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《Earthquake Research in China》 2016-03
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The discovery and identification of activities of the Fuyubei fault in Songyuan

Wan Yongkui;Shen Jun;Liu Xia;Yu Yang;Yu Xiaohui;Wang Lei;Shao Bo;Institute of Disaster Prevention;First Crust Deformation Monitoring and Application Center,CEA;Lanzhou Institute of Seismology,CEA;  
Based on 3D and a large number of 2D oil seismic exploration data,the paper discovered and identified the Fuyubei fault in Songyuan which is only 10 km away in the north of the city. The Fuyubei fault is northern boundary of the Fuyu uplift with the total length 26 km,in the direction of near EW. The fault starts in the west of Sunjiaweizi and extends to the east of Dawa town. The fault has an apparent sharp dip of 60°-80° and the main fault is an early Cretaceous layer and serves as a thrust since the new tectonic movement. Shallow artificial seismic,drilling,optical stimulated luminescence dating and other ways were used to study the Fuyubei fault activities. The results show that the latest active period was at( 23.9±0.6) ka-( 28.9±0.6) ka ago.It reveals the Fuyubei fault is a concealed active fault of late Pleistocene. The Quaternary strata dislocation by fault activities is 2.5m and there is an obvious disturbance in the middle-late strata of Pleistocene series.
【Fund】: 中国地震局教师科研基金项目(20120101);; 国家自然科学基金项目(41372216);; 国家国际科技合作专项项目(2012DFR20440);; 中央高校基本科研业务费专项资金创新团队资助计划项目“我国地震重点监视防御区活动断层地震危险性评价-松原市活断层探测与地震危险性评价”联合资助
【CateGory Index】: P315
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