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《Seismology and Geology》 2012-02
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WEI Zhan-yu1) HE Hong-lin1) SHI Feng1) XU Yue-ren1,2) BI Li-si3) SUN Hao-yue1) 1)Key Laboratory of Active Tectonics and Volcano,Institute of Geology, China Earthquake Administration, Beijing 100029,China 2)Institute of Earthquake Science,China Earthquake Administration,Beijing 100036,China 3)Guangdong Earthquake Administration,Guangzhou 510700,China  
Daliangshan Fault zone constitutes an important part of the eastern boundary of Sichuan-yunnan active block. The studies of slip rate along the fault is not only significant to the crust movement and deformation pattern on the southeast edge of Tibetan Plateau,but also has great value in seismic hazard assessment and mid- and long-term forecasting of earthquake of the Daliangshan region. Through detailed field work along the south segment of Daliangshan Fault zone,namely the Butuo Fault and the Jiaojihe Fault,and based on accurate RTK(GPS)survey for the alluvial fans and activity dating,we suggest that left-lateral slip rate of the south segment of the fault zone is between 2.5~4.5mm/a,and the slip rate of Jiaojihe Fault is slightly higher than that of the Butuo Fault. Due to partitioning of part of the strike-slip component on the Daliangshan Fault zone,there is an obvious deficit in the displacement and slip rate on the Anninghe-Zemuhe Fault,compared to the Xianshuihe and Xiaojiang Faults. Comparing to the slip rates between Daliangshan Fault and Anninghe-Zemuhe Fault,it is found that they have similar horizontal slip rate,indicating the seismicity level of the Daliangshan Fault will not be lower than that of Anninghe-Zemuhe Fault. As the Daliangshan Fault gradually replaces the role of Anninghe-Zemuhe Fault in the Xianshuihe-Xiaojiang Fault system,the seismicity on the Daliangshan Fault zone will increase,and the Dalianghan region will have a higher risk of earthquake damage.
【Fund】: 财政部重大专项“我国地震重点监视防御区活动断层地震危险性评价”项目(201108001)
【CateGory Index】: P315.2
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