Long-term Activity of Earthquake-induced Landslides： A Case Study from Qionghai Lake basin, Southwest of China
Earthquake-triggered landslides are a major geological hazard in the eastern Tibetan Plateau, and have prolonged impact on earth surface processes and fluvial system. To determine how long co-seismic landslides affect basins, a massive number of landslides existing in Qionghai Lake Basin were invest...
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| Veröffentlicht in: | Journal of mountain science 2014-05, Vol.11 (3), p.607-624 |
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| creator | Wei, Xue-li Chen, Ning-sheng Cheng, Qian-gong He, Na Deng, Ming-feng Tanoli, Javed Iqbal |
| description | Earthquake-triggered landslides are a major geological hazard in the eastern Tibetan Plateau, and have prolonged impact on earth surface processes and fluvial system. To determine how long co-seismic landslides affect basins, a massive number of landslides existing in Qionghai Lake Basin were investigated for landslide distribution characteristics and geomorphological evidences, with further comparison and analysis using historic seismic analog method. The landslides found in Qionghai Lake Basin showed clear features of seismic triggering with strongly controlled by Zemuhe fault. These landslides are still active at present. Some new slides generally occur in ancient slope failure zones causing serious secondary hazards in recent years. In this study we strengthen the idea that the landslides triggered by the 185o Xichang earthquake （Ms7.5） have long term activity and prolonged impact on the mountain disasters with a period of more than 16o years. Our results support growing evidence that coseismic landslides have a prolonged effect on secondary disasters in a basin, and invite more careful consideration of the relationship between current basin condition and landslide history for a longer period. |
| doi_str_mv | 10.1007/s11629-013-2970-4 |
| format | Article |
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To determine how long co-seismic landslides affect basins, a massive number of landslides existing in Qionghai Lake Basin were investigated for landslide distribution characteristics and geomorphological evidences, with further comparison and analysis using historic seismic analog method. The landslides found in Qionghai Lake Basin showed clear features of seismic triggering with strongly controlled by Zemuhe fault. These landslides are still active at present. Some new slides generally occur in ancient slope failure zones causing serious secondary hazards in recent years. In this study we strengthen the idea that the landslides triggered by the 185o Xichang earthquake （Ms7.5） have long term activity and prolonged impact on the mountain disasters with a period of more than 16o years. Our results support growing evidence that coseismic landslides have a prolonged effect on secondary disasters in a basin, and invite more careful consideration of the relationship between current basin condition and landslide history for a longer period.</description><identifier>ISSN: 1672-6316</identifier><identifier>EISSN: 1993-0321</identifier><identifier>EISSN: 1008-2786</identifier><identifier>DOI: 10.1007/s11629-013-2970-4</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Earthquakes ; Ecology ; Environment ; Geography ; Geological hazards ; Geomorphology ; Lake basins ; Lakes ; Landslides ; Landslides & mudslides ; Seismic activity ; Seismology ; Slope stability ; 中国西南 ; 地质灾害 ; 地震模拟 ; 山体滑坡 ; 引发 ; 次生灾害 ; 邛海流域 ; 青藏高原东部</subject><ispartof>Journal of mountain science, 2014-05, Vol.11 (3), p.607-624</ispartof><rights>Science Press, Institute of Mountain Hazards and Environment, CAS and Springer-Verlag Berlin Heidelberg 2014</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c376t-3fe6a1061b1bb8568d3023dd873ddb28ce4a5f29a29589318a1ba894ed4f8d403</citedby><cites>FETCH-LOGICAL-c376t-3fe6a1061b1bb8568d3023dd873ddb28ce4a5f29a29589318a1ba894ed4f8d403</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/87799X/87799X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11629-013-2970-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11629-013-2970-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Wei, Xue-li</creatorcontrib><creatorcontrib>Chen, Ning-sheng</creatorcontrib><creatorcontrib>Cheng, Qian-gong</creatorcontrib><creatorcontrib>He, Na</creatorcontrib><creatorcontrib>Deng, Ming-feng</creatorcontrib><creatorcontrib>Tanoli, Javed Iqbal</creatorcontrib><title>Long-term Activity of Earthquake-induced Landslides： A Case Study from Qionghai Lake basin, Southwest of China</title><title>Journal of mountain science</title><addtitle>J. 