also provide insight into how slip along linked fault systems accommodates global plate motions.
引用
收藏
页码:298 / 305
页数:8
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