Estimation of coseismic surface displacement in the Aso-Caldera area caused by the 2016 Kumamoto Earthquake, with the Geomorphic Image Analysis using differential LiDAR DEM
After the main shock of 2016 Kumamoto Earthquake (Mj7.3), coseismic wide-area crustal deformation was observed around Aso region in Kumamoto Prefecture, Japan. In this study, multi-temporal LiDAR DEMs and Digital Geomorphic Image Matching method was applied to measure ground displacements of 1m scal...
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| Published in | Journal of the Japan society of photogrammetry and remote sensing Vol. 60; no. 5; pp. 248 - 251 |
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| Main Authors | , , |
| Format | Journal Article |
| Language | English Japanese |
| Published |
Tokyo
Japan Society of Photogrammetry and Remote Sensing
2021
Japan Science and Technology Agency |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0285-5844 1883-9061 |
| DOI | 10.4287/jsprs.60.248 |
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| Abstract | After the main shock of 2016 Kumamoto Earthquake (Mj7.3), coseismic wide-area crustal deformation was observed around Aso region in Kumamoto Prefecture, Japan. In this study, multi-temporal LiDAR DEMs and Digital Geomorphic Image Matching method was applied to measure ground displacements of 1m scale in wide-area.As a result, seismic wide-area crustal deformation around caldera and displacements along a lot of surface ruptures of the earthquake faults were observed. Additionally, large lateral slides of the area of 1-2km diameter were observed in the flat caldera floor filled with unconsolidated sediment. Amount of displacements of these area were 1-4m. |
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| AbstractList | After the main shock of 2016 Kumamoto Earthquake (Mj7.3), coseismic wide-area crustal deformation was observed around Aso region in Kumamoto Prefecture, Japan. In this study, multi-temporal LiDAR DEMs and Digital Geomorphic Image Matching method was applied to measure ground displacements of 1m scale in wide-area.As a result, seismic wide-area crustal deformation around caldera and displacements along a lot of surface ruptures of the earthquake faults were observed. Additionally, large lateral slides of the area of 1-2km diameter were observed in the flat caldera floor filled with unconsolidated sediment. Amount of displacements of these area were 1-4m. |
| Author | SATO, Takumi NISHIMURA, Tomohiro MUKOYAMA, Sakae |
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| Copyright | 2021 Japan Society of Photogrammetry and Remote Sensing Copyright Japan Science and Technology Agency 2021 |
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| References | 国土地理院，2016．平成28年熊本地震に関する情報，https://www.gsi.go.jp/BOUSAI/H27-kumamoto-earthquake-index.html#dd.」（2021年10月8日最終閲覧） 向山 栄・佐藤 匠・高見智之・西村智博，2017．2時期の航空レーザ計測地形データ解析による平成28年（2016年）熊本地震前後の阿蘇カルデラ地域における地表変位，2016年熊本・大分地震災害調査団報告書，日本応用地質学会・九州応用地質学会，pp. 55-63 Fujiwara et al., 2016. Small-displacement linear surface ruptures of the 2016 Kumamoto earthquake sequence detected by ALOS-2 SAR interferometry, Earth, Planets and Space (2016) 68 : 160 TSUJI, T. ISHIBASHI, J. ISHITSUKA, K. & KAMATA, R., 2017. Horizontal sliding of kilometer scale hot spring area during the 2016 Kumamoto earthquake, Scientific Reports 7, Article number : 42947 |
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| SubjectTerms | Calderas Diameters Digital imaging Displacement Earthquakes Geomorphology Image analysis Lidar |
| Title | Estimation of coseismic surface displacement in the Aso-Caldera area caused by the 2016 Kumamoto Earthquake, with the Geomorphic Image Analysis using differential LiDAR DEM |
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