Three-Dimensional Deformation of the 2023 Turkey Mw 7.8 and Mw 7.7 Earthquake Sequence Obtained by Fusing Optical and SAR Images

被引:23
作者
An, Qi [1 ]
Feng, Guangcai [1 ]
He, Lijia [1 ]
Xiong, Zhiqiang [1 ]
Lu, Hao [1 ]
Wang, Xiuhua [1 ]
Wei, Jianchao [2 ]
机构
[1] Cent South Univ, Sch Geosci & Info Phys, Changsha 410083, Peoples R China
[2] Hunan Univ Sci & Technol, Sch Earth Sci & Spatial Informat Engn, Xiangtan 411199, Peoples R China
基金
中国国家自然科学基金;
关键词
Turkey earthquake; optical image correlation; pixel offset tracking; 3D deformation monitoring; COSEISMIC DISPLACEMENTS; GLACIER; IMPROVEMENT; KINEMATICS; VELOCITIES; DYNAMICS; RADAR; INSAR; FIELD; SLIP;
D O I
10.3390/rs15102656
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In February 2023, Mw 7.8 and Mw 7.7 earthquakes struck southeastern Turkey. Generating a coseismic 3D deformation field that can directly reflect the characteristics of surface deformation is important for revealing the movement mode of a seismogenic fault and analyzing the focal mechanism. Optical image sub-pixel correlation (SPC) only captures deformation in the horizontal direction, and SAR image pixel offset tracking (POT) obtains range deformation that is not sensitive to north-south deformation signals. Thus, neither of them can capture the complete 3D deformation alone. Combining them may be able to allow the monitoring of 3D deformation. In this study, we used Sentinel-2 optical images to obtain the horizontal deformation (east-west and north-south) and Sentinel-1 and ALOS-2 data to extract the range and azimuth offsets. The least-squares method was used to fuse the optical and SAR offsets to obtain the 3D deformation field of the 2023 Turkey earthquake sequence, which indicates that the two events were both left-lateral strike-slip earthquakes. The surface deformation caused by the two large earthquakes is mainly in the east-west direction. In the vertical direction, the two earthquakes caused a small-magnitude uplift and subsidence. The findings in this paper can be used as a reference for the study of coseismic 3D deformation.
引用
收藏
页数:13
相关论文
共 39 条
[1]   Measuring two-dimensional movements using a single InSAR pair [J].
Bechor, Noa B. D. ;
Zebker, Howard A. .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (16)
[2]   Inversion of deformation fields time-series from optical images, and application to the long term kinematics of slow-moving landslides in Peru [J].
Bontemps, Noelie ;
Lacroix, Pascal ;
Doin, Marie-Pierre .
REMOTE SENSING OF ENVIRONMENT, 2018, 210 :144-158
[3]   Earthquake doublet in Turkey and Syria [J].
Dal Zilio, Luca ;
Ampuero, Jean-Paul .
COMMUNICATIONS EARTH & ENVIRONMENT, 2023, 4 (01)
[4]   Displacement history and potential triggering factors of Baige landslides, China revealed by optical imagery time series [J].
Ding, Chao ;
Feng, Guangcai ;
Liao, Mingsheng ;
Tao, Pengjie ;
Zhang, Lu ;
Xu, Qiang .
REMOTE SENSING OF ENVIRONMENT, 2021, 254 (254)
[5]  
Dogru F, 2020, PURE APPL GEOPHYS, V177, P5761, DOI 10.1007/s00024-020-02606-w
[6]   The East Anatolian Fault: geometry, segmentation and jog characteristics [J].
Duman, Tamer Y. ;
Emre, Omer .
GEOLOGICAL DEVELOPMENT OF ANATOLIA AND THE EASTERNMOST MEDITERRANEAN REGION, 2013, 372 :495-529
[7]   Three-dimensional deformation caused by the Bam, Iran, earthquake and the origin of shallow slip deficit [J].
Fialko, Y ;
Sandwell, D ;
Simons, M ;
Rosen, P .
NATURE, 2005, 435 (7040) :295-299
[8]   Geographic analysis of earthquake damage in Turkey between 1900 and 2012 [J].
Gokkaya, Kemal .
GEOMATICS NATURAL HAZARDS & RISK, 2016, 7 (06) :1948-1961
[9]   Velocities and flux of the Filchner ice shelf and its tributaries determined from speckle tracking interferometry [J].
Gray, AL ;
Short, N ;
Mattar, KE ;
Jezek, KC .
CANADIAN JOURNAL OF REMOTE SENSING, 2001, 27 (03) :193-206
[10]   Probabilistic Seismic-Hazard Assessment for East Anatolian Fault Zone Using Planar Fault Source Models [J].
Gulerce, Zeynep ;
Shah, Syed Tanvir ;
Menekse, Akin ;
Ozacar, Atilla Arda ;
Kaymakci, Nuretdin ;
Cetin, Kemal Onder .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2017, 107 (05) :2353-2366