2008
DOI: 10.1111/j.1365-246x.2007.03713.x
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A non-linear geodetic data inversion using ABIC for slip distribution on a fault with an unknown dip angle

Abstract: S U M M A R YWe have developed a method of geodetic data inversion for slip distribution on a fault with an unknown dip angle. A common strategy for obtaining slip distribution in previous studies is to first determine the fault geometry by minimizing the square misfit under the assumption of a uniform slip on a rectangular fault, and then apply the usual linear inversion technique to estimate a slip distribution on the determined fault. It is not guaranteed, however, that the fault determined under the assump… Show more

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Cited by 120 publications
(97 citation statements)
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“…This example highlights the abstract nature of the coimage subspace: a truncated model, although robust, may display source patterns that are not directly amenable for physical interpretation. The enhanced sensitivity of the near-field observations is particularly visible when considering static displacement data, such as Interferometric Synthetic Aperture Radar data (e.g., Fukahata and Wright, 2008).…”
Section: Discussion Effect Of Station Distribution On Final Slip Biasmentioning
confidence: 99%
“…This example highlights the abstract nature of the coimage subspace: a truncated model, although robust, may display source patterns that are not directly amenable for physical interpretation. The enhanced sensitivity of the near-field observations is particularly visible when considering static displacement data, such as Interferometric Synthetic Aperture Radar data (e.g., Fukahata and Wright, 2008).…”
Section: Discussion Effect Of Station Distribution On Final Slip Biasmentioning
confidence: 99%
“…Previous studies (e.g., [44,47,48]) indicate that the fault geometry (especially the dip angle) derived from the uniform slip model is not optimal for the distribution slip model. In this study, the grid search method proposed by Feng et al [44] is used to determine the optimal dip and smoothing factor simultaneously.…”
Section: Finite Fault Slip Modelmentioning
confidence: 99%
“…We incorporate the cross-terms of the covariance matrix in the inversion scheme, following the equation presented by Fukahata and Wright (2008), and now take the characteristic correlation distance of errors to be 10 km (Wright et al, 2003;Fukahata and Wright, 2008). Figure 8 shows the calculated LOS displacement predicted from our model and the residual between the observations and the calculations.…”
Section: Slip Distribution Model For the M J 70 Eventmentioning
confidence: 99%
“…We cannot neglect the contribution of the cross-terms of the covariance matrix for the InSAR data, because they have a strong spatial correlation in general, which largely results from the variations of atmospheric water vapour (Lohman and Simons, 2005;Fukahata and Wright, 2008). We incorporate the cross-terms of the covariance matrix in the inversion scheme, following the equation presented by Fukahata and Wright (2008), and now take the characteristic correlation distance of errors to be 10 km (Wright et al, 2003;Fukahata and Wright, 2008).…”
Section: Slip Distribution Model For the M J 70 Eventmentioning
confidence: 99%