鲁西上五井断裂中北段晚第四纪活动特征

doi:10.3969/j.issn.0253-4967.20250065

地震地质 ›› 2026, Vol. 48 ›› Issue (1): 1-18.DOI: 10.3969/j.issn.0253-4967.20250065

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

收稿日期:2025-03-11 修回日期:2025-06-05 出版日期:2026-02-20 发布日期:2026-03-14
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)

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

摘要/Abstract

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

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

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.

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.

图/表 9

图1 研究区附近地震构造略图

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

表1 上五井断裂露头年代样品数据

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

图2 研究区上五井断裂展布 a 谷歌影像; b 分辨率为12.5m的DEM数据; c 文中机载雷达获取的高分辨率DEM数据

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

图3 九杰村南上五井断裂的地质地貌 a 机载雷达获取的高分辨率DEM数据; b、 c 九杰村南上五井断裂的地貌; d 九杰村南上五井断裂的地质露头; e 上五井断裂滑动擦痕; f 擦痕, 图e的局部放大

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

图4 崔木村东上五井断裂的地质地貌 a 机载雷达获取的高分辨率DEM数据; b 崔木村东上五井断裂的地貌

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

图5 东流水村西上五井断裂地貌 a 机载雷达获取的高分辨率DEM数据; b 东流水村西上五井断裂的地貌照片; c 东流水村西上五井断裂的地貌解译; d 基于LaDiCaoz程序测量的冲沟位错; e 位错恢复; f 冲沟位置示意图; g 冲沟位错的拟合值

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

图6 九杰村南上五井断裂的地质剖面 a 断层带照片; b 断层泥带照片; c 断层泥局部放大照片, 可见水平擦痕; d 断层带剖面, 断层泥ESR测年结果为(188±17)kaBP

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

图7 崔木村东上五井断裂的地质剖面 a 断层破碎带的照片; b 断层破碎带露头的地质剖面; c 断层泥带, 图a的局部放大, 由SE向NW分别为黄绿色断层泥、灰白色断层泥、紫红色断层泥和黄色断层泥, 红色方块为断层泥采样位置

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

图8 晚第四纪鲁西地块东缘断裂的构造格局 a 华北地区的走滑作用和运动模式示意图, 修改自Li等(2023); b 鲁西地块东缘断裂分布图, 大地电磁资料引自罗旭(2016); c 鲁西地块东缘断裂的平面图和运动模式

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

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鲁西上五井断裂中北段晚第四纪活动特征

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

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