依兰-伊通断裂带尚志段晚全新世以来的强震复发间隔:来自古地震与历史文献的约束

doi:10.3969/j.issn.0253-4967.2016.04.004

地震地质 ›› 2016, Vol. 38 ›› Issue (4): 844-861.DOI: 10.3969/j.issn.0253-4967.2016.04.004

依兰-伊通断裂带尚志段晚全新世以来的强震复发间隔:来自古地震与历史文献的约束

余中元^1,2,3, 张培震², 闵伟¹, 韦庆海³, 刘玉刚¹, 刘双³

1. 活动构造与火山重点实验室, 中国地震局地质研究所, 北京 100029;
2. 地震动力学国家重点实验室, 中国地震局地质研究所, 北京 100029;
3. 黑龙江省地震局, 哈尔滨 150090

收稿日期:2015-10-21 修回日期:2016-03-24 出版日期:2016-12-20 发布日期:2017-01-20
通讯作者: 闵伟,研究员,E-mail:dzs_min@163.com
作者简介:余中元,男,1982年生,2016年在中国地震局地质研究所获构造地质学专业博士学位,高级工程师,研究方向为东北地区的新构造与活动构造,电话:010-62009006,E-mail:yuyangzi9811@126.com。
基金资助:
中国地震局地震科技星火计划项目（XH14018Y）；黑龙江省国土资源科技研究项目（依舒断裂第四纪构造活动研究）与国家自然科学基金（41272235）共同资助

LATE HOLOCENE AVERAGE RECURRENCE INTERVAL OF GREAT EARTHQUAKES OF SHANGZHI PART OF THE YILAN-YITONG FAULT ZONE, NE CHINA: CONSTRAINTS FROM PALEO-EARTHQUAKES AND HISTORICAL WRITTEN RECORDS

YU Zhong-yuan^1,2,3, ZHANG Pei-zhen², MIN Wei¹, WEI Qing-hai³, LIU Yu-gang¹, LIU Shuang³

1. Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
2. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
3. Heilongjiang Earthquake Administration, Harbin 150090, China

Received:2015-10-21 Revised:2016-03-24 Online:2016-12-20 Published:2017-01-20

摘要/Abstract

摘要：

尽管依兰-伊通断裂中生代-早新生代以来的运动学和动力学研究在过去几十年中取得了显著进展和丰富成果，但受研究条件和手段所限，该断裂晚第四纪以来的强震复发间隔长期以来缺乏可靠的研究结果，致使无法科学认识其活动习性和地震危险性。基于高精度卫星影像解译和野外地质调查，发现该断裂尚志段存在至少长约25km的线性断层槽谷和陡坎。探槽开挖揭露出该断裂在全新世晚期发生EⅠ和EⅡ两期古地震事件，运动方式为走滑兼逆冲挤压，伴随明显的地层褶皱与缩短变形，累计垂直同震位移量约为（3.2±0.1）m。¹⁴C测试年代结果约束古地震事件EⅠ发生于（440±30）~（180±30）a BP，事件EⅡ发生于（4 090±30）~（3 880±30）a BP。晚全新世以来的强震复发间隔约为（3 675±235）a。进一步的史料挖掘研究表明，EⅠ事件可能对应于朝鲜《日省录》记录的于公元1810年（清朝）发生在该地区的宁古塔历史地震，震级约7.0级。

关键词: 依兰-伊通断裂, 晚全新世, 古地震, 复发间隔, 历史记录, 约束

Abstract:

