[HTML][HTML] InSAR observation and inversion of the seismogenic fault for the 2017 Jiuzhaigou MS7.0 earthquake in China
LY JI, CJ LIU, J XU, L LIU, F LONG… - Chinese Journal of …, 2017 - en.dzkx.org
An earthquake with MS 7.0 occurred in Jiuzhaigou County, Sichuan Province on 8 August
2017. This work derives the coseismic deformation field based on Sentinel-1 SAR images by …
2017. This work derives the coseismic deformation field based on Sentinel-1 SAR images by …
Measuring coseismic deformation with spaceborne synthetic aperture radar: A review
JP Merryman Boncori - Frontiers in Earth Science, 2019 - frontiersin.org
In the past 25 years, space-borne Synthetic Aperture Radar imagery has become an
increasingly available data source for the study of crustal deformation associated with …
increasingly available data source for the study of crustal deformation associated with …
The 12 November 2017 Mw 7.3 Ezgeleh‐Sarpolzahab (Iran) Earthquake and Active Tectonics of the Lurestan Arc
Abstract The 12 November 2017 M w 7.3 Ezgeleh‐Sarpolzahab earthquake is the largest
instrumentally recorded earthquake in the Zagros Simply Folded Belt by a factor of∼ 10 in …
instrumentally recorded earthquake in the Zagros Simply Folded Belt by a factor of∼ 10 in …
Geodetic Constraints of the 2017 Mw7.3 Sarpol Zahab, Iran Earthquake, and Its Implications on the Structure and Mechanics of the Northwest Zagros Thrust‐Fold Belt
We reveal transient surface deformation following the 2017 Mw7. 3 Sarpol Zahab (Iran)
earthquake using Interferometric Synthetic Aperture Radar (InSAR) measurements. Based …
earthquake using Interferometric Synthetic Aperture Radar (InSAR) measurements. Based …
Coseismic Deformation Field of the Mw 7.3 12 November 2017 Sarpol-e Zahab (Iran) Earthquake: A Decoupling Horizon in the Northern Zagros Mountains Inferred …
The study of crustal deformation fields caused by earthquakes is important for a better
understanding of seismic hazard and growth of geological structures in tectonically active …
understanding of seismic hazard and growth of geological structures in tectonically active …
[HTML][HTML] Monitoring active open-pit mine stability in the Rhenish coalfields of Germany using a coherence-based SBAS method
W Tang, M Motagh, W Zhan - … Journal of Applied Earth Observation and …, 2020 - Elsevier
With the recent progress in synthetic aperture radar (SAR) technology, especially the new
generation of SAR satellites (Sentinel-1 and TerraSAR-X), our ability to assess slope …
generation of SAR satellites (Sentinel-1 and TerraSAR-X), our ability to assess slope …
Complex co-and postseismic faulting of the 2017–2018 seismic sequence in western Iran revealed by InSAR and seismic data
The largest earthquake in the Zagros Mountains struck the city of Azgeleh on the Iran–Iraq
border on 12 November 2017. This M w 7.3 earthquake was followed by an intense seismic …
border on 12 November 2017. This M w 7.3 earthquake was followed by an intense seismic …
Characterizing interseismic deformation of the **anshuihe fault, eastern Tibetan Plateau, using Sentinel-1 SAR images
L Ji, W Zhang, C Liu, L Zhu, J Xu, X Xu - Advances in Space Research, 2020 - Elsevier
The **anshuihe fault is a very large left-lateral strike-slip fault, located on the eastern
boundary of the Tibetan Plateau. In the late Cenozoic, this fault played a vital role in …
boundary of the Tibetan Plateau. In the late Cenozoic, this fault played a vital role in …
[HTML][HTML] 九寨沟MS7.0地震的InSAR观测及发震构造分析
季灵运， 刘传金， 徐晶， 刘雷， 龙锋， 张致伟 - 地球物理学报, 2017 - html.rhhz.net
2017 年8 月8 日四川省九寨沟县发生MS 7.0 地震. 本文基于Sentinel-1 SAR 影像, 利用InSAR
技术获取了此次地震的同震形变场, 反演获得同震滑动分布, 计算了同震位错对余震分布和周边 …
技术获取了此次地震的同震形变场, 反演获得同震滑动分布, 计算了同震位错对余震分布和周边 …
Depth‐Varying Friction on a Ramp‐Flat Fault Illuminated by∼ 3‐Year InSAR Observations Following the 2017 Mw 7.3 Sarpol‐e Zahab Earthquake
We use interferometric synthetic aperture radar observations to investigate the fault
geometry and afterslip evolution within 3 years after a mainshock. The postseismic …
geometry and afterslip evolution within 3 years after a mainshock. The postseismic …