Zobrazeno 1 - 10
of 43
pro vyhledávání: '"FURUYA, Gen"'
Autor:
Wang, Gonghui a, ⁎, Watanabe, Naoki b, Hoshikawa, Keisuke c, Furuya, Gen c, Cai, Fei d, Wu, Shengshan e
Publikováno v:
In Engineering Geology January 2023 312
Autor:
Wang, Gonghui a, ⁎, Zhang, Fanyu b, Furuya, Gen c, Hayashi, Koichi d, Hu, Wei e, McSaveney, Mauri e, f, Huang, Runqiu e
Publikováno v:
In Engineering Geology January 2021 280
Autor:
Wang, Gonghui a, ⁎, Furuya, Gen b, Zhang, Fanyu c, Doi, Issei a, Watanabe, Naoki d, Wakai, Akihiko e, Marui, Hideaki d
Publikováno v:
In Geomorphology 15 August 2016 267:48-58
Publikováno v:
In Engineering Geology 23 May 2014 174:36-45
Publikováno v:
京都大学防災研究所年報. A. 62:48-56
Numerous landslides were triggered by 2018 Hokkaido Eastern Iburi Earthquake on the tephra slopes, resulting in 36 casualties. Although one large landslide was initiated with its sliding surface being in the bedrock of sandstone and siltstone, most o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::903b0e0406f2d8a6dc799809cf975564
http://hdl.handle.net/2433/244887
http://hdl.handle.net/2433/244887
Autor:
Furuya, Gen a, ⁎, Suemine, Akira b, 1, Sassa, Kyoji c, Komatsubara, Takeshi d, Watanabe, Naoki e, Marui, Hideaki e
Publikováno v:
In Engineering Geology 2006 85(3):332-346
Publikováno v:
京都大学防災研究所年報. B. 56:237-241
The north-Kyushu heavy rainfall on July 2012 triggered severe shallow landsliding of hillslopes of caldera wall and volcanic central cones located in the Aso caldera area. The sliding materials are mainly tephra deposits with stratified structure cov
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::35676539c4b0c3e5160ef3492a1f08a5
http://hdl.handle.net/2433/181543
http://hdl.handle.net/2433/181543
Publikováno v:
京都大学防災研究所年報. B. 48:413-420
平成16 年7 月25 日に発生した台風10 号に伴って, 徳島県南部地域では7 月30 日から8 月2 日までの4日間で連続降雨量が2, 000mm を超過する記録的な豪雨が発生した。この豪雨により，徳島県
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::5ebfb46da19158903dbdb60b2a83f2e2
http://hdl.handle.net/2433/26522
http://hdl.handle.net/2433/26522
Publikováno v:
京都大学防災研究所年報. C. 47:183-192
結晶片岩の地すべり地において，地温探査，安定解析および水質分析結果から斜面崩壊と地下水脈の分布の関係について検討した。その結果，崩壊発生箇所は地下水脈の分布に関連する
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::3368c27574938a4f9146fc3cc3da6543
http://hdl.handle.net/2433/129007
http://hdl.handle.net/2433/129007
Autor:
Tiwari, Binod, Marui, Hideaki, Sato, Osamu, Yamagishi, Hiromitsu, Watanabe, Naoki, Furuya, Gen, Suzuki, Koji, Inaba, Kazunari, Shimura, Kazuo, Yamazaki, Fumiaki
Publikováno v:
新潟大学積雪地域災害研究センター研究年報. 23:63-76
Mount Usu is erupting frequently from 18th century. Comparing the recent eruptions, the property of the erupted materials have been found different in various eruption periods. The major eruption in 1978 had been concentrated in Mount Koushu and Moun
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::76c638d2763dec5a4034c30f80d47402
https://niigata-u.repo.nii.ac.jp/records/27996
https://niigata-u.repo.nii.ac.jp/records/27996