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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第45卷

期数:

2023年第05期

页码:

1257-1269

栏目:

庆贺汤中立院士从事地质工作七十周年专辑

出版日期:

2023-09-15

文章信息/Info

Title:

Characteristics of Surface Rupture Zone of 1679 Sanhe-Pinggu M 8 Earthquake in Xiadian Fault of Beijing Plain, China

文章编号:

1672-6561(2023)05-1257-13

作者:

邢晓琴¹; 2; 3; 戚帮申²; 3*; 丰成君²; 3; 杨肖肖²; 3; 谭成轩²; 3; 邓亚虹¹; 宋焱勋¹; 慕焕东⁴

(1. 长安大学 地质工程与测绘学院,陕西 西安 710054; 2. 中国地质科学院地质力学研究所,北京 100081; 3. 自然资源部活动构造与地质安全重点实验室,北京 100081; 4. 西安理工大学 土木建筑工程学院,陕西 西安 710048)

Author(s):

XING Xiao-qin¹; 2; 3;  QI Bang-shen²; 3*;  FENG Cheng-jun²; 3;  YANG Xiao-xiao²; 3;  TAN Cheng-xuan²; 3;  DENG Ya-hong¹;  SONG Yan-xun¹;  MU Huan-dong⁴

(1. School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China; 2. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China; 3. Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China; 4. School of Civil Engineering and Architecture, Xi'an University of Technology, Xi'an 710048, Shaanxi, China)

关键词:

古地震;  夏垫断裂;  三河—平谷地震;  地表破裂带;  大地震;  探槽;  地层位错;  北京

Keywords:

paleoearthquake;  Xiadian fault;  Sanhe-Pinggu earthquake;  surface rupture zone;  violent earthquake;  trench;  formation dislocation;  Beijing

分类号:

P316

DOI:

10.19814/j.jese.2022.12077

文献标志码:

A

摘要:

夏垫断裂是北京地区重要的活动断裂之一。1679年该断裂发生三河—平谷8级地震,是北京及邻区历史记录的最大地震,地表形成了至今仍清晰可见的地震地表破裂带。弄清楚该断裂古地震活动和地表破裂带特征是优化北京地区国土空间开发格局和防灾减灾体系建设的重要内容。通过探槽开挖、光释光(OSL)测年、断层陡坎形态及地层位错分析,揭示了夏垫断裂古地震活动性、古地震序列和地表破裂带特征。结果表明:①夏垫断裂大胡庄南探槽显示的地层错断、地震楔及崩积楔等揭示了夏垫断裂的两次古地震事件,分别约为(1.610±0.130)ka B.P.古地震及1679年三河—平谷8级地震,地层位错分别约为0.3、2.5 m; ②夏垫断裂20 ka以来存在7个期次的古地震事件,大地震的平均复发周期约为2 716年; ③地震地表破裂带地层位错整体趋势与地形测量数据所得结果基本一致,但在大康庄段到齐心庄段,地层位错距离大于断层陡坎地面测量的高度,表明地表断层陡坎形态可能受人类活动的影响,探槽揭露的地层位错量有助于进一步理解夏垫断裂1679年三河—平谷8级地震地表破裂带特征。

Abstract:

The Xiadian fault is one of the most important active faults in Beijing. The Sanhe-Pinggu M 8 earthquake, which occurs on the fault in 1679, is the largest earthquake on record in Beijing and its adjacent areas. The surface forms a seismic surface rupture zone that is still clearly visible. The characteristics of the ancient seismic activity and surface rupture zone of the fault are important for optimizing the land-space development pattern and the disaster prevention and mitigation system in Beijing. Through trench excavation, optically stimulated luminescence(OSL)dating, fault scarp morphology and stratigraphic dislocation analysis, the paleoseismic activity, paleoseismic sequence, and surface rupture zone characteristics of Xiadian fault were revealed. The results show that ① the stratigraphic dislocations, seismic wedges, and colluvial wedges displayed by Dahuzhuang south trench of Xiadian fault reveal two paleoseismic events, which are about(1.610±0.130)ka B.P. and 1679 Sanhe-Pinggu M 8 earthquake; the stratigraphic dislocations are about 0.3 and 2.5 m, respectively; ② there has been seven periods of paleoearthquake events since 20 ka on Xiadian fault, and the average recurrence period of violent earthquakes is about 2 716 years; ③ however, in the Dakangzhuang-Qixinzhuang sections, the stratigraphic dislocation distance is greater than the height of the fault scarp measured on the ground, indicating that the surface fault scarp morphology may be affected by human activities. The amount of stratigraphic dislocation revealed by the trench is helpful to further understand the surface rupture zone characteristics of 1679 Sanhe-Pinggu M 8 earthquake on Xiadian fault.

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[1]庞炜,何文贵,袁道阳,等.青海大柴旦断裂古地震特征[J].地球科学与环境学报,2015,37(03):87.
　PANG Wei,HE Wen-gui,YUAN Dao-yang,et al.Paleoseismic Characteristics of Dachaidan Fault in Qinghai[J].Journal of Earth Sciences and Environment,2015,37(05):87.

备注/Memo

备注/Memo:

收稿日期:2022-12-31; 修回日期:2023-04-06投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41772275,42102236); 中国地质调查局地质调查项目(DD20230540,DD20190317)
作者简介:邢晓琴(1997-),女,山西阳泉人,长安大学工学硕士研究生,E-mail:xiaoqin18870773341@163.com。
*通讯作者:戚帮申(1988-),男,江苏徐州人,中国地质科学院地质力学研究所副研究员,工学博士,E-mail:qibangshen@126.com。

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