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In this study we strengthen the idea that the landslides triggered by the 185o Xichang earthquake （Ms7.5） have long term activity and prolonged impact on the mountain disasters with a period of more than 16o years. Our results support growing evidence that coseismic landslides have a prolonged effect on secondary disasters in a basin, and invite more careful consideration of the relationship between current basin condition and landslide history for a longer period.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Ecology</subject><subject>Environment</subject><subject>Geography</subject><subject>Geological hazards</subject><subject>Geomorphology</subject><subject>Lake basins</subject><subject>Lakes</subject><subject>Landslides</subject><subject>Landslides & mudslides</subject><subject>Seismic activity</subject><subject>Seismology</subject><subject>Slope stability</subject><subject>中国西南</subject><subject>地质灾害</subject><subject>地震模拟</subject><subject>山体滑坡</subject><subject>引发</subject><subject>次生灾害</subject><subject>邛海流域</subject><subject>青藏高原东部</subject><issn>1672-6316</issn><issn>1993-0321</issn><issn>1008-2786</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kcFOGzEQhi3USkDgAbhZcOFQg8f2eu1jFKW0UqSqopwt79rLGpLdxN5tlVfhWXgnXgFHQQhx6GVmDv__zWh-hM6AXgGl5XUCkEwTCpwwXVIiDtARaM0J5Qy-5FmWjEgO8hAdp_RAqSy1giO0XvTdPRl8XOFpPYS_YdjivsFzG4d2M9pHT0Lnxto7vLCdS8vgfHp5fsJTPLPJ49thdFvcxH6Ff4dMam3IwkePK5tC9w3f9uPQ_vNp2EFnbejsCfra2GXyp299gu6-z__MfpDFr5ufs-mC1LyUA-GNlxaohAqqShVSOU4Zd06VuVRM1V7YomHaMl0ozUFZqKzSwjvRKCcon6DLPXcd-82YLzCrkGq_XNrO92MyUIhSScbyxybo4pP0oR9jl6_LKiY4U6zYAWGvqmOfUvSNWcewsnFrgJpdBmafgclEs8vAiOxhe0_K2u7exw_k_5jO3xa1-aOb7HvfJCVoRgWn_BXQ-5Ut</recordid><startdate>20140501</startdate><enddate>20140501</enddate><creator>Wei, Xue-li</creator><creator>Chen, Ning-sheng</creator><creator>Cheng, Qian-gong</creator><creator>He, Na</creator><creator>Deng, Ming-feng</creator><creator>Tanoli, Javed Iqbal</creator><general>Science Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>SOI</scope><scope>7TG</scope><scope>KL.</scope></search><sort><creationdate>20140501</creationdate><title>Long-term Activity of Earthquake-induced Landslides： A Case Study from Qionghai Lake basin, Southwest of China</title><author>Wei, Xue-li ; 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Some new slides generally occur in ancient slope failure zones causing serious secondary hazards in recent years. In this study we strengthen the idea that the landslides triggered by the 185o Xichang earthquake （Ms7.5） have long term activity and prolonged impact on the mountain disasters with a period of more than 16o years. Our results support growing evidence that coseismic landslides have a prolonged effect on secondary disasters in a basin, and invite more careful consideration of the relationship between current basin condition and landslide history for a longer period.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11629-013-2970-4</doi><tpages>18</tpages></addata></record> |
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| identifier | ISSN: 1672-6316 |
| ispartof | Journal of mountain science, 2014-05, Vol.11 (3), p.607-624 |
| issn | 1672-6316 1993-0321 1008-2786 |
| language | eng |
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| source | Springer Nature - Complete Springer Journals; Alma/SFX Local Collection |
| subjects | Earth and Environmental Science Earth Sciences Earthquakes Ecology Environment Geography Geological hazards Geomorphology Lake basins Lakes Landslides Landslides & mudslides Seismic activity Seismology Slope stability 中国西南 地质灾害 地震模拟 山体滑坡 引发 次生灾害 邛海流域 青藏高原东部 |
| title | Long-term Activity of Earthquake-induced Landslides： A Case Study from Qionghai Lake basin, Southwest of China |
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