Although the kinematics and mechanics of the Yilan-Yitong fault zone (YYFZ) since the Mesozoic-early Cenozoic were studied very well in the past decades,few results about the average recurrence interval of great earthquakes in late Quaternary,which is the most important parameter for us to understand the active tectonics and potential seismic hazard of this crucial structure,were obtained because of its unfavorable work environments.Based on interpretations of high-resolution satellite images and detailed geologic and geomorphic mapping,we discovered that there exist linear fault scarp landforms and troughs in the Shangzhi part of YYFZ with a length of more than 25km.Synthesized results of trenches excavation and differential GPS measurements of terrace surfaces indicate two paleo-events EⅠ and EⅡ occurring in Shangzhi part during the late Holocene,which resulted in ca.(3.2±0.1) m accumulated vertical coseismic displacement with strike-slip motion accompanied by thrusting and shortening deformation.¹⁴C samples dating suggests that event EⅠ might occur at (440±30) and (180±30) a BP and event EⅡ might happen between (4 090±30) and (3 880±30) a BP,and the average recurrence interval of major earthquakes on the YYFZ is around (3 675±235) a.Historical written records discovered from Korea show that the event EⅠ may correspond to the earthquake occurring in AD 1810(Qing Dynasty in Chinese history) in Ningguta area with magnitude 7.0.

Key words: Yilan-Yitong fault zone, late Holocene, paleo-earthquakes, average recurrence interval of great earthquakes, historical written records, constraints

中图分类号:

P315.2

余中元, 张培震, 闵伟, 韦庆海, 刘玉刚, 刘双. 依兰-伊通断裂带尚志段晚全新世以来的强震复发间隔:来自古地震与历史文献的约束[J]. 地震地质, 2016, 38(4): 844-861.

YU Zhong-yuan, ZHANG Pei-zhen, MIN Wei, WEI Qing-hai, LIU Yu-gang, LIU Shuang. LATE HOLOCENE AVERAGE RECURRENCE INTERVAL OF GREAT EARTHQUAKES OF SHANGZHI PART OF THE YILAN-YITONG FAULT ZONE, NE CHINA: CONSTRAINTS FROM PALEO-EARTHQUAKES AND HISTORICAL WRITTEN RECORDS[J]. SEISMOLOGY AND GEOLOGY, 2016, 38(4): 844-861.

