Correction: Liu, Y. et al. Time-Dependent Afterslip of the 2009 Mw 6.3 Dachaidan Earthquake (China) and Viscosity beneath the Qaidam Basin Inferred from Postseismic Deformation Observations. Remote Sens. 2016, 8, 649

نویسندگان

  • Yang Liu
  • Caijun Xu
  • Zhenhong Li
  • Yangmao Wen
  • Jiajun Chen
  • Zhicai Li
چکیده

Yang Liu 1,2,3,4,*, Caijun Xu 1,2,3, Zhenhong Li 4, Yangmao Wen 1,2,3, Jiajun Chen 4 and Zhicai Li 5 1 School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China; [email protected] (C.X.); [email protected] (Y.W.) 2 Key Laboratory of Geospace Environment and Geodesy, Ministry of Education, Wuhan University, Wuhan 430079, China 3 Collaborative Innovation Center for Geospatial Technology, Wuhan 430079, China 4 COMET, School of Civil Engineering and Geosciences, Newcastle University, Newcastle upon Tyne NE1 7RU, UK; [email protected] (Z.L.); [email protected] (J.C.) 5 Department of Geodesy, National Geomatics Center of China, Beijing 100048, China; [email protected] * Correspondence: [email protected]; Tel.: +86-27-6877-8404

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Time-Dependent Afterslip of the 2009 Mw 6.3 Dachaidan Earthquake (China) and Viscosity beneath the Qaidam Basin Inferred from Postseismic Deformation Observations

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A New Perspective on Fault Geometry and Slip Distribution of the 2009 Dachaidan Mw 6.3 Earthquake from InSAR Observations

On 28 August 2009, the northern margin of the Qaidam basin in the Tibet Plateau was ruptured by an Mw 6.3 earthquake. This study utilizes the Envisat ASAR images from descending Track 319 and ascending Track 455 for capturing the coseismic deformation resulting from this event, indicating that the earthquake fault rupture does not reach to the earth's surface. We then propose a four-segmented f...

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عنوان ژورنال:
  • Remote Sensing

دوره 8  شماره 

صفحات  -

تاریخ انتشار 2016