THE LATE QUATERNARY ACTIVITY CHARACTERISTICS OF THE MIDDLE-NORTHERN SECTION OF THE SHANGWUJING FAULT IN THE LUXI BLOCK

doi:10.3969/j.issn.0253-4967.20250065

SEISMOLOGY AND GEOLOGY ›› 2026, Vol. 48 ›› Issue (1): 1-18.DOI: 10.3969/j.issn.0253-4967.20250065

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THE LATE QUATERNARY ACTIVITY CHARACTERISTICS OF THE MIDDLE-NORTHERN SECTION OF THE SHANGWUJING FAULT IN THE LUXI BLOCK

WANG Lei¹^,²^,³^,⁴^,⁵⁾(), REN Zhi-kun¹⁾^,^*(), WU Hong-bin²^,³^,⁴^,⁵⁾, WANG Zhi-cai²^,³^,⁴^,⁵⁾, ZHU Xiao-xiao¹⁾, FU Jun-dong²^,³^,⁴^,⁵⁾, JI Hao¹⁾, XUE Jun-zhao⁴⁾, LEI Zhao-wei⁴⁾, WANG Ji-qiang²^,³^,⁴^,⁵⁾

¹⁾ State Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake Administration, Beijing 100029, China
²⁾ Shandong Earthquake Agency, Jinan 250102, China
³⁾ Shandong Engineering Research Center of Earthquake Disaster Risk Prevention and Governance, Jinan 250014, China
⁴⁾ Shandong Luzhen Science and Technology Engineering Limited Liability Company, Jinan 250014, China
⁵⁾ Earthquake Risk Prevention and Governance of Shandong Province, Jinan 250014, China

Received:2025-03-11 Revised:2025-06-05 Online:2026-02-20 Published:2026-03-14

鲁西上五井断裂中北段晚第四纪活动特征

王雷¹^,²^,³^,⁴^,⁵⁾(), 任治坤¹⁾^,^*(), 吴洪斌²^,³^,⁴^,⁵⁾, 王志才²^,³^,⁴^,⁵⁾, 朱笑笑¹⁾, 付俊东²^,³^,⁴^,⁵⁾, 姬昊¹⁾, 薛俊召⁴⁾, 雷兆伟⁴⁾, 王纪强²^,³^,⁴^,⁵⁾

¹⁾ 地震动力学与强震预测全国重点实验室(中国地震局地质研究所), 北京 100029
²⁾ 山东省地震局, 济南 250102
³⁾ 地震灾害风险防治山东省工程研究中心, 济南 250014
⁴⁾ 山东省鲁震科技工程有限公司, 济南 250014
⁵⁾ 山东省震灾风险防治中心, 济南 250014

通讯作者: * 任治坤, 男, 1980年生, 研究员, 博士生导师, 主要从事活动构造与构造地貌研究, E-mail: rzk@ies.ac.cn。
作者简介:
王雷, 男, 1988年生, 工程师, 现为中国地震局地质研究所构造地质学专业在读博士研究生, 主要从事活动构造、地震地质研究, E-mail: wangleifz0421@qq.com。
基金资助:
中国地震局地震科技星火计划项目(XH25014YA); 山东省地震局科研项目(YB2406); 山东省地震局科研项目(YB2106); 山东省地震局科研项目(YW2303); 山东省地震局科研项目(YW2304); 国家自然科学基金(U2239202); 科技部项目(2021FY100103); 山东省地震局科技创新团队培育专项(震灾风险评估研究团队); 山东省地震局科技创新团队培育专项(地震构造研究团队)

Abstract

Abstract:

Since the Middle to Late Miocene, the tectonic regime of eastern North China has undergone a significant transition from extensional deformation to a shear-dominated system under a nearly E-W compressional stress field. This shift is attributed to the combined influence of the eastward extrusion of the Tibetan plateau and the retreat of the West Pacific Plate. The Tanlu fault zone, a major active strike-slip structure in eastern China, serves as the tectonic boundary between the Luxi and Ludong blocks. Within the Luxi Uplift, located in the east part of the North China Craton, a prominent basin-and-range system has developed, controlled by a series of NW-trending faults. Late Quaternary activity along these faults, including the Cangni Fault, Xintai-Mengyin Fault, Tongyedian-Sunzu Fault, Zhangdian-Renhe Fault, Yidu Fault, and Shuangshan-Lijiazhuang Fault, demonstrates a parallel, roughly equidistant arrangement, with a convergent pattern toward the Tanlu fault zone.

