Additional file 1: Figure S1. Co-seismic surface deformation observed by Multiple Aperture Interferometry (MAI) analysis using ALOS-2/PALSAR-2 data (modified after Geospatial Information Authority of Japan 2016a). Blue and red areas represent forward (roughly south) and backward (roughly north) horizontal deformation with respect to the flight direction. These analyses were performed by the Geospatial Information Authority of Japan from ALOS-2 raw data measured by the Japan Aerospace Exploration Agency
Additional file 1: Fig. S1. MAI analysis results. a Original MAI result. Note that the color scale f...
The ~30-km-long surface ruptures associated with the M w 7.0 (M j 7.3) earthquake at 01:25 JST on Ap...
Magma movements from reservoir toward the surface are responsible for volcanic unrest. Unrest can cu...
The 2016 Kumamoto earthquake involved a series of events culminating in an Mw 7.0 main shock on 2016...
Additional file 1: Figure A. Interferograms used in this study and identified linear surface rupture...
Additional file 3: Figure S3. Calculated density contrast model beneath Aso volcano in horizontal s...
Additional file 2: Figure S2. Calculated density contrast models beneath Aso volcano in horizontal s...
Additional file 5: Table S1. Inversion parameters for Additional file 2: Figure S2. Table S2. Invers...
Coseismic and postseismic crustal deformations caused by earthquake episodes are important in unders...
We resolve the density structure of a possible magma reservoir beneath Aso, an active volcano on Kyu...
I have been conducting a study of postseismic deformation following the 2016 Kumamoto earthquake usi...
The 2016 Kumamoto earthquake sequence occurred on the Futagawa–Hinagu fault zone near the Aso volcan...
Additional file 3: Figure S3. A comparison of observed crustal deformation (red arrows) with that ca...
Additional file 2: Figure S2. A comparison of observed crustal deformation (red arrows) with that ca...
Abstract Large earthquakes occurred in the central part of Kumamoto Prefecture on April 14–16, 2016,...
Additional file 1: Fig. S1. MAI analysis results. a Original MAI result. Note that the color scale f...
The ~30-km-long surface ruptures associated with the M w 7.0 (M j 7.3) earthquake at 01:25 JST on Ap...
Magma movements from reservoir toward the surface are responsible for volcanic unrest. Unrest can cu...
The 2016 Kumamoto earthquake involved a series of events culminating in an Mw 7.0 main shock on 2016...
Additional file 1: Figure A. Interferograms used in this study and identified linear surface rupture...
Additional file 3: Figure S3. Calculated density contrast model beneath Aso volcano in horizontal s...
Additional file 2: Figure S2. Calculated density contrast models beneath Aso volcano in horizontal s...
Additional file 5: Table S1. Inversion parameters for Additional file 2: Figure S2. Table S2. Invers...
Coseismic and postseismic crustal deformations caused by earthquake episodes are important in unders...
We resolve the density structure of a possible magma reservoir beneath Aso, an active volcano on Kyu...
I have been conducting a study of postseismic deformation following the 2016 Kumamoto earthquake usi...
The 2016 Kumamoto earthquake sequence occurred on the Futagawa–Hinagu fault zone near the Aso volcan...
Additional file 3: Figure S3. A comparison of observed crustal deformation (red arrows) with that ca...
Additional file 2: Figure S2. A comparison of observed crustal deformation (red arrows) with that ca...
Abstract Large earthquakes occurred in the central part of Kumamoto Prefecture on April 14–16, 2016,...
Additional file 1: Fig. S1. MAI analysis results. a Original MAI result. Note that the color scale f...
The ~30-km-long surface ruptures associated with the M w 7.0 (M j 7.3) earthquake at 01:25 JST on Ap...
Magma movements from reservoir toward the surface are responsible for volcanic unrest. Unrest can cu...