| Item type |
テクニカルレポート / Technical Report(1) |
| 公開日 |
2015-03-26 |
| タイトル |
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タイトル |
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 |
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言語 |
en |
| 言語 |
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言語 |
eng |
| 資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_18gh |
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資源タイプ |
technical report |
| 著者 |
村上, 亮
Briole, Pierre
Elias, Panagiotis
Guglielmino, Francesco
Puglisi, Giuseppe
Murakami, Makoto
Wegmuller, Urs
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| 著者所属 |
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北海道大学地震火山観測研究センター |
| 著者所属（英） |
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en |
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UMR 7538,Laboratoire de Geologie, Ecole Normale Superieure, CNRS |
| 著者所属（英） |
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en |
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Institute for Space Applications and Remote Sensing, National Observatory of Athens |
| 著者所属（英） |
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en |
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Osservatorio Etneo, Istituto Nazionale di Geofisica e Vulcanologi |
| 著者所属（英） |
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en |
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Osservatorio Etneo, Istituto Nazionale di Geofisica e Vulcanologi |
| 著者所属（英） |
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en |
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Institute of Seismology and Volcanology, Hokkaido University |
| 著者所属（英） |
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en |
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GAMMA Remote Sensing |
| 出版者 |
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出版者 |
宇宙航空研究開発機構地球観測研究センター (JAXA)(EORC) |
| 出版者（英） |
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出版者 |
Earth Observation Research Center, Japan Aerospace Exploration Agency (JAXA)(EORC) |
| 書誌情報 |
宇宙航空研究開発機構特別資料
en : JAXA Special Publication: Final Reports of the ALOS Research Announcement Programs 1&2, 2011
巻 JAXA-SP-11-007E,
p. PI167-1-PI167-6,
発行日 2011
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| 抄録（英） |
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内容記述タイプ |
Other |
|
内容記述 |
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. |
| 内容記述 |
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内容記述タイプ |
Other |
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内容記述 |
形態: カラー図版あり |
| 内容記述 |
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内容記述タイプ |
Other |
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内容記述 |
形態: DVD-ROM1枚 |
| 内容記述（英） |
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内容記述タイプ |
Other |
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内容記述 |
Physical characteristics: Original contains color illustrations |
| 内容記述（英） |
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内容記述タイプ |
Other |
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内容記述 |
Note: One DVD-ROM |
| ISSN |
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収録物識別子タイプ |
ISSN |
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収録物識別子 |
1349-113X |
| 書誌レコードID |
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収録物識別子タイプ |
NCID |
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収録物識別子 |
AA11984031 |
| 資料番号 |
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内容記述タイプ |
Other |
|
内容記述 |
資料番号: AA0065135095 |
| レポート番号 |
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内容記述タイプ |
Other |
|
内容記述 |
レポート番号: JAXA-SP-11-007E |
65135095.pdf (1.5 MB)