The Shangwujing Fault is a crucial NE-trending dextral strike-slip fault, and the Shuangshan-Lijiazhuang Fault is a NW-trending sinistral strike-slip fault. Spatially, these two faults form an X-shaped conjugate structure, which governs the formation and evolution of the Linqu Basin. The shallow surface expression of the Shangwujing Fault can be segmented into northern, central-northern, central-southern, and southern sections, demarcated by Tongyugou Village, Dongliushui Village, and Yiyuan Beibudong Village. While prior studies identified Late Pleistocene activity in the central-northern segment, evidence for fault motion between Jiujie Village and Dongliushui Village remained insufficient.

Key words: Luxi block, Shangwujing Fault, Airborne Light Detection and Ranging (LiDAR), right-lateral strike-slip, late Pleistocene activity

摘要：

上五井断裂是鲁西地块内一条重要的NE向晚第四纪活动断裂, 与双山-李家庄断裂共同构成了“X”形共轭构造。在地表浅层, 上五井断裂从北向南以桐峪沟村、东流水村、沂源北埠东村为界, 大致可以划分为北段、中北段、中南段和南段。文中采用地质地貌调查、机载激光雷达航测、断层泥定年等方法, 重点对上五井断裂中北段九杰村—东流水村之间的段落进行了位移测量和活动性研究, 发现了该段落的新活动证据。结果表明, 九杰村—东流水村之间的断裂长约18km, 右旋走滑活动显著。九杰村南山脊的右旋位移量为475~580m, 崔木村东山脊的右旋位移量为48~74m, 东流水村附近冲沟的最小右旋位移量为35m。根据地貌位错和断层泥电子自旋共振定年结果((94±5)kaBP), 确定该段落晚更新世有活动。基于文中研究, 确定上五井断裂中北段晚第四纪活动段长约45km。历史上, 上五井断裂与双山-李家庄断裂的交会处曾发生1829年 6¼ 级地震, 综合分析认为上五井断裂的潜在发震能力可达6.5级。

关键词: 鲁西, 上五井断裂, 激光雷达, 右旋走滑, 晚更新世活动

WANG Lei, REN Zhi-kun, WU Hong-bin, WANG Zhi-cai, ZHU Xiao-xiao, FU Jun-dong, JI Hao, XUE Jun-zhao, LEI Zhao-wei, WANG Ji-qiang. THE LATE QUATERNARY ACTIVITY CHARACTERISTICS OF THE MIDDLE-NORTHERN SECTION OF THE SHANGWUJING FAULT IN THE LUXI BLOCK[J]. SEISMOLOGY AND GEOLOGY, 2026, 48(1): 1-18.

王雷, 任治坤, 吴洪斌, 王志才, 朱笑笑, 付俊东, 姬昊, 薛俊召, 雷兆伟, 王纪强. 鲁西上五井断裂中北段晚第四纪活动特征[J]. 地震地质, 2026, 48(1): 1-18.

Figures/Tables 9

Fig. 1 A schematic map of the seismic structure near the study area.

Table1 Dating samples collected from the outcrop of the Shangwujing Fault

样品编号	实验室编号	样品类别	深度/m	测试方法	等效剂量/Gy	剂量率/Gy·ka^-1	年龄/ka
SWJ-011	24016	断层泥	2	ESR	1 088±98	5.79±0.29	188±17
SWJ-015	24017	断层泥	0.3	ESR	421±23	4.48±0.22	94±5

Fig. 2 The surface geometric distribution of the Shangwujing Fault in the study area.

Fig. 3 Geological and geomorphological features of the Shangwujing Fault in the south of Jiujie Village.

Fig. 4 Geological and geomorphological features of the Shangwujing Fault in the east of Cuimu Village.

Fig. 5 Geomorphic features of the Shangwujing Fault in the west of Dongliushui Village.

Fig. 6 Geological profile of the Shangwujing Fault in the south of Jiujie Village.

