1The 2008 Wenchuan, 2013 Lushan and 2017 Jiuzhaigou earthquakes, Sichuan, in the last more than one thousand years of rupture history of the eastern margin of the Bayan Har blockWen Xueze255-2672Are there links between the localized deformation in the northeastern section of Wenchuan earthquake source zone and the May 25, 2008 Qingchuan strong aftershock?Ni Sidao, Zhou Yong, Qian Yunyi, Luo Xinyu, Wang Xiangteng268-2783Seismogenic mechanism and the intermediate-and long-term earthquake risks of the 2008 Wenchuan and 2013 Lushan earthquakesLin Banghui, Chen Zu'an, Bai Wuming, Cheng Xu279-2904Triggering relationship in strong earthquake sequence around the Bayan Har block and its tectonic significance based on Coulomb stress changes and seismicityJia Ke, Zhou Shiyong291-3035Discussion on the largest aftershock of the Wenchuan aftershock sequenceXie Mengyu, Shi Baoping304-3156Aftershock rate decay induced by postseismic creep: A case study from the Mw7.9 Wenchuan earthquake sequenceXie Mengyu, Shi Baoping, Lin Luchun316-3317Geomorphic formation and crustal stress evolution mechanism in the Longmenshan fault zone and its adjacent regionsShi Haoyu, Ma Nianjie332-3408Crustal isostasy model and strong earthquakes in the Tibetan Plateau and its surroundingsSun Shaobo, Chen Shi, Gong Lizhuo, Xu Weimin341-3509Abnormal signals of geoelectric field related to Wenchuan Ms8.0 earthquake recorded at the Chengdu stationMa Qinzhong351-36310Determination of the surface-wave magnitude of the Wenchuan earthquake and its seismic Doppler effectLiu Ruifeng, Zou Liye, Zhang Liwen364-37311Parameter estimation of ground-motion prediction model in Longmenshan region based on strong motion dataFu Lei, Li Xiaojun, Rong Mianshui, Chen Su, Zhou Yue374-38612Real-time estimation of rupture length of earthquake source based on records of strong motion arrayLiu Chen, Li Xiaojun, Jing Bingbing387-39813@@后插114@@后插215@@前插1 