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Ma Zhixia, Zhang Guohong, Chen Xugeng, Zhao Guocun, Ding Rui, Li Guangchen. 2018: Shallow structural characteristics and spatial distribution of Xiadian fault
by shallow seismic reflection method. Acta Seismologica Sinica, 40(4): 399-410. DOI: 10.11939/jass.20170166
Citation: Ma Zhixia, Zhang Guohong, Chen Xugeng, Zhao Guocun, Ding Rui, Li Guangchen. 2018: Shallow structural characteristics and spatial distribution of Xiadian fault
by shallow seismic reflection method. Acta Seismologica Sinica, 40(4): 399-410. DOI: 10.11939/jass.20170166
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Shallow structural characteristics and spatial distribution of Xiadian fault
by shallow seismic reflection method

  • Institute of Crustal Dynamics，China Earthquake Administration，Beijing 100085，China

More Information
  • Received Date: August 23, 2017
  • Revised Date: February 03, 2018
  • Available Online: July 25, 2018
  • Published Date: June 30, 2018
    Graphical Abstract
    • Abstract
  • In order to further study the seismogenic structure and activity of Xiadian fault, the shallow seismic exploration is carried out in the epicenter of Xiadian fault with the seismic exploration lines of small trace interval and high density; and the seismic reflection profiles are comprehensively interpreted. The seismic exploration lines are laied toward both sides with Pangezhuang as center. There are 12 seismic exploration lines with a total length of about 18 km. Field data acquisition geometry is intermediate excitation and bilateral asymmetric reception with no less than 12 full coverages. Through the normal and fine processing, the reflected wave stacking time sections are acquired, revealing the wave group variation characteristics and the clear fracture features. Xiadian fault is interpreted as normal fault with dip SE, apparent dip angle about 72°. Meanwhile, the stacked time sections also show the shallow structural characteristics and distribution of Xiadian fault from Xiaoshigezhuang to Nanzhangdai, about 20 km long. The fault strike is about N40°E in exploration line scope. Therefore, it is inferred that Xiadian fault is a Holocene active fault according to the microtopographic survey and previous research findings. As for the center section of Xiadian fault, secondary fault develop and diffracted waves appear obviously, and weaken toward the two sides, which is coincident with the distribution of fault scarp and continuous elevation changes, verifying that the epicenter was located near Pangezhuang, Xiadian town. The spatial distribution of Xiadian fault and the strata structure features revealed by exploration agree well with geological data.
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  • 高景华, 徐明才, 荣立新, 柴铭涛, 王广科, 王小江, 刘冠军. 2008. 利用地震剖面研究夏垫断裂西南段的活动性[J]. 地震地质, 30（2）: 497-504.
    Gao J H, Xu M C, Rong L X, Chai M T, Wang G K, Wang X J, Liu G J. 2008. Activity of the southwest segment of Xiadian fault investigated by seismic reflection profiling[J]. Seismology and Geology, 30（2）: 497–504 （in Chinese）.
    高文学, 马瑾. 1993. 首都圈地震地质环境与地震灾害[M]. 北京: 地震出版社: 1–452.
    Gao W X, Ma J. 1993. Seismo-Geological Background and Earthquake Hazard in Beijing Area[M]. Beijing: Seismological Press: 1–452 （in Chinese）.
    高战武. 2001. 张家口—蓬莱断裂带地震地质特征研究[D]. 北京: 中国地震局地质研究所: 1–130.
    Gao Z W. 2001. A Study on Characteristics of Earthquake Geology of the Zhangjiakou-Penglai Fault Zone[D]. Beijing: Institute of Geology, China Earthquake Administration: 1–130 （in Chinese）.
    江娃利, 侯治华, 肖振敏, 谢新生. 2000. 北京平原夏垫断裂齐心庄探槽古地震事件分析[J]. 地震地质, 22（4）: 413-422.
    Jiang W L, Hou Z H, Xiao Z M, Xie X S. 2000. Study on paleoearthquakes of Qixinzhuang trench at the Xiadian fault, Beijing plain[J]. Seismology and Geology, 22（4）: 413-422 （in Chinese）.
    李善明. 1987. 北京平原区钻孔柱状图图集[M]. 北京: 北京市地震地质会战办公室: 1–333.
    Li S M. 1987. Atlas of Borehole Histograms in Beijing Plain[M]. Beijing: Beijing Seismological Geology Office: 1–333 （in Chinese）.
    刘保金, 张先康, 陈颙, 酆少英, 姬计法, 袁洪克, 左莹. 2011. 三河—平谷8.0级地震区地壳结构和活动断裂研究—利用单次覆盖深反射和浅层地震剖面[J]. 地球物理学报, 54（5）: 1251-1259.
    Liu B J, Zhang X K, Chen Y, Feng S Y, Ji J F, Yuan H K, Zuo Y. 2011. Research on crustal structure and active fault in the Sanhe-Pinggu earthquake （M8.0） zone based on single-fold deep seismic reflection and shallow seismic reflection profiling[J]. Chinese Journal of Geophysics, 54（5）: 1251-1259 （in Chinese）.
    毛昌伟, 丁锐, 龚正, 张世民. 2010. 1679年三河—平谷8级地震地表断层陡坎的GPS测量[G]//地壳构造与地壳应力文集, 22卷. 北京: 中国地震局地壳应力研究所: 11–18.
