[1] Guo Xiaojun*, Li Yong, Cui Peng, Yan Hua, Zhuang Jianqi. 2020. Intermittent viscous debris flow formation in Jiangjia Gully from the perspectives of hydrological processes and material supply.Journal of Hydrology, 589: 125184.
[2] Guo Xiaojun, Cui Peng*, Li Yong, Ma Li, Ge Yonggang, William B. Mahoney. 2016. Intensity-duration threshold of rainfall-triggered debris flows in the Wenchuan Earthquake affected area, China.Geomorphology, 253: 208-216.
[3] Guo Xiaojun, Cui Peng*, Li Yong, Zou Qiang, Kong Yingde. 2016. The formation and development of debris flows in large watersheds after the 2008 Wenchuan Earthquake.Landslides, 13(1): 116-125.
[4] Guo Xiaojun, Cui Peng*, Li Yong, Zhang Jianqiang, Ma Li, William B. Mahoney. 2016. Spatial distribution of debris flows and responsible rainfall threshold in the Wenchuan earthquake area.Landslides, 13(5): 1215-1229.
[5] Guo Xiaojun*, Cui Peng, Li Yong, Fan Jianglin, Yan Yan, Ge Yonggang. 2016. Temporal differentiation of rainfall thresholds for debris flows in Wenchuan earthquake-affected areas,Environmental Earth Sciences, 75(2): 109-121.
[6] Guo Xiaojun,Cui Peng, Lorenzo Marchi, Ge Yonggang*. 2017. Characteristics of rainfall responsible for debris flows in Wenchuan Earthquake area.Environmental Earth Sciences, 2017, 76: 596-605.
[7] Guo Xiaojun, Li Yong*, Cui Peng, Zhao Wanyu, Jiang Xingyuan, Yan Yan. 2016. Discontinuous slope failures and pore-water pressure variation.Journal of Mountain Science, 13(1): 116-125.
[8] Guo Xiaojun; Cui Peng*; Li Yong; Liu Jinfeng; Ge Yonggang; Wang Cide; Evaluation of a traditional method for peak flow discharge estimation for floods in the Wenchuan Earthquake area, Sichuan Province, China.Journal of Mountain Science, 2019, 16(3): 641-656.
[9] Guo Xiaojun,Cui Peng*, Li Yong. 2013. Debris flow warning threshold based on antecedent rainfall:a case study in Jiangjia Ravine, Yunnan, China.Journal of Mountain Science, 10(2): 305–314
[10] Cui Peng,Guo Xiaojun*, Yan Yan, Li Yong, Ge Yonggang. 2018. Real-time observation of an active debris flow watershed in the Wenchuan Earthquake area.Geomorphology, 321: 153-166. |