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Interferometric synthetic aperture radar (InSAR) technique has been successfully used for mapping surface deformations [1-2], but it has been normally limited to a measurement along the radar line-of-sight (LOS) direction. For this reason, it is impossible to determine the north (N-S) component of surface deformation because of using data from near-polar orbiting satellites, and it is not sufficient to resolve the parameters of models for earthquakes and volcanic activities because there is a marked trade-off among model parameters . ?? 2011 KIEES.
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Three-dimensional surface deformation mapping by convensional interferometry and multiple aperture interferometry
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2011 3rd International Asia-Pacific Conference on Synthetic Aperture Radar, APSAR 2011