2010
DOI: 10.1785/0120090253
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Coseismic Slip Distribution of the 2008 Mw 7.9 Wenchuan Earthquake from Joint Inversion of GPS and InSAR Data

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Cited by 117 publications
(101 citation statements)
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“…1). The depth of 5 km suggests that a large part of the seismic moment releases in shallow depths, which is consistent with existing fault slip models (Shen et al 2009;Xu et al 2010;Wang et al 2011). The best-fit mechanism distribution along the optimal line fault is shown in Fig.…”
Section: A P P L I C At I O N T O T H E 2 0 0 8 M W 7 9 W E N C H Usupporting
confidence: 88%
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“…1). The depth of 5 km suggests that a large part of the seismic moment releases in shallow depths, which is consistent with existing fault slip models (Shen et al 2009;Xu et al 2010;Wang et al 2011). The best-fit mechanism distribution along the optimal line fault is shown in Fig.…”
Section: A P P L I C At I O N T O T H E 2 0 0 8 M W 7 9 W E N C H Usupporting
confidence: 88%
“…At the two ends of the line fault, where neither ruptures nor aftershocks were found (Xu et al 2010;Wang et al 2011;Hartzell et al 2013), scalar moments were fixed to be zeros. We have tried different smoothing factors (λ), and found that values between 1 and 10 are all acceptable.…”
Section: A P P L I C At I O N T O T H E 2 0 0 8 M W 7 9 W E N C H Umentioning
confidence: 99%
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“…In the joint inversion, the Helmert variance component estimation (HVCE) method (Xu et al, 2010) was applied to determine the relative weighting between InSAR and GPS data. The final weighting between InSAR and GPS convergences to 1:3.6, close to the value derived by Wang and Fialko (2015).…”
Section: Data Handling and Modeling Methodsmentioning
confidence: 99%
“…Thus, we obtain more realistic models by discretizing the fault planes into sub-faults and solve for the slip on each patch, thereby allowing the slip to smoothly taper to zero towards the edges of the fault plane. We use the inversion code SDM [25] based on the constrained least-squares method, which has been used in a number of recent publications for analyzing GPS and InSAR coseismic deformation data (e.g., [26][27][28][29]). To overcome the problem of the non-uniqueness and instability of the inversion result, a smoothing constraint is applied to the slip distribution.…”
Section: Distributed Slip Modelmentioning
confidence: 99%