    Mao C W, Ding R, Gong Z, Zhang S M. 2010. GPS survey of the surface fault scarp of 1679 Sanhe-Pinggu M8 earth-quake[G]//Bulletin of the Institute of Crustal Dynamics, Vol. 22. Beijing: Institute of Crustal Dynamics, China Earthquake Administration: 11–18 （in Chinese）.
    孟宪梁, 杜春涛, 王瑞, 刘士平. 1983. 1679年三河—平谷大震的地震断裂带[J]. 地震, （3）: 18-23.
    Meng X L, Du C T, Wang R, Liu S P. 1983. The earthquake fault zone in 1679 Sanhe-Pinggu great earthquke[J]. Earthquake, （3）: 18-23 （in Chinese）.
    彭一民, 李鼎容, 谢振钊, 王安德, 刘清泗. 1981. 北京平原区同生断裂的某些特征及其研究意义[J]. 地震地质, 3（2）: 57-64.
    Peng Y M, Li D R, Xie Z Z, Wang A D, Liu Q S. 1981. Some features of contemporaneous faults in Beijing plain and their significance[J]. Seismology and Geology, 3（2）: 57-64 （in Chinese）.
    冉勇康, 邓起东, 杨晓平, 张晚霞, 李如成, 向宏发. 1997. 1679年三河—平谷8级地震发震断层的古地震及其重复间隔[J]. 地震地质, 19（3）: 193-201.
    Ran Y K, Deng Q D, Yang X P, Zhang W X, Li R C, Xiang H F. 1997. Paleoearthquakes and recurrence interval on the seismogenic fault of 1679 Sanhe-Pinggu M8 earthquake, Hebei and Beijing[J]. Seismology and Geology, 19（3）: 193-201 （in Chinese）.
    向宏发, 方仲景, 徐杰, 李如成, 贾三发, 郝书俭, 王景钵, 张晚霞. 1988. 三河—平谷8级地震区的构造背景与大震重复性研究[J]. 地震地质, 10（1）: 15-28.
    Xiang H F, Fang Z J, Xu J, Li R C, Jia S F, Hao S J, Wang J B, Zhang W X. 1988. Tectonic background of Sanhe-Pinggu seismic area and research on large earthquake repeatability[J]. Seismology and Geology, 10（1）: 15-28 （in Chinese）. （
    向宏发, 方仲景, 张晚霞, 贾三发, 李如成. 1993. 北京平原区隐伏断裂晚第四纪活动性的初步研究[J]. 地震学报, 15（3）: 385-388.
    Xiang H F, Fang Z J, Zhang W X, Jia S F, Li R C. 1993. Preliminary study of Late Quaternary activities of concealed fractures in Beijing plain[J]. Acta Seismologica Sinica, 15（3）: 385-388 （in Chinese）.
    向宏发, 方仲景, 张晚霞,李如成, 贾三发. 1995. 北京平原区隐伏断裂晚第四纪活动特征的联合剖面研究[J]. 地震研究, 18(1):75-79.
    Xiang H F, Fang Z J, Zhang W X, Li R C, Jia S F. 1995. Joint profile survey of active features for the Late Quaternary subsurface faults in Beijing plain region[J]. Seismology and Geology, 18(1):75-79 （in Chinese）.
    徐锡伟, 计凤桔, 于贵华, 陈文彬, 王峰, 江娃利. 2000. 用钻孔地层剖面记录恢复古地震序列: 河北夏垫断裂古地震研究[J]. 地震地质, 22（1）: 9-19.
    Xu X W, Ji F J, Yu G H, Chen W B, Wang F, Jiang W L. 2000. Reconstruction of paleoearthquake sequence using stratigraphic records from drill logs: A study at the Xiadian fault, Beijing[J]. Seismology and Geology, 22（1）: 9-19 （in Chinese）.
    徐锡伟, 吴卫民, 张先康, 马胜利, 马文涛, 于贵华, 顾梦林, 江娃利. 2002. 首都圈地区地壳最新构造变动与地震[M]. 北京: 科学出版社: 1–376.
    Xu X W, Wu W M, Zhang X K, Ma S L, Ma W T, Yu G H, Gu M L, Jiang W L. 2002. New Changing of Crustal Tectonic and Earthquake in Capital Circle[M]. Beijing: Science Press: 1–376 （in Chinese）.
    雍凡, 蒋正中, 罗水余, 李颜贵, 刘建生, 刘子龙. 2014. 夏垫断裂北段浅部构造的高分辨率地震反射勘探研究[J]. 工程地球物理学报, 11（6）: 832-836.
    Yong F, Jiang Z Z, Luo S Y, Li Y G, Liu J S, Liu Z L. 2014. The seismic reflection study on high-resolution profile of shallow structure in north part of Xiadian fault[J]. Chinese Journal of Engineering Geophysics, 11（6）: 832-836 （in Chinese）.
    赵成彬, 酆少英, 秦学业, 刘保金, 寇昆朋, 郭新景, 李吉昌, 孙振国. 2010. 夏垫断裂浅部特征高分辨反射地震探测研究[J]. 地震研究, 33（1）: 81-85.
    Zhao C B, Feng S Y, Qin X Y, Liu B J, Kou K P, Guo X J, Li J C, Sun Z G. 2010. Research on the shallow structure characteristics of Xiadian fault using high-resolution artificial seismic exploration method[J]. Journal of Seismological Research, 33（1）: 81-85 （in Chinese）.
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