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Fig. 4 | Earth, Planets and Space

Fig. 4

From: Impact of crustal deformation detection by the DSI (difference of split-band interferograms) method with PALSAR-2 data: a case study on the 2016 Kumamoto Earthquake

Fig. 4

a Distribution of the GEONET stations used in the comparison of slant-range changes. The background depicts the slant-range change maps for Path 126 using the difference of split-band interferograms (DSI) analysis. The open diamond indicates GEONET station “960699,” the reference point of crustal deformation. b Comparison of slant-range changes obtained from the DSI analysis and GEONET. Triangles and circles indicate the slant-range changes for Paths 28 and 126, respectively

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