沂沭断裂带北段东支断裂的浅部构造特征及活动性
|
摘要
沂沭断裂带北段即潍坊市朱里以北的隐伏构造区,其主要隐伏活动断裂对第四系的发育具有控制作用。沂沭断裂带的活动性具有东强西弱的特点,其东支主干断裂是新构造运动强活动带,对地震的发生具有控制作用。莱州湾地区所开展的1∶5万区域地质调查、工程地质调查,通过大量的地面调查、物探、钻探等工作,对沂沭断裂带北段安丘-莒县断裂、昌邑-大店断裂的空间分布及活动性进行了深入调查研究,结果表明:两条主干断裂呈NNE向大致平行展布延伸,进入莱州湾海域,其中昌邑-大店断裂活动性质表现为走滑为主兼具逆冲运动,倾角近直立,倾向大致以东冢村北为界,由南段的倾向东转为北段的倾向西,该断裂最晚活动时代为晚更新世。安丘-莒县断裂控制了新生代地层的空间分布,新生代以来活动方式以向西正断为主,错断全新世地层并造成地表建筑物的开裂,目前仍处于活动期。本次调查首次确定了昌邑潜凸起的存在,该凸起位于断裂带北段东支两条主断裂之间,凸起区第四系厚度明显变薄,局部基岩出露;以柳疃断裂为界,北段潜凸区第四系下伏地层为新近纪明化镇组、馆陶组;南段潜凸区第四系下伏地层为新近纪八亩地组、牛山组,古近纪朱碧店组和白垩纪红土崖组。昌邑潜凸起区的发现对于莱州湾南岸水文地质、工程地质调查研究工作具有重要意义。
The northern segment of the Yishu fault zone refers to the concealed tectonic area which distributes to the north of Juli, Weifang city, and its main concealed active faults play a controlling role in the development of the Quaternary System. The east segments of the Yishu fault zone are more active than the west segments. The main east branch fault is a strong activity zone of the new tectonic movement, which has a controlling effect on the occurrence of earthquakes. The spatial distribution and activity of the Anqiu-Juxian fault and the Changyi-Dadian fault of the northern segment of the Yishu fault zone were investigated through ground investigation, geophysical prospecting and drilling by the 1∶50000 regional geological survey and engineering geological survey programs carried out in the Laizhou Bay Area. The results show that the two main faults have roughly parallel distribution of NNE direction, extending into the Laizhou Bay Area. The activity of the Changyi-Dadian fault is dominated by strike-slip, together with thrust motion, and the fault dip angles are nearly vertical. The fault dip of the Changyi-Dadian fault changes at the north of the Dongzhong village, which shifts from east at the south part of the fault to west at the north part. The latest activity age of the fault is the late Pleistocene. The Anqiu-Juxian fault controls the spatial distribution of the Cenozoic strata, and is mainly west dipping normal fault since the Cenozoic Era. The fault breaks the Holocene strata significantly and causes the cracking of the surface buildings, which indicates that the fault is a Holocene active fault and is still active at present. The geological survey of this time firstly confirms the existence of the Changyi Salient, which is located between the two main east branch faults in the northern part of the fault zone. The Quaternary thickness of the salient area is thinner significantly, and the bedrock is exposed at some area. Divided by the Liutuan fault, the Quaternary underlying strata of the north part of the salient are the Minghuazhen Formation and the Guantao Formation of the Neogene, and the underlying strata of the south part of the salient are the Bamudi Formation, the Niushan Formation of the Neogene, Zhubidian Formation of the Paleogene and the Hongtuya Formation of the Cretaceous. The discovery of the Changyi Salient is of great significance to the investigation and study of hydrogeological and engineering geology in the south coast of the Laizhou Bay.
The northern segment of the Yishu fault zone refers to the concealed tectonic area which distributes to the north of Juli, Weifang city, and its main concealed active faults play a controlling role in the development of the Quaternary System. The east segments of the Yishu fault zone are more active than the west segments. The main east branch fault is a strong activity zone of the new tectonic movement, which has a controlling effect on the occurrence of earthquakes. The spatial distribution and activity of the Anqiu-Juxian fault and the Changyi-Dadian fault of the northern segment of the Yishu fault zone were investigated through ground investigation, geophysical prospecting and drilling by the 1∶50000 regional geological survey and engineering geological survey programs carried out in the Laizhou Bay Area. The results show that the two main faults have roughly parallel distribution of NNE direction, extending into the Laizhou Bay Area. The activity of the Changyi-Dadian fault is dominated by strike-slip, together with thrust motion, and the fault dip angles are nearly vertical. The fault dip of the Changyi-Dadian fault changes at the north of the Dongzhong village, which shifts from east at the south part of the fault to west at the north part. The latest activity age of the fault is the late Pleistocene. The Anqiu-Juxian fault controls the spatial distribution of the Cenozoic strata, and is mainly west dipping normal fault since the Cenozoic Era. The fault breaks the Holocene strata significantly and causes the cracking of the surface buildings, which indicates that the fault is a Holocene active fault and is still active at present. The geological survey of this time firstly confirms the existence of the Changyi Salient, which is located between the two main east branch faults in the northern part of the fault zone. The Quaternary thickness of the salient area is thinner significantly, and the bedrock is exposed at some area. Divided by the Liutuan fault, the Quaternary underlying strata of the north part of the salient are the Minghuazhen Formation and the Guantao Formation of the Neogene, and the underlying strata of the south part of the salient are the Bamudi Formation, the Niushan Formation of the Neogene, Zhubidian Formation of the Paleogene and the Hongtuya Formation of the Cretaceous. The discovery of the Changyi Salient is of great significance to the investigation and study of hydrogeological and engineering geology in the south coast of the Laizhou Bay.