参考文献

邓起东, 冉勇康, 杨晓平, 等. 2007. 中国活动构造图. 北京:地震出版社. 2-3.
DENG Qi-dong, RAN Yong-kang, YANG Xiao-ping, et al. 2007. Active Tectonics Map of China(1 ︰ 4 million). Seismological Press, Beijing. 2-3(in Chinese).
邓起东, 于贵华, 叶文华. 1992. 地震地表破裂参数与震级关系的研究［M］//国家地震局地质研究所编. 活动断裂研究(2). 北京:地震出版社. 247-264.
DENG Qi-dong, YU Gui-hua, YE Wen-hua. 1992. Study on the Relations between Parameters Of Surface Rupture and Magnitude［M］//Institute of Geology, State Seismological Bureau(ed). Research of Active fault (2). Seismological Press, Beijing. 247-264(in Chinese).
侯治华, 任俊杰, 舒赛兵. 2009. 吉林省舒兰-伊通断裂的分段及其地震活动性研究［J］. 地球物理学进展, 24(4):1275-1283.
HOU ZHi-hua, REN Jun-jie, SHU Sai-bing. 2009. Segmentation and seismicity of the Shulan-Yitong fault zone in eastern Jilin Province［J］. Progress in Geophysics, 24(4):1275-1283(in Chinese).
李裕澈, 时振梁, 曹学锋. 2013. 朝鲜史料记载的中国地震［J］. 中国地震, 29(2):276-283.
LI Yu-che, SHI Zhen-liang, CAO Xue-feng. 2013. The records of Chinese earthquakes in the Korean historical documents［J］. Earthquake Research in China, 29(2):276-283(in Chinese).
闵伟, 焦德成, 周本刚, 等. 2011. 依兰-伊通全新世活动的新发现及其意义［J］. 地震地质, 33(1):74-79. doi:10.3969/j.issn.0253-4967.2011.01.014.
MIN Wei, JIAO De-cheng, ZHOU Ben-gang, et al. 2011. The significance of discovery on Holocene activity on the Yilan-Yitong fault in Northeast China［J］. Seismology and Geology, 33(1):74-79(in Chinese).
冉勇康, 陈立春, 陈文山, 等. 2012. 中国大陆古地震研究的关键技术与案例解析(2):汶川地震地表变性特征与褶皱逆断层古地震识别［J］. 地震地质, 34(3):385-399. doi:10.3969/j.issn.0253-4967.2012.02.001.
RAN Yong-kang, CHEN Li-chun, CHEN Wen-shan, et al. 2012. Key techniques and several cases analysis in paleoseismic studies in mainland China(2):Surface deformation characteristics of Wenchuan earthquake and paleoseismic indicators on fold-reverse fault［J］. Seismology and Geology, 34(3):385-399(in Chinese).
冉勇康, 史翔, 王虎, 等. 2010. 汶川M8地震最大地表同震垂直位移量及其地表变形样式［J］. 科学通报, 55(2):154-162.
RAN Yong-kang, SHI Xiang, WANG Hu, et al. 2010. The maximum coseismic vertical surface displacement and surface deformation pattern accompanying the M_S8.0 Wenchuan earthquake［J］. Chinese Science Bulletin, 55(2):154-162(in Chinese).
吴戈, 房贺岩, 李志田, 等. 1987. 1119年 "肇州之始兴, 隆州之利涉"地震考［J］. 东北地震研究, 2:35-41.
WU Ge, FANG He-yan, LI Zhi-tian, et al. 1987. The textual research on "Zhaozhou Shixing" and "Longzhou Lishe" earthquake, 1119［J］. Northeastern Seismological Research, 2:35-41(in Chinese).
吴戈, 房贺岩, 李志田, 等. 1988. 1119年前郭地震考察与研究［J］. 东北地震研究, 4(1):67-76.
WU Ge, FANG He-yan, LI Zhi-tian, et al. 1988. The investigation and study of Qianguo earthquake, 1119［J］. Northeastern Seismological Research, 4(1):67-76(in Chinese).
吴福元, 徐义刚, 朱日祥, 等. 2014. 克拉通岩石圈减薄与破坏［J］. 中国科学(D辑), 11(23):2358-2372.
WU Fu-yuan, XU Yi-gang, ZHU Ri-xiang, et al. 2014. Lithospheric thinning and destruction of the Craton［J］. Science in China(Ser D), 11(23):2358-2372(in Chinese).
徐嘉炜, 马国锋. 1992. 郯庐断裂带研究的十年回顾［J］. 地质论评, 38(4):316-324.
XU Jia-wei, MA Guo-feng. 1992. The ten-year research history on Tanlu Fault［J］. Geological Review, 38(4):316-324(in Chinese).
杨宝俊, 穆石敏. 1996. 中国满洲里-绥芬河地学断面地球物理综合研究［J］. 地球物理学报, 39(6):772-782.
YANG Bao-jun, MU Shi-min. 1996. The geophysical comprehensive study of Manzhouli-Suifenhe geological sections［J］. Journal of Geophysics, 39(6):772-782(in Chinese).
余中元, 闵伟, 韦庆海, 等. 2015. 松辽盆地北部反转构造的几何特征、变形机制及其地震地质意义［J］. 地震地质, 37(1):13-32. doi:10.3969/j.issn.0253-4967.2015.01.002.
