@techreport{oai:jaxa.repo.nii.ac.jp:00004565,
 author = {村上, 亮 and Briole, Pierre and Elias, Panagiotis and Guglielmino, Francesco and Puglisi, Giuseppe and Murakami, Makoto and Wegmuller, Urs},
 month = {},
 note = {We investigated the available ALOS/PALSAR data over two active areas in Europe: Etna volcano (Italy) and the western rift of Corinth (Greece). All data processing was performed at the National Observatory of Athens using the version 3.0 of ROI-PAC. At Etna the level of coherence of all interferograms is good, even for those with large baselines, in the rift of Corinth the level of coherence is in general less good than at Etna. One M=6.3 earthquake (June 8, 2008) and two M=5.3 (January 18 and 22, 2010) occurred in the western rift of Corinth during the investigated period, but no ground deformation was observed with PALSAR. In the case of the M=6.3 one the absence of ground deformation provides constraints on the depth of the fault, the two M=5.3 are too small for the L-band PALSAR-ALOS interferometry but they are visible with C-band ENVISAT-ASAR interferometry and with GPS. On Etna the sampled period was characterized by volcanic activity at the summit and shallow seismicity and creep along the Pernicana fault which is a major left-lateral strike slip structure located east-north-east of the volcano. The available C-band and L-band interferometry is combined with GPS and levelling data to model the ground deformation using. The tool used for merging the various ground deformation data is a new tool developed at INGV-Catania called SISTEM., 形態: カラー図版あり, 形態: DVD-ROM1枚, Physical characteristics: Original contains color illustrations, Note: One DVD-ROM, 資料番号: AA0065135095, レポート番号: JAXA-SP-11-007E},
 title = {GEOMORPHOLOGY AND GEOMORPHOLOGICAL CHANGES AT VOLCANOES AND ACTIVE FAULTS OBSERVED WITH ALOS. FUSION WITH OTHER REMOTE SENSING AND GROUND DATA. APPLICATION TO NATURAL DISASTER MONITORING},
 year = {2011}
}