[1]
Liu Chuanzheng, Liu Yanhui, Lian Jianfa. Study on Genetic Mechanism of the Badong Slope System in the Three Gorges of the Yangtze River [J]. Geological review.2006,52(4).
Google Scholar
[2]
Chang Zhonghua, Wu Faquan, Zhang Eryong, etc. Deformation and failure modes and genetic mechanisms of typical rocky slopes in Fengjie County, Three Gorges reservoir region [J]. Journal of Chinese geological disaster prevention and control. 2004, 15 (4).
Google Scholar
[3]
Li Hualiang, Yi Shunhua, Deng Qinglu. Development characteristics and their spatial variations of Badong formation in the Three Gorges reservoir region [J]. Journal of Engineering Geology.2006,14(5).
Google Scholar
[4]
Zhang Jiagui. Features and Genesis of Large Complex Landslide Developed from 3rd Member of Badong Formation in the Newly Built Wushan County Seat, Three Gorges Reservoir Region [J]. Journal of the Earth.2001,22(2).
Google Scholar
[5]
Wang Zhihua. The primary investigation of landslide distributional characteristics and developmental rule at middle-ahead sectional towns in the Three Gorges reservoir area [R]. The fifth national prevention of geological disasters academic conference.
Google Scholar
[6]
Chai Bo, Yin Kunlong, Jian Wenxing, Dai Yunxia. Deep stability analysis of typical reservoir bank in Badong county [J]. Geotechnical Mechanics.2008,28(supplement).
Google Scholar
[7]
Chang Zhonghua, Wu Faquan, Liu Haiyan, Qi Shengwen. Bank slope types and rock mass structural features in new Fengjie county Three Gorges reservoir region [J]. Rock Mechanics and Engineering Journal.2005,24(17).
Google Scholar
[8]
Luo Yuanhua,Wu Faquan,Chang Zhonghua. Phenomenology research on deformation and failure modes of slopes composed of argillaceous limestone of the third number of Badong group (T2b3) in new site of Fengjie county of Three Gorges reservoir area [J]. Rock Mechanics and Engineering Journal.2005,24(12).
Google Scholar
[9]
Qi Shengwen, Wu Faquan, Chang Zhonghua, Liu Haiyan,Si Weibing. Mechanism and model for deformation of bank slope with slightly inclined soil layers in Fengjie County of Three Gorges [J]. Journal of Geotechnical Engineering.2006,28(1).
Google Scholar
[10]
Liu Chuanzheng. The study on development process of slope in the connected part between Chuan and Xia rivers in Changjiang river [J]. Journal of Chinese geological disaster prevention and control.2000,11(1).
Google Scholar
[11]
Liu Chuanzheng. The geological disasters in the Three Gorges reservoir area [J]. Geotechnical Engineering World.6(6).
Google Scholar
[12]
Lu Haifeng. Research on Engineering Characteristics and Failure Mechanism of Badong Formation Soft Rock Slope [D]. Ph.D. Thesis of Graduate University of Chinese Academy of Sciences.2010.5.
Google Scholar
[13]
Yin Yueping,Zhang Jiagui,Chen Baosun,Kang Hongda. Formation mechanism of large-scale loose sediment at the relocation sites of Wushan county on the Three Gorges [J].
Google Scholar
[14]
Sun Guangzhong. Rock mass structure mechanics [M]. Science Press.1988.
Google Scholar
[15]
Xiao Yongjun, Yin Kunlong, Huang Xuebing, Xu Kaixiang. Weak intercalated layers' geologic feature in deep-seated rock mass of Baitupo slope in Badong new town-site of the Three Gorges reservoir [J]. Hydrogeology and Engineering Geology.2007, (6).
Google Scholar
[16]
Chai Bo,Yin Kunlong. Interlayer weakness zones in Badong formation of middle Triassic forming bank slopes of Three Gorges reservoir in new Badong county [J]. Journal of Engineering Geology.2009, 17(6).
Google Scholar