Fig. 7 Geological profile of the Shangwujing Fault in the east of Cuimu Village.

Fig. 8 Late Quaternary tectonic framework of the eastern margin of the Luxi block.

References 63

[1]	晁洪太, 崔昭文, 李家灵. 1992. 鲁中地区NW向断裂及其第四纪晚期的活动特征[J]. 地震学刊, (2): 1—10.
	CHAO Hong-tai, CUI Zhao-wen, LI Jia-ling. 1992. The NW trending faults in middle part of Shandong Province and their activities in the late Quaternary[J]. Journal of Seismology, (2): 1—10 (in Chinese).
[2]	晁洪太, 李家灵, 崔昭文. 1995. 山东及其沿海地区强震(M≥6)发生的地质构造背景[J]. 地震研究, 18(2): 188—196.
	CHAO Hong-tai, LI Jia-ling, CUI Zhao-wen. 1995. Tectonic conditions of strong earthquakes with M≥6 in Shandong Province and its adjacent seas[J]. Journal of Seismological Research, 18(2): 188—196 (in Chinese).
[3]	晁洪太, 李家灵, 崔昭文, 等. 1997. 与1668年郯城8(½)级地震断层有关的几个问题讨论[J]. 华北地震科学, 15(4): 18—25.
	CHAO Hong-tai, LI Jia-ling, CUI Zhao-wen, et al. 1997. Discussion on several problems related to the seismic fault of the 1668 Tancheng earthquake(M=8½)[J]. North China Earthquake Sciences, 15(4): 18—25 (in Chinese).
[4]	晁洪太, 王志才, 王雷, 等. 2018. 发震断裂带内黏土矿物的纳微米变形[J]. 地球科学, 43(5): 1746—1754.
	CHAO Hong-tai, WANG Zhi-cai, WANG Lei, et al. 2018. Nano/micro-scale deformation of clay minerals in seismogenic fault zone[J]. Earth Science, 43(5): 1746—1754 (in Chinese).
[5]	邓起东, 卢造勋, 杨主恩. 2007. 城市活动断层探测和断层活动性评价问题[J]. 地震地质, 29(2): 189—200.
	DENG Qi-dong, LU Zao-xun, YANG Zhu-en. 2007. Remarks on urban active faults exploration and associated activity assessment[J]. Seismology and Geology, 29(2): 189—200 (in Chinese).
[6]	丁国瑜, 卢演俦. 1983. 华北地块新构造变形基本特点的讨论[J]. 华北地震科学, 1(2): 1—9.
	DING Guo-yu, LU Yan-chou. 1983. Discussion on the basic characteristics of Neotectonic deformation in the North China block[J]. North China Earthquake Sciences, 1(2): 1—9 (in Chinese).
[7]	付碧宏, 王萍, 孔屏, 等. 2008. 四川汶川5.12大地震同震滑动断层泥的发现及构造意义[J]. 岩石学报, 24(10): 2237—2243.
	FU Bi-hong, WANG Ping, KONG Ping, et al. 2008. Preliminary study of coseismic fault gouge occurred in the slip zone of the Wenchuan M_S8.0 earthquake and its tectonic implications[J]. Acta Petrologica Sinica, 24(10): 2237—2243 (in Chinese).
[8]	高维明, 李家灵, 孙竹友. 1980. 沂沭大陆裂谷的生成与演化[J]. 地震地质, 2(3): 11—18.
	GAO Wei-min, LI Jia-ling, SUN Zhu-you. 1980. Development and evolution of the Yishu rift[J]. Seismology and Geology, 2(3): 11—18 (in Chinese).
[9]	雷启云, 柴炽章, 孟广魁, 等. 2011. 隐伏活断层钻孔联合剖面对折定位方法[J]. 地震地质, 33(1): 45—55. doi: 10.3969/j.issn.0253-4967.2011.01.005.
	LEI Qi-yun, CAI Chi-zhang, MEN Guang-kui, et al. 2011. Method of locating buried active fault by composite drilling section doubling exploration[J]. Seismology and Geology, 33(1): 45—55 (in Chinese).
[10]	李海兵, 许志琴, 王焕, 等. 2018. 汶川地震断裂带滑移行为、物理性质及其大地震活动性——来自汶川地震断裂带科学钻探的证据[J]. 地球物理学报, 61(5): 1680—1697.