引文
Chao Hongtai, Li Jialing, Zhao Qingyu, Cui Zhaowen. 1998. Active folds in the Yishu fault zone and their relations to active faults. Journal of Seismological Research, 21(3): 261～267. (in Chinese with English abstract)
Chao Hongtai, Deng Qidong, Li Jialing, Wang Zhicai, Man Hongmin. 2001. Deformation styles of unconsolidated Quaternary sediments on active faults. Seismology and Geology, 23(3):399～406. (in Chinese with English abstract)
Chao Hongtai, Yu Shen’e, Li Jialing, Wang Qi, Wang Zhicai. 2001. Research on active faults in the Shandong Peninsula. Seismological Research of Northeast China, 17(4): 2～8. (in Chinese with English abstract)
Ding Guoyu. 1990. The inhomogeneity of faulting in Holocene. Earthquake Research in China, 6(1): 1～9. (in Chinese with English abstract)
Fan Jun,Zhai Zhenghong, Guan Yanxin, Liu Shiyou, Li Dongliang, Xiong Wei. 2015. Spatial location and activity research on the north section of Anqiu-Juxian fault and Changyi-Dadian fault from Zhuli. North China Earthquake Sciences, 33(1): 39～45. (in Chinese with English abstract)
Fang Zhongjing, Ji Fengju, Xiang Hongfa, Ding Menglin. 1976. The characteristics of Quaternary movements along the middle segment of the old Tancheng-Lujiang fracture-zone and their seismogeologic conditions. Scientia Geologica Sinica, (4): 354～365. (in Chinese with English abstract)
Fang Zhongjing, Ding Menglin, Xiang Hongfa, Ji Fengju, Li Rucheng. 1986. The basic characteristics of the Tanlu Fault Zone. Chinese Science Bulletin, (1):52～55. (in Chinese without English abstract)
Gao Zhanwu, Xu Jie, Zhao Tiehu, Zhang Jin, Ji Fengju, Zhou Bengang. 2017. Re-cognition of the neotectonics and activities of the Yingkou-Weifang fault zone. Seismology and Geology, 39(1): 43～53. (in Chinese with English abstract)
Hou Jianhua, Ren Tianlong, Zhu Xueqiang, Liu Yin, Huang Yongbo, Yang Shipeng. 2015. Preliminary study on new tectonic activity of Zhuli section of Anqiu-Juxian fault in Shandong Province. Geological Review, 61(Supplement): 647～650. (in Chinese without English abstract)
Hu Wei, ZhuGuang, Song Lihong, Yan Lejia, Liu Bei. 2013. Analysis of Quaternary activity along the Bohai segment of the Tan-Lu fault zone. Earth Science Frontiers, 20(4): 137～150. (in Chinese with English abstract)
Jiang Wenliang, ZhangJingfa, Chen Ding, Lu Xiaocui, Zhang Peng, Li Limei. 2011. Tectonic characteristics of Su-Lu segment of the Tan-Lu fault zone derived from RS and gravity multi-source information. Acta Geoscientica Sinica, 32(2): 143～153. (in Chinese with English abstract)
Li Jialing, ChaoHongtai, Cui Zhaowen, Zhao Qingyu. 1994. Segmentation of active fault along the Tancheng-Lujiang fault zone and evaluation of strong earthquake risk. Seismology and Geology, 16(2): 121～126. (in Chinese with English abstract)
Liu Bei, Zhu Guang, Hu Honglei, Song Lihong. 2015. Analysis on new tectonic activity of the Jiangsu part of the Tan-Lu fault zone. Acta Geologica Sinica, 89(8):1352～1366. (in Chinese with English abstract)
Li Xishuang, Zhao Yuexia, Liu Baohua, Liu Chenguang, Pei Yanliang, Han Guozhong, Hua Qingfeng. 2010a. Structural deformation and fault activity of the Tan-Lu Fault zone in the Bohai Sea since the Late Pleistocene. Chinese Science Bulletin, 55(8): 684～692.
