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Surface deformations of the 6 February 2023 earthquake sequence, eastern Türkiye
被引:12
|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
来源:
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.
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页码:298 / 305
页数:8
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