	LI Hai-bing, XU Zhi-qin, WANG Huan, et al. 2018. Fault behavior, physical properties and seismic activity of the Wenchuan earthquake fault zone: Evidence from the Wenchuan earthquake Fault Scientific Drilling project(WFSD)[J]. Chinese Journal of Geophysics, 61(5): 1680—1697 (in Chinese).
[11]	李洪奎, 禚传源, 耿科, 等. 2017. 郯-庐断裂带陆内伸展构造: 以沂沭断裂带的表现特征为例[J]. 地学前缘, 24(2): 73—84.
	LI Hong-kui, ZHUO Chuan-yuan, GEN Ke, et al. 2017. Intra-continental extensional tectonics of the Tan-Lu fault zone: An example from the appearance characteristics of the Yishu fault zone[J]. Earth Seience Frontiers, 24(2): 73—84 (in Chinese).
[12]	李家灵, 晁洪太, 崔昭文, 等. 1994. 1668年郯城 8½ 级地震断层及其破裂机制[J]. 地震地质, 16(3): 229—237.
	LI Jia-ling, CHAO Hong-tai, CUI Zhao-wen, et al. 1994. Earthquake fault and Its Rupture Mechanism of the 1668 Tancheng M=8½ Earthquake[J]. Seismology and Geology, 16(3): 229—237 (in Chinese).
[13]	李家灵, 晁洪太, 崔昭文. 1996. 山东临朐盆地边界断裂活动特征及其地震意义[A]. 中国地震学会第6次学术大会论文摘要集[C]. 中国地震学会:59.
	LI Jia-ling, CHAO Hong-tai, CUI Zhao-wen. 1996. Characteristics of Boundary Fault Activity in the Linqu Basin, Shandong Province and Its Seismic Significance [A]. Abstracts Collection of the 6th Academic Conference of the Chinese Seismological Society[C]. Chinese Seismological Society : 59 (in Chinese).
[14]	李少俊, 李三忠, 李玺瑶, 等. 2018. 鲁西地块新生代断裂体系活动性与深部动力机制[J]. 海洋地质与第四纪地质, 38(4): 123—134.
	LI Shao-jun, LI San-zhong, LI Xi-yao, et al. 2018. Activity of Cenozoic fault system in the Luxi block and deep dynamics[J]. Marine Geology & Quaternary Geology, 38(4): 123—134 (in Chinese).
[15]	刘保金, 柴炽章, 酆少英, 等. 2008. 第四纪沉积区断层及其上断点探测的地震方法技术——以银川隐伏活动断层为例[J]. 地球物理学报, 51(5): 1475—1483.
	LIU Bao-jin, CHAI Chi-zhang, FENG Shao-ying, et al. 2008. Seismic exploration method for buried fault and its up-breakpoint in Quaternary sediment area: An example of Yinchuan buried active fault[J]. Chinese Journal of Geophysics, 51(5): 1475—1483 (in Chinese).
[16]	刘春茹, 尹功明, Rainer G. 2013. 石英ESR测年信号衰退特征研究进展[J]. 地球科学进展, 28(1): 24—30.
	LIU Chun-ru, YIN Gong-min, Rainer G. 2013. Research progress of the resetting features of quartz ESR signal[J]. Advance in Earth Science, 28(1): 24—30 (in Chinese).
[17]	罗旭. 2016. 郯庐断裂带中段及其邻区三维电性结构研究: 据Sinoprobe大地电磁测深标准网数据[D]. 北京: 中国地质大学(北京).
	LUO Xu. 2016. The research of three dimensional conductivity structure of the middle section of Tancheng-Lujiang Fault zone and its surrounding regions: Based the data from SinoProbe MT standard network[D]. China University of Geosciences(Beijing), Beijing (in Chinese).
[18]	马洪超. 2011. 激光雷达测量技术在地学中的若干应用[J]. 地球科学(中国地质大学学报), 36(2): 347—354.
	MA Hong-chao. 2011. Review on applications of LiDAR mapping technology to geosciences[J]. Earth Science(Journal of China University of Geosciences), 36(2): 347—354 (in Chinese).
[19]	冉勇康, 王虎, 李彦宝, 等. 2012. 中国大陆古地震研究的关键技术与案例解析(1): 走滑活动断裂的探槽地点、布设与事件识别标志[J]. 地震地质, 34(2): 197—210. doi: 10.3969/j.issn.0253-4967.2012.02.001.