Li Xishuang, Liu Baohua, Zhao Yuexia, Liu Chenguang, Wu Jingung. 2010b. Late Pleistocene-Holocene submarine active structures in the Bohai Sea. Acta Oceanologica Sinica, 32(5):52～59. (in Chinese with English abstract)
Song Fangmin, Yang Xiaoping, He Honglin, Li Chuanyou, Zhang Lanfeng. 2005. Quantitative analysis of recent activity of the Xiaodianzi-Maobu segment of the Anqiu-Juxian fault, Shangdong Province. Seismology and Geology, 27(2): 200～211. (in Chinese with English abstract)
Tang Xingong, Chen Yongshun, Tang Zhe. 2006. Bouguer gravity study of middle section of Tanlu fault. Acta Seismologica Sinica, 28(6):603～610. (in Chinese with English abstract)
Wan Guimei, Tang Liangjie, Jin Wenzheng, Yu Yixin. 2009. Progresses and problems in the study of Tancheng-Lujiang fault zone. Geological Review,55(2):251～259. (in Chinese with English abstract)
Wang Yingbin, Huang Lei. 2013. Distribution characteristic of the Ying-Wei fault zone offshore the Bohai Sea and Cenozoic basin-controlling model. Acta Geologica Sinica, 87(12):1811～1818. (in Chinese with English abstract)
Wang Xin, ZhangJingfa, Fu Pingjie, Gao Min. 2015. Deep structures of Yishu fault zone derived from gravity data. Seismology and Geology, 37(3): 731～746. (in Chinese with English abstract)
Wang Xin, ZhangJingfa, Jiang Wenliang, Gao Min, Fu Pingjie. 2015. Deep structures of Jiangsu segment of Tan-Lu fault zone derived from bouguer gravity data. Progress in Geophysics, 30(4): 1516～1525. (in Chinese with English abstract)
Wang Yuye, Zhu Xueqiang, Ren Tianlong, Tao Youbing, Zhang Zhigang, Guo Jing. 2017. Significance of Holocene activity on the north part of Yishu fault. Shandong Land and Resources, 33(4): 1～5. (in Chinese with English abstract)
Wang Zhicai, Jia Rongguang, Sun Shaomin, Shi Ronghui, Chao Hongtai. 2005. Geometry and activity of the Anqiu-Zhuli segment of the Anqiu-Juxian fault in the Yishu fault zone. Seismology and Geology, 27(2): 212～220. (in Chinese with English abstract)
Wang Zhicai, Deng Qidong, Du Xianrong, Chao Hongtai, Wu Ziquan, Xiao Lanxi, Sun Shaomin, Min Wei, Ling Hong, Yang Xihai, Li Changchuan. 2006. Active fault survey on the Tanlu fault zone in Laizhou Bay. Acta Seismologica Sinica, 28(5): 493～503. (in Chinese with English abstract)
Wei Guangxing, Diao Shouzhong, Zhou Cuiying. 1993. Study of Seismicity along the Tancheng-Lujang Seismic Zone. Beijing: Seismological Press. (in Chinese)
Wu Shiguo, Yu Zhaohua, Zou Dongbo, Zhang Haiying. 2006. Structural features and Cenozoic evolution of the Tan-Lu fault zone in the Laizhou Bay, Bohai Sea. Marine Geology & Quaternary Geology, 26(6): 101～110. (in Chinese with English abstract)
Xiang Hongfa, Fang Zhongjing, Zhang Wanxia, Jia Sanfa, Li Rucheng. 1994. Integrated investigation and study on buried faults of plain area. Seismological Committee, Seismological Society of China. Study on active faults in China. Seismological Press, 205～214. (in Chinese with English abstract)
Xu Jianguo, Xu Hua, Zhang Tao, Zhang Zhuo, Qi Xiaofan, Ji Wenlong. 2018. Stratigraphic characteristics age and indicated Holocene coastal variation of Heituhu Formation in Laizhou Bay coastal area, Shandong Peninsula. Acta Geoscientica Sinica, 29(2): 133～143. (in Chinese with English abstract)
Yan Lejia, Zhu Guang, Lin Shaoze, Zhaotian. 2014. Neotectonic activity and formation mechanism of the Yishu Fault Zone. Science China: Earth Sciences, 44(7): 1452～1467. (in Chinese with English abstract)
Yang Yichong. 1993. Segmentation characteristics of Yishu active faults and seismic tendency prediction. Earthquake, 1:45～48. (in Chinese with English abstract)
Zhang Peng, WangLiangshu, Shi Huosheng, Li Limei, Tan Huiming. 2010. The Mesozoic-Cenozoic tectonic evolution of the Shandong segment of the Tan-Lu fault zone. Acta Geologica Sinica, 84(9):1316～1323. (in Chinese with English abstract)
Zhao Dasheng, Xiao Zengyue, Wang Yifen. 1983. Petrological characteristics and genesis of the Cenozoic volcanic rocks in Tancheng-Lujiang fault belt and the adjacent areas. Acta Geologica Sinica, 2:128～141. (in Chinese with English abstract)
Zheng Langsun, Gao Weiming, Zheng Chuanbei. 1988. Division of Tan-Lu fault zone and activity of Yishu fault. Earthquake Research in China, 4(3