YU Zhong-yuan, MIN Wei, WEI Qing-hai, et al. 2015. The geometric characteristics and tectonic deformation mechanism of inversion structures in northern Songliao Basin and their seismo-geological significance:A case from Da'an-Dedu Fault［J］. Seismology and Geology, 37(1):13-32(in Chinese).
张培震, 邓起东, 徐锡伟, 等. 1994. 盲断层 "褶皱地震"与1906年玛纳斯地震［J］. 地震地质, 16(3):193-204.
ZHANG Pei-zhen, DENG Qi-dong, XU Xi-wei, et al. 1994. Blind thrust, folding earthquake, and the 1906 Manas earthquake, Xinjiang［J］. Seismology and Geology, 16(3):193-204(in Chinese).
张培震, 邓起东, 张国民, 等. 2003. 中国大陆的强震活动与活动地块［J］. 中国科学(D辑), S1:12-20.
ZHANG Pei-zhen, DENG Qi-dong, ZHANG Guo-min, et al. 2003. Active tectonic blocks and strong earthquakes in the continent of China［J］. Science in China(Ser D), S1:12-20(in Chinese).
张培震, 邓起东, 张竹琪, 等. 2013. 中国大陆的活动断裂、地震灾害及其动力过程［J］. 中国科学(D辑), 10:1607-1620.
ZHANG Pei-zhen, DENG Qi-dong, ZHANG Zhu-qi, et al. 2013. Active faults, earthquake hazards and associated geodynamic processes in continental China［J］. Science in China(Ser D), 10:1607-1620(in Chinese).
张培震, 王琪, 马宗晋. 2002. 中国大陆现今构造运动的GPS速度场与活动地块［J］. 地学前缘, 9(2):430-431.
ZHANG Pei-zhen, WANG Qi, MA Zong-jin. 2002. GPS velocity field and active crustal blocks of contemporary tectonic deformation in continental China［J］. Earth Science Frontiers, 9(2):430-431(in Chinese).
张培震, 张会平, 郑文俊, 等. 2014. 东亚大陆新生代构造演化［J］. 地震地质, 36(3):574-585. doi:10.3969/j.issn.0253-4967.2014.03.003.
ZHANG Pei-zhen, ZHANG Hui-ping, ZHEN Wen-jun, et al. 2014. Cenozoic tectonic evolution of continental eastern Asia［J］. Seismology and Geology, 36(3):574-585(in Chinese).
朱日祥, 陈凌, 吴福元, 等. 2011. 华北克拉通破坏的时间、范围与机制［J］. 中国科学(D辑), 5:583-592. doi:10.1007/s11430-011-4203-4.
ZHU Ri-xiang, CHEN Ling, WU Fu-yuan, et al. 2011. Timing, scale and mechanism of the destruction of the North China Craton［J］. Science in China(Ser D), 5:583-592(in Chinese).
朱日祥, 徐义刚, 朱光, 等. 2012. 华北克拉通破坏［J］. 中国科学(D辑), 42(8):1135-1159.
ZHU Ri-xiang, XU Yi-gang, ZHU Guang, et al. 2012. Destruction of the North China Craton［J］. Science in China(Ser D), 42(8):1135-1159(in Chinese).
Allen M B, Macdonald D I M, Xun Z, et al. 1997. Early Cenozoic two-phase extension and late Cenozoic thermal subsidence and inversion of the Bohai Basin, North China［J］. Mar Pet Geol, 14(7-8):951-972.
Gurpinar A. 2005. The importance of paleoseismology in seismic hazard studies for critical facilities［J］. Tectonophysics, 408(1-4):23-28.
Hsiao L, Graham S A, Tilander N. 2004. Seismic reflection imaging of a major strike-slip fault zone in a rift system:Paleogene structure and evolution of the Tan-Lu fault system, Liaodong Bay, Bohai, offshore China［J］. AAPG Bull, 88(1):71-97.
Huang L, Liu C Y, Timothy M K. 2014. Cenozoic evolution of the Tanlu fault zone(East China)-Constraints from seismic data［J］. Gondwana Research, 28(3):1079-1095. doi:10.1016/j.gr.2014.09.005.
Huang J, Zhao D P. 2006. High-resolution mantle tomography of China and surrounding regions［J］. Journal of Geophysical Research, 111:B09305.
Li X S, Zhao Y X, Liu B H, et al. 2010. Structural deformation and fault activity of the Tanlu fault zone in the Bohai Sea since the late Pleistocene［J］. Chinese Science Bulletin, 55:1908-1916.