	RAN Yong-kang, WANG Hu, LI Yan-bao, et al. 2012. Key techniques and several cases analysis in paleoseismic studies in mainland China(1): Trenching sites, layouts and paleoseismic indicators on active strike-slip faults[J]. Seismology and Geology, 34(2): 197—210 (in Chinese).
[20]	任治坤, 陈涛, 张会平, 等. 2014. LiDAR 技术在活动构造研究中的应用[J]. 地质学报, 88(6): 1196—1207.
	REN Zhi-kun, CHEN Tao, ZHANG Hui-ping, et al. 2014. LiDAR survey in active tectonics studies: An introduction and overview[J]. Acta Geologica Sinica, 88(6): 1196—1207 (in Chinese).
[21]	申俊峰, 申旭辉, 曹忠全, 等. 2007. 断层泥石英微形貌特征在断层活动性研究中的意义[J]. 矿物岩石, 27(1): 90—96.
	SHEN Jun-feng, SHEN Xu-hui, CAO Zhong-quan, et al. 2007. The characteristics and significances of quartz mico-appearance in the fault gouges on evaluation of the fault activity[J]. Mineralogy and Petrology, 27(1): 90—96 (in Chinese).
[22]	史兰斌, 林传勇, 刘行松, 等. 1996. 基岩区断层新活动年代学研究的问题讨论[J]. 地震地质, 18(4): 319—324.
	SHI Lan-bin, LIN Chuan-yong, LIU Xing-song, et al. 1996. Discussion on the chronology of recent fault activity in bedrock area[J]. Seismology and Geology, 18(4): 319—324 (in Chinese).
[23]	疏鹏, 徐锡伟, 酆少英, 等. 2023. 板泉拉分盆地沉积-构造演化及其对郯庐断裂带新生代晚期右旋走滑运动的响应[J]. 中国科学(D辑), 53(4): 784—805.
	SHU Peng, XU Xi-wei, FENG Shao-ying, et al. 2023. Sedimentary and tectonic evolution of the Banquan pull-apart basin and implications for late Cenozoic dextral strike-slip movement of the Tanlu fault zone[J]. Science China: Earth Sciences, 53(4): 784—805 (in Chinese).
[24]	孙强, 王涛. 2020. 淄博及邻区活动断裂地震危险性评估[J]. 四川地震, (1): 16—23.
	SUN Qiang, WANG Tao. 2020. Seismic hazard assessment of active faults in Zibo city and its adjacent area[J]. Earthquake Research in Sichuan, (1): 16—23 (in Chinese).
[25]	孙瑛杰, 卢演俦, 尹功明. 1999. 沂沭断裂带大水场剖面断层泥的ESR年代学研究[J]. 地震地质, 21(4): 346—350.
	SUN Ying-jie, LU Yan-chou, YIN Gong-ming. 1999. A study on ESR dating for the Dashuichang gouge profile of the Yishu fault zone[J]. Seismology and Geology, 21(4): 346—350 (in Chinese).
[26]	田婷婷, 吴中海, 张克旗, 等. 2013. 第四纪主要定年方法及其在新构造与活动构造研究中的应用综述[J]. 地质力学学报, 19(3): 242—266.
	TIAN Ting-ting, WU Zhong-hai, ZHANG Ke-qi, et al. 2013. Overview of Quaternary dating methods and their application in neotectonics and active tectonics research[J]. Journal of Geomechanics, 19(3): 242—266 (in Chinese).
[27]	田同亮. 2020. 山东省沂源县中—新生代盆地成生、演化作用讨论[J]. 西部探矿工程, 32(7): 177—180, 183.
	TIAN Tong-liang. 2020. The discussion on the genesis and evolution of the Mesozoic-Cenozoic Basin in Yiyuan County, Shandong Province[J]. West-China Exploration Engineering, 32(7): 177—180, 183 (in Chinese).
[28]	万天丰. 1995. 郯庐断裂带的演化与古应力场[J]. 地球科学, 20(5): 526—534.
	WAN Tian-feng. 1995. Evolution of Tancheng-Lujiang Fault zone and paleostress fields[J]. Earth Science, 20(5): 526—534 (in Chinese).
[29]	王华林. 1995. 山东青州地震研究与地震区划[M]. 北京: 地震出版社.
	WANG Hua-lin. 1995. Earthquake Research and Earthquake Zoning in Qingzhou, Shandong[M]. Seismological Press, Beijing (in Chinese).
