引文
[1]陈国光,计凤桔,周荣军,等.龙门山断裂带晚第四纪活动性分段的初步研究[J].地震地质,2007,29(3):657-673.Chen G G,Ji F J,Zhou R J,et al.Primary research of activity segmentation of Longmenshan fault zone since Late-Quaternary[J].Seismology and Gelology,2007,29(3):657-673.
[2]唐新功,胡文宝.龙门山断裂带地震时空分布规律探讨[J].长江大学学报:自然科学版理工,2012,9(6):21-23.Tang X G,Hu W B.Discussion on spatio-temporal distribution characters of earthquake on Longmenshan fault zone[J].Journal of Yangtze University:Nat Sci Edit Sci and Eng,2012,9(6):21-23.
[3]Dong S W,Zhang Y Q,Wu Z H,el al.Surface rupture and coseismic displacement produced by the Ms 8.0 Wenchuan earthquake o of May 12th,2008,Sichuan,China:Eastwards growth of the Qinghai-Tibet Plateau[J].Acta Geologica Sinica,2008,82(5):938-948.
[4]Xu Z Q,Ji S C,Li H B,et al.Uplift of the Longmenshan range and the Wenchuan earthquake[J].Episodes,2008,31(3):291-30l.
[5]徐锡伟,闻学泽,叶建青,等.汶川Ms 8.0地震地表破裂及其发震构造[J].地震地质,2008,30(3):597-629.Xu X W,Wen X Z,Ye J Q,et al.The Ms 8.0 Wenehuan earthquake surface ruptures and its seismogenic structure[J].Seismology and Geology,2008,30(3):597-629.
[6]Huang Y,Wu J P,Zhang T Z,et al.Relocation of the Ms 8.0 Wenchuan earthquake and its aftershock sequence[J].Science in China D:Earth Sciences,2008,51(12):1703-1711.
[7]黄润秋,李为乐.“5·12”汶川大地震触发地质灾害的发育分布规律研究[J].岩石力学与工程学报,2008,27(12):285-292.Huang R Q,Li W L.Research on development and distribution rules of geohazards induced by Wenchuan earthquake on 12th May,2008[J].Chinese Journal of Rock Mechanics and Engineering,2008,27(12):285-292.
[8]黄润秋.“5·12”汶川大地震地质灾害的基本特征及其对灾后重建影响的建议[J].中国地质教育,2008(2):21-24.Huang R Q.Characteristics of geological disasters of“5·12”Wenchuan earthquake and recommendation on its impact on reconstruction[J].Chinese Geological Education,2008(2):21-24.
[9]Parsons T,Chen J,Kirby E.Stress changes from the 2008 Wenchuan earthquake and increased hazard in the Sichuan basin[J].Nature,2008,454:509-510.
[10]陈晓利,邓俭良,冉洪流.汶川地震滑坡崩塌的空间分布特征[J].地震地质,2011,33(1):191-202.Chen X L,Deng J L,Ran H L.Analysis of landslides triggered by Wenchuan earthquake[J].Seismology and Geology,2011,33(1):191-202.
[11]王秀英,聂高众,马牧军.地震滑坡灾害评估中地震影响因素的联合应用[J].地震学报,2012,34(1):76-84.Wang X Y,Nie G Z,Ma M J.Application of multiple ground motion factors in earthquake-induced landslide hazard evaluation[J].Acta Seismologica Sinica,2012,34(1):76-84.
[12]陈正宜,魏成阶,魏永明,等.工程环境遥感应用[M].北京:煤炭工业出版社,1996.Chen Z Y,Wei C J,Wei Y M,et al.Remote Sensing Application of Engineering Environment[M].Beijing:China Coal Industry Press,1996.
[13]彭立,杨武年,黎小东,等.面向对象的地质灾害信息提取——以汶川地震为例[J].西南师范大学学报:自然科学版,2011,36(2):77-82.Peng L,Yang W N,Li X D,et al.Information extraction of geological hazards in an object oriented approach:A case study in Wenchuan earthquake[J].Journal of Southwest China Normal University:Natural Science Edition,2011,36(2):77-82.
[14]董金玉,杨国香,杨继红,等.汶川地震灾区滑坡的成因及典型实例分析[J].华北水利水电学院学报,2011,32(5):10-13.Dong J Y,Yang G X,Yang J H,et al.Analysis of causes and typical examples of the landslide in Wenchuan earthquake disaster area[J].Journal of North China Institute of Water Conservancy and Hydroelectric Power,2011,32(5):10-13.
[15]张雨霆,肖明,李玉婕.汶川地震对映秀湾水电站地下厂房的震害影响及动力响应分析[J].岩石力学与工程学报,2010,29(s2):3663-3671.Zhang Y T,Xiao M,Li Y J.Effect of Wenchuan earthquake on earthquake damage and dynamic response analysis of underground powerhouse of Yingxiuwan Hydropower Station[J].Chinese Journal of Rock Mechanics and Engineering,2010,29(s2):3663-3671.
[16]聂洪峰,童立强,李建存,等.基于遥感技术的“6·5”重庆武隆鸡尾山崩滑灾害特征及应急救援工程布置研究[J].国土资源遥感,2014,26(1):115-121.Nie H F,Tong L Q,Li J C,et al.Study on disaster characteristics and emergency rescue engineering for Jiweishan rockslide in Wulong,Chongqing,June 5,2009 using remote sensing technology[J].Remote Sensing for Land and Resources,2014,26(1):115-121.
[17]童立强,聂洪峰,李建存,等.喜马拉雅山地区大型泥石流遥感调查与发育特征研究[J].国土资源遥感,2013,25(4):104-112.Tong L Q,Nie H F,Li J C,et al.Large-scale debris flow survey and development study using remote sensing technology in the Himalayas,China[J].Remote Sensing for Land and Resources,2013,25(4):104-112.