Li Z G, Jia D, Chen W, et al. 2013. Structural deformation and evolution of right-lateral strike-slip tectonics of the Liaohe western depression during the early Cenozoic［J］. J Asian Earth Sci, 77:1-11.
Liu B, Zhu G, Zhai M J, et al. 2015. Quaternary faulting of the Jiangsu part of the Tanlu fault zone, East China:Evidence from field investigations and OSL dating［J］. J Asian Earth Sci. doi:10.1016/j.jseaes.2015.04.003.
Liu M, Stein S, Wang H. 2010. 2000 years of migrating earthquakes in North China:How earthquakes in midcontinent differ from those at plate boundaries［J］. Lithosphere, 3:128-132.
Liu M, Yang Y Q, Shen Z K, et al. 2007. Active tectonics and intracontinental earthquakes in China:The kinematics and geodynamics［J］. The Geological of America, 425:299-318.
Min W, Liu Y G, Jiao D C, et al. 2013. Evidence for Holocene activity of the Yilan-Yitong Fault, northeastern section of the Tanlu fault zone in Northeast China［J］. Journal of Asian Earth Sciences, 67:207-216. doi:10.1016/j.jseaes.2013.02.031.
Ren J Y, Tamaki K, Li S T, et al. 2002. Late Mesozoic and Cenozoic rifting and its dynamic setting in eastern China and adjacent areas［J］. Tectonophysics, 344(3):175-205.
Sieh K E. 1984. Lateral offsets and revised dates of large prehistoric earthquakes at Pallett Creek, southern California［J］. J Geophysics Res, 89:7641-7670.
Wallace R E. 1970. Earthquake recurrence intervals on the San Andreas Fault［J］. Geol Soc Am Bull, 81:2875-2890.
Wang Q, Zhang P Z, Freymueller J T, et al. 2001. Present-day crustal deformation in China constrained by Global Positioning System measurements［J］. Science, 294:574-577.
Wang Z C, Deng Q D, Du X S, et al. 2006. Active fault survey on the Tanlu fault zone in Laizhou Bay［J］. Acta Seismologica Sinica, 19:530-541.
Wesnousky S G. 2006. Predicting the endpoints of earthquake ruptures［J］. Nature, 444:358-360.
Yang T H, Xu T G. 2004. Hydrocarbon habitat of the offshore Bohai Basin, China［J］. Mar Petrol Geol, 21(6):691-708.
Yin A. 2010. Cenozoic tectonic evolution of Asia:A preliminary synthesis［J］. Tectonophysics, 488(1):293-325.
Yin A, Yu X J, Shen Z K, et al. 2015. A possible seismic gap and high earthquake hazard in the North China Basin［J］. Geology, 43(1):19-22.
Yu Z Y, Zhan P Z, Min W, et al. 2015. Late Cenozoic deformation of the Da'an-Dedu fault zone and its implications for the earthquake activities in the Songliao Basin, NE China［J］. Journal of Asian Earth Sciences, 17:83-95.
Zhang F Q, Chen H L, Yang S F, et al. 2012. Late Mesozoic-Cenozoic evolution of the Sanjiang Basin in NE China and its tectonic implications for the West Pacific continental margin［J］. J Asian Earth Sci, 49:287-299.
Zhang P Z, Deng Q D, Zhang G M, et al. 2003. Active tectonic blocks and strong earthquakes in the continent of China［J］. Science in China(Ser D), 46:13-24.
Zhang P Z, Min W, Deng Q D, et al. 2005. Paleoearthquake rupture behavior and recurrence of great earthquakes along the Haiyuan Fault, northwestern China［J］. Science in China(Ser D), 48(3):364-375.
Zhang R Q, Wu Q J, Sun L, et al. 2014. Crustal and lithospheric structure of Northeast China from S-wave receive functions［J］. Earth and Planetary Science Letters, 41:196-205.
Zhu G, Hu W, Song L H, et al. 2015. Quaternary activity along the Tanlu fault zone in the Bohai Bay, East China:Evidence from seismic profiles［J］. J Asian Earth Sci. doi:10.1016/j.jseaes.2015.03.030.

[1]	刘庆, 刘韶, 张世民. 大凉山断裂带中段越西断裂晚第四纪古地震[J]. 地震地质, 2023, 45(2): 321-337.
[2]	李安, 万波, 王晓先, 计昊旻, 索锐. 金州断裂盖州北鞍山段古地震破裂的新证据[J]. 地震地质, 2023, 45(1): 111-126.
[3]	郑海刚, 姚大全, 赵朋, 杨源源, 黄金水. 郯庐断裂带赤山段全新世新活动的特征[J]. 地震地质, 2023, 45(1): 127-138.
[4]	杨源源, 李鹏飞, 路硕, 疏鹏, 潘浩波, 方良好, 郑海刚, 赵朋, 郑颖平, 姚大全. 郯庐断裂带中段F₅断裂淮河-女山湖段的古地震与垂直滑动速率[J]. 地震地质, 2022, 44(6): 1365-1383.
[5]	石文芳, 徐伟, 尹金辉, 郑勇刚. 秦岭北缘古地震基岩崩塌和滑坡施密特锤暴露年龄[J]. 地震地质, 2022, 44(6): 1384-1402.
[6]	李倩, 酆少英, 秦晶晶, 田一鸣. 用高分辨率谱分解方法研究三河-平谷大地震区的深部细结构[J]. 地震地质, 2022, 44(5): 1257-1272.
[7]	刘兴旺, 袁道阳, 姚赟胜, 邹小波. 三危山断裂敦煌段古地震活动特征[J]. 地震地质, 2021, 43(6): 1398-1411.
[8]	常祖峰, 常昊, 李鉴林, 毛泽斌, 臧阳. 维西-乔后断裂全新世活动与古地震[J]. 地震地质, 2021, 43(4): 881-898.
[9]	冯嘉辉, 陈立春, 王虎, 刘姣, 韩明明, 李彦宝, 高帅坡, 卢丽莉. 大凉山断裂带北段石棉断裂的古地震[J]. 地震地质, 2021, 43(1): 53-71.
[10]	马骏, 周本刚, 王明明, 安力科. 鲜水河断裂带折多塘断裂西北段全新世活动的地质地貌依据[J]. 地震地质, 2020, 42(5): 1021-1038.
[11]	张玲, 杨晓平, 李胜强, 黄伟亮, 杨海波. 秋里塔格褶皱带东段探槽的古地震事件[J]. 地震地质, 2020, 42(5): 1039-1057.
[12]	黄帅堂, 胡伟华, 杨攀新, 李帅, 伊力亚尔. 东天山唐巴勒-塔斯墩断裂带晚第四纪活动特征[J]. 地震地质, 2020, 42(5): 1058-1071.
[13]	王莅斌, 尹功明, 袁仁茂, 王盈, 苏刚. 金沙江中游永胜昔格达层软沉积变形构造[J]. 地震地质, 2020, 42(5): 1072-1090.
[14]	胡宗凯, 杨晓平, 杨海波, 吴国栋, 李军, 周本刚. 北天山博罗可努-阿齐克库都克断裂精河段的古地震事件[J]. 地震地质, 2020, 42(4): 773-790.
[15]	覃金堂, 陈杰, 李涛. 阿尔金断裂带中段现代沉积物样品钾长石红外激发后红外释光的残留信号——对年轻古地震事件测年的指示意义[J]. 地震地质, 2020, 42(4): 981-992.

依兰-伊通断裂带尚志段晚全新世以来的强震复发间隔:来自古地震与历史文献的约束

LATE HOLOCENE AVERAGE RECURRENCE INTERVAL OF GREAT EARTHQUAKES OF SHANGZHI PART OF THE YILAN-YITONG FAULT ZONE, NE CHINA: CONSTRAINTS FROM PALEO-EARTHQUAKES AND HISTORICAL WRITTEN RECORDS

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价