[30]	王纪强, 王冬雷, 鹿子林, 等. 2020. 双山-李家庄断裂地表破裂特征与最新活动性研究[J]. 地震, 40(4): 115—128.
	WANG Ji-qiang, WANG Dong-lei, LU Zi-lin, et al. 2020. The surface rupture characteristics and latest activities of the Shuangshan-Lijiazhuang Fault[J]. Earthquake, 40(4): 115—128 (in Chinese).
[31]	王金辉. 2004. 遥感技术在潍坊地区活动断裂研究中的应用[D]. 青岛: 山东科技大学.
	WANG Jin-hui. 2004. Application of remote sensing image information in the research of active faults in Weifang district[D]. Shandong University of Science and Technology, Qingdao (in Chinese).
[32]	王雷. 2016. 活动断裂带断层泥纳微米尺度的特征研究[D]. 廊坊: 防灾科技学院.
	WANG Lei. 2016. Research on the characteristics of active fault gouges at the nano/micro scale[D]. Institute of Disaster Prevention, Langfang (in Chinese).
[33]	王雷, 任治坤, 何仲太, 等. 2024. 天山内部那拉提断裂带全新世活动证据[J]. 地震地质, 46(4): 821—836. doi: 10.3969/j.issn.0253-4967.2024.04.004.
	WANG Lei, REN Zhi-kun, HE Zhong-tai, et al. 2024. Evidence of Holocene activity of Nalati fault zone within the Tianshan[J]. Seismology and Geology, 46(4): 821—836 (in Chinese).
[34]	王先美, 钟大赉, 王毅. 2008. 鲁西NW向断裂系晚中生代活动的几何学、运动学及年代学研究[J]. 地质学报, 82(9): 1258—1273.
	WANG Xian-mei, ZHONG Da-lai, WANG Yi. 2008. Geometry, kinematics and thermochronology study of the late Mesozoic movement of NW-trending faults, western Shandong[J]. Acta Geologica Sinica, 82(9): 1258—1273 (in Chinese).
[35]	王志才, 贾荣光, 孙昭民, 等. 2005. 沂沭断裂带安丘-莒县断裂安丘—朱里段几何结构与活动特征[J]. 地震地质, 27(2): 212—220.
	WANG Zhi-cai, JIA Rong-guang, SUN Zhao-min, et al. 2005. Geometry and activity of the Anqiu-Zhuli segment of the Anqiu-Juxian Fault in the Yishu fault zone[J]. Seismology and Geology, 27(2): 212—220 (in Chinese).
[36]	王志才, 石荣会, 晁洪太, 等. 2001. 鲁中南隆起区第四纪晚期断裂活动特征[J]. 海洋地质与第四纪地质, 21(4): 95—102.
	WANG Zhi-cai, SHI Rong-hui, CHAO Hong-tai, et al. 2001. Characteristics of the Quaternary fault activities in the middle and south region of Shandong Province[J]. Marine Geology & Quaternary Geology, 21(4): 95—102 (in Chinese).
[37]	徐嘉炜, 朱光. 1995. 中国东部郯庐断裂带构造模式讨论[J]. 华北地质矿产杂志, 10(2): 121—134.
	XU Jia-wei, ZHU Guang. 1995. Discussion on tectonic models for the Tan-Lu fault zone, Eastern China[J]. Journal of Geology and Mineral Resources North China, 10(2): 121—134 (in Chinese).
[38]	徐杰, 周本刚, 计凤桔, 等. 2012. 华北渤海湾盆地区大震发震构造的基本特征[J]. 地震地质, 34(4): 618—636. doi: 10.3969/j.issn.0253-4967.2012.04.008.
	XU Jie, ZHOU Ben-gang, JI Feng-ju, et al. 2012. Features of seismogenic structures of great earthquakes in the Bohai Bay Basin area, North China[J]. Seismology and Geology, 34(4): 618—636 (in Chinese).
[39]	杨会丽. 2013. 地震相关快速沉积物释光测年研究[D]. 北京: 中国地震局地质研究所.
	YANG Hui-li. 2013. Optical dating research of rapidly deposited sediments related to earthquakes[D]. Institute of Geology, China Earthquake Administration, Beijing (in Chinese).
[40]	杨主恩, 胡碧茹, 杨继武. 1985. 红河和曲江断裂带断层泥的特征及其地震地质意义[J]. 地震地质, 7(1): 25—32.
