Crustal Deformation Observed by Synthetic Aperture Radar (SAR)
Released:2011.04.25 Japanese
Crustal Deformation by InSAR
A M=7.0 (JMA) earthquake occurred in Fukushima Hamadori Region, Japan on April 11, 2011 (UTC). An interferometric analysis of the data acquired by the Phased Array type L-band Synthetic Aperture Radar (PALSAR) onboard the Advanced Land Observing Satellite (ALOS) allows us to clarify spatial distribution of surface deformation associated with the earthquake.
The interferogram shows clear displacement discontinuities along Idosawa fault and Yunotake fault.
The interferogram shows clear displacement discontinuities along Idosawa fault and Yunotake fault.
Interferogram
Fukushima Hamadori, Japan Earthquake
| Date-Time | April 11, 2011 17:16 (Local Time), April 11, 2011 08:16 (UTC) |
| Hypocenter Location | 36.94567°N, 140.67267°E Depth:6.4 km (JMA, as of 2011-04-25)
37.007°N, 140.477°E Depth:10 km (USGS, as of 2011-04-25) |
| Magnitude | 7.0 (JMA, as of 2011-04-25)
6.6 (USGS, as of 2011-04-25) |
Satellite and Sensor
PALSAR sensor onboard "Daichi" (ALOS) satellite launched by Japan Aerospace Exploration Agency on January 24, 2006
Paper, Report, Presentation
Under preparation
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