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Open AccessArticle

Heterogeneous Fault Mechanisms of the 6 October 2008 MW 6.3 Dangxiong (Tibet) Earthquake Using Interferometric Synthetic Aperture Radar Observations

by 1,2,3,*, 1, 1,2,3 and 1,2,3
1
School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China
2
Key Laboratory of Geospace Environment and Geodesy, Ministry of Education, Wuhan 430079, China
3
Collaborative Innovation Center of Geospatial Technology, Wuhan 430079, China
*
Author to whom correspondence should be addressed.
Academic Editors: Cheinway Hwang, Wenbin Shen, C.K. Shum, Stéphane Calmant, Zhong Lu and Prasad S. Thenkabail
Remote Sens. 2016, 8(3), 228; https://doi.org/10.3390/rs8030228
Received: 23 October 2015 / Revised: 25 February 2016 / Accepted: 1 March 2016 / Published: 12 March 2016
(This article belongs to the Special Issue Remote Sensing in Tibet and Siberia)
Most current crustal deformation models do not account for topographic effects, crustal lateral variations, and complex fault geometries. To overcome these limitations, we apply finite element models constrained by interferometric Synthetic Aperture Radar (InSAR) images of co-seismic displacements to the 2008 Mw 6.3 Dangxiong earthquake that occurred in Yadong–Gulu rift, southern Tibet. For mountainous plateau environments, InSAR observations are advantageous for studying crustal deformation and crustal medium structure. We evaluate the effect of topography and variations in Poisson’s ratio and elastic moduli on estimation of coseismic deformation from InSAR observations. The results show that coseismic surface displacements are more sensitive to variations in Young’s modulus than to variations in topography and Poisson’s ratio. Therefore, with constant Poisson’s ratio and density, we change the Young’s modulus on each side of the fault to obtain the model that best fits the observations. This is attained when the Young’s moduli in the eastern and western sides of the fault were 2.6 × 1010 Pa and 7.8 × 1010 Pa, respectively. The result is consistent with previous field surveys that the medium on either side of the fault is different. View Full-Text
Keywords: InSAR; finite element model; heterogeneous medium; coseismic deformation; Dangxiong earthquake InSAR; finite element model; heterogeneous medium; coseismic deformation; Dangxiong earthquake
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MDPI and ACS Style

Xu, C.; Xu, B.; Wen, Y.; Liu, Y. Heterogeneous Fault Mechanisms of the 6 October 2008 MW 6.3 Dangxiong (Tibet) Earthquake Using Interferometric Synthetic Aperture Radar Observations. Remote Sens. 2016, 8, 228. https://doi.org/10.3390/rs8030228

AMA Style

Xu C, Xu B, Wen Y, Liu Y. Heterogeneous Fault Mechanisms of the 6 October 2008 MW 6.3 Dangxiong (Tibet) Earthquake Using Interferometric Synthetic Aperture Radar Observations. Remote Sensing. 2016; 8(3):228. https://doi.org/10.3390/rs8030228

Chicago/Turabian Style

Xu, Caijun; Xu, Bei; Wen, Yangmao; Liu, Yang. 2016. "Heterogeneous Fault Mechanisms of the 6 October 2008 MW 6.3 Dangxiong (Tibet) Earthquake Using Interferometric Synthetic Aperture Radar Observations" Remote Sens. 8, no. 3: 228. https://doi.org/10.3390/rs8030228

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