	YANG Zhu-en, HU Bi-ru, YANG Ji-wu. 1985. The characteristics of gouge from Honghe and Qujiang fault zones and their seismogeological implications[J]. Seismology and Geology, 7(1): 25—32 (in Chinese).
[41]	余中元, 张培震, 闵伟, 等. 2016. 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, 38(4): 844—861. doi: 10.3969/j.issn.0253-4967.2016.04.004.
	YU Zhong-yuan, ZHANG Pei-zhen, MIN Wei, et al. 2003. Late Holocene active 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, 38(4): 844—861 (in Chinese).
[42]	袁仁茂, 张秉良, 徐锡伟, 等. 2013. 汶川地震北川-映秀断裂北段断层泥显微构造和黏土矿物特征及其意义[J]. 地震地质, 35(4): 685—700. doi: 10.3969/j.issn.0253-4967.2013.04.001.
	YUAN Ren-mao, ZHANG Bing-liang, XU Xi-wei, et al. 2013. Microstructural features and mineralogy of clay-rich fault gouge at the northern segment of the Yingxiu-Beichuan Fault, China[J]. Seismology and Geology, 35(4): 685—700 (in Chinese).
[43]	袁仁茂, 张秉良, 徐锡伟, 等. 2014. 汶川地震剪切滑动面微-纳米级颗粒的特征、形成机制及地震意义[J]. 中国科学(D辑), 44(8): 1821—1832.
	YUAN Ren-mao, ZHANG Bing-liang, XU Xi-wei, et al. 2014. Features and genesis of micro-nanometer-sized grains on shear slip surface of the 2008 Wenchuan earthquake[J]. Science China: Earth Sciences, 44(8): 1821—1832 (in Chinese).
[44]	张克旗, 吴中海, 吕同艳, 等. 2015. 光释光测年法——综述及进展[J]. 地质通报, 34(1): 183—203.
	ZHANG Ke-qi, WU Zhong-hai, LÜ Tong-yan, et al. 2015. Review and progress of OSL dating[J]. Geological Bulletin of China, 34(1): 183—203 (in Chinese).
[45]	张培震, 闵伟, 邓起东, 等. 2003. 海原活动断裂带的古地震与强震复发规律[J]. 中国科学(D辑), 33(8): 705—713.
	ZHANG Pei-zhen, MIN Wei, DENG Qi-dong, et al. 2003. The law of ancient earthquake and strong earthquake recurrence in the Haiyuan active fault zone[J]. Science in China(Ser D), 33(8): 705—713 (in Chinese).
[46]	张岳桥, 董树文. 2008. 郯庐断裂带中生代构造演化史: 进展与新认识[J]. 地质通报, 127(9): 1371—1390.
	ZHANG Yue-qiao, DONG Shu-wen. 2008. Mesozoic tectonic evolution history of the Tan-Lu fault zone, China: Advances and new understanding[J]. Geological Bulletin of China, 127(9): 1371—1390 (in Chinese).
[47]	郑朗荪, 高维明, 郑传贝. 1988. 郯庐断裂带的分段与沂沭断裂的活动性[J]. 中国地震, 4(3): 129—135.
	ZHENG Lang-sun, GAO Wei-ming, ZHENG Chuan-bei. 1988. Characteristics of various segments in the Tanlu zone and activities of the Yishu Fault[J]. Earthquake Research in China, 4(3): 129—135 (in Chinese).
[48]	周本刚, 沈得秀. 2006. 地震安全性评价中若干地震地质问题探讨[J]. 震灾防御技术, 1(2): 113—120.
	ZHOU Ben-gang, SHEN De-xiu. 2006. Discussion on some geological problems in earthquake safety evaluation[J]. Technology for Earthquake Disaster Prevention, 1(2): 113—120 (in Chinese).
[49]	邹俊杰, 何宏林, 耿爽, 等. 2022. 三维激光扫描技术与断层面形貌量化分析在基岩区古地震研究中的应用[J]. 震灾防御技术, 17(1): 56—67.
	ZOU Jun-jie, HE Hong-lin, GENG Shuang, et al. 2022. Application of 3D Laser Scanning and Quantitative morphology analysis method to bedrock fault surface in paleo-seismic research in bedrock area[J]. Technology for Earthquake Disaster Prevention, 17(1): 56—67 (in Chinese).
