Coseismic deformation of the 2022 Luding <italic>M</italic><sub>S</sub>6.8 earthquake and seismic potential along adjacent major faults

Author:

Shan Xinjian,Li Yanchuan,Gao Zhiyu,Hua Jun,Huang Xing,Gong Wenyu,Qu Chunyan,Zhao Dezheng,Chen Junxian,Huang Chuanchao,Zhang Yingfeng,Zhang Guohong

Publisher

Science China Press., Co. Ltd.

Subject

Multidisciplinary

Reference25 articles.

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2. Wang M, Shen Z K, Gan W J, et al. GPS continuous monitoring of the dynamic evolution of the deformation field of the Xianshuihe fault (in Chinese). Sci China Ser D Earth Sci, 2008, 38: 575–581 [王敏, 沈正康, 甘卫军, 等. GPS连续监测鲜水河断裂形变场动态演化. 中国科学D辑: 地球科学, 2008, 38: 575–581].

3. Wen X Z, Xu X W, Zheng R Z, et al. Average slip-rate and recent large earthquake ruptures along the Garze-Yushu fault (in Chinese). Sci China Ser D Earth Sci, 2003, (S1): 199–208 [闻学泽, 徐锡伟, 郑荣章, 等. 甘孜-玉树断裂的平均滑动速率与近代大地震破裂. 中国科学D辑: 地球科学, 2003, (S1): 199–208].

4. Wen X, Ma S, Xu X. Historical pattern and behavior of earthquake ruptures along the eastern boundary of the Sichuan-Yunnan faulted-block, southwestern China. Phys Earth Planet Inter, 2008, 168: 16-36.

5. Deng Q D, Cheng S P, Ma J, et al. Seismic activities and earthquake potential in the Tibetan Plateau (in Chinese). Chin J Geophys, 2014, 57: 2025–2042 [邓起东, 程绍平, 马冀, 等. 青藏高原地震活动特征及当前地震活动形势. 地球物理学报, 2014, 57: 2025–2042].

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