| 松原市扶余北断裂的发现及活动性鉴定 |
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| 引用本文： | 万永魁,沈军,刘峡,尉洋,于晓辉,王雷,邵博.松原市扶余北断裂的发现及活动性鉴定[J].中国地震,2016,32(3):477-484. |
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| 作者姓名： | 万永魁 沈军 刘峡 尉洋 于晓辉 王雷 邵博 |
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| 作者单位： | 防灾科技学院, 河北省三河燕郊开发区学院街 065201;中国地震局第一监测中心, 天津市河东区耐火路7号 300180,防灾科技学院, 河北省三河燕郊开发区学院街 065201,中国地震局第一监测中心, 天津市河东区耐火路7号 300180,中国地震局兰州地震研究所, 兰州 730000,防灾科技学院, 河北省三河燕郊开发区学院街 065201,防灾科技学院, 河北省三河燕郊开发区学院街 065201,防灾科技学院, 河北省三河燕郊开发区学院街 065201 |
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| 基金项目： | 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 |
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| 摘 要： | 通过对3D及大量2D石油勘探资料的精细解释,发现并确认了位于松原市主城区北侧、距主城区仅10km处的扶余北断裂。该断裂是扶余隆起的北部边界,走向近EW,全长26km,西起孙家围子,向东延伸至大洼镇附近;断层倾向南,视倾角较陡,约60°~80°,早白垩纪为正断层,新构造运动以来表现为逆冲作用。利用浅层人工地震勘探、钻探、释光测年等多重组合方式对扶余北断裂的活动性作了鉴定,结果表明,扶余北断裂最新活动距今(23.9±0.6)ka~(28.9±0.6)ka,为晚更新世活动断裂,断裂活动造成第四系底界位错2.5m,中晚更新世地层存在明显扰动。
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| 关 键 词： | 松原 扶余北断裂 活动性鉴定 |
| 收稿时间： | 2015/5/7 0:00:00 |
| 修稿时间： | 2016/9/19 0:00:00 |
The discovery and identification of activities of the Fuyubei fault in Songyuan |
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| Wan Yongkui,Shen Jun,Liu Xi,Yu Yang,Yu Xiaohui,Wang Lei and Shao Bo.The discovery and identification of activities of the Fuyubei fault in Songyuan[J].Earthquake Research in China,2016,32(3):477-484. |
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| Authors: | Wan Yongkui Shen Jun Liu Xi Yu Yang Yu Xiaohui Wang Lei and Shao Bo |
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| Institution: | Institute of Disaster Prevention, Sanhe 065201, Hebei, China;First Crust Deformation Monitoring and Application Center, CEA, Tianjin 300180, China,Institute of Disaster Prevention, Sanhe 065201, Hebei, China,First Crust Deformation Monitoring and Application Center, CEA, Tianjin 300180, China,Lanzhou Institute of Seismology, CEA, Lanzhou 730000, China,Institute of Disaster Prevention, Sanhe 065201, Hebei, China,Institute of Disaster Prevention, Sanhe 065201, Hebei, China and Institute of Disaster Prevention, Sanhe 065201, Hebei, China |
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| Abstract: | 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 10km away in the north of the city. The Fuyubei fault is northern boundary of the Fuyu uplift with the total length 26km,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. |
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| Keywords: | Songyuan Fuyubei Fault Identification of fault activity |
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