Static Slip Model of the 2017 Mw 5.4 Pohang, South Korea, Earthquake Constrained by the InSAR Data

被引:41
作者
Song, Seok Goo [1 ]
Lee, Hoonyol [2 ]
机构
[1] Korea Inst Geosci & Mineral Resources, Earthquake Res Ctr, 124 Gwahang No, Daejeon 34132, South Korea
[2] Kangwon Natl Univ, Dept Geophys, 1 Gangwondaehak Gil, Gangwon Do, South Korea
基金
新加坡国家研究基金会;
关键词
TENSILE FAULTS; DEFORMATION; INVERSION; SHEAR; RADAR; GPS;
D O I
10.1785/0220180156
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
An M-w 5.4 earthquake occurred in the city of Pohang in the southeastern part of the Korean Peninsula on 15 November 2017. It was a moderate-sized crustal event but triggered enormous attention from the Korean public because strong shaking was felt over the whole country, and it had been just a year since the M-w 5.5 Gyeongju earthquake, the largest instrumentally recorded event in the country. Both earthquakes occurred within 40 km of each other. The Pohang earthquake provides a unique opportunity to constrain the static slip model of an earthquake in Korea using spaceborne Interferometric Synthetic Aperture Radar (InSAR) observations because the focal depth is relatively shallow (similar to 4 km), and surface displacement fields were successfully obtained by both descending and ascending orbits of the Sentinel-1A/B satellites. We performed a linear slip inversion using the InSAR data. Our slip model reveals that a major slip associated with the event occurred in the northeastern part of the hypocenter rather than in the southwestern part. In addition, its rupture dimension and mean slip are 5 km (width) by 6 km (length) and 15 cm, respectively. The InSAR data also show that no significant postseismic deformation occurred after the event.
引用
收藏
页码:140 / 148
页数:9
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