[50]	Giaccio B, Galadini F, Sposato A, et al. 2003. Image processing and roughness analysis of exposed bedrock fault planes as a tool for paleoseismological analysis: Results from the Campo Felice Fault(central Apennines, Italy)[J]. Geomorphology, 49(3-4): 281—301.
[51]	Goodall H, Gregory L C, Wedmore L N J, et al. 2021. Determining histories of slip on normal faults with bedrock scarps using cosmogenic nuclide exposure data[J]. Tectonics, 40(3): e2020TC006457.
[52]	Jones R R, Kokkalas S, McCaffrey K J W. 2009. Quantitative analysis and visualization of nonplanar fault surfaces using terrestrial laser scanning(LiDAR): The Arkitsa Fault, Central Greece, as a case study[J]. Geosphere, 5(6): 465—482.
[53]	Kuo L W, Song S R, Yeh E C, et al. 2009. Clay mineral anomalies in the fault zone of the Chelungpu Fault, Taiwan, and their implications[J]. Geophysical Research Letters, 36(18).
[54]	Li X N, Hammond W C, Pierce I K D, et al. 2023. Present-day strike-slip faulting and intracontinental deformation of North China: Constraints from improved GPS observations[J]. Geochemistry, Geophysics, Geosystems, 24(7): e2022GC010781.
[55]	Ma K F, Tanaka H, SONG S R, et al. 2006. Slip zone and energetics of a large earthquake from the Taiwan Chelungpu-fault Drilling Project[J]. Nature, 444(7118): 473—476.
[56]	McCalpin J. 2009. Paleoseismology(2nd ed)[M]. Academic Press, Burlington.
[57]	Oskin M E, Arrowsmith J R, Corona A H, et al. 2012. Near-field deformation from the EI Mayor-cucapah earthquake revealed by differential LiDAR[J]. Science, 335(6069): 702—705.
[58]	Ren Z K, Zielke O, Yu J X. 2018. Active tectonics in 4D high-resolution[J]. Journal of Structural Geology, 117: 264—271.
[59]	Su P, He H L, Tan X B, et al. 2021. Initiation and evolution of the Shanxi Rift System in North China: Evidence from low-temperature thermochronology in a plate reconstruction framework[J]. Tectonics, 40: e2020TC006298.
[60]	Wang L, Wang Z C, Chao H T, et al. 2021. Characteristics and implications of nanocoatings on gouges in a seismically active fault zone[J]. Journal of Nanoscience and Nanotechnology, 21(1): 707—714.
[61]	Wu C Y, Ren G X, Yu J X, et al. 2020. Oblique right-lateral faulting along the northern margin of the Ili Basin in the northern Tian Shan, northwest China[J]. Tectonics, 39: e2020TC006061.
[62]	Xu X W, Ma X Y. 1992. Geodynamics of the Shanxi rift system, China[J]. Tectonophysics, 28: 325—340.
[63]	Zhang Y G, Zheng W J, Wang Y J, et al. 2018. Contemporary deformation of the North China Plain from global positioning system data[J]. Geophysical Research Letters, 45(4): 1851—1859.

THE LATE QUATERNARY ACTIVITY CHARACTERISTICS OF THE MIDDLE-NORTHERN SECTION OF THE SHANGWUJING FAULT IN THE LUXI BLOCK

鲁西上五井断裂中北段晚第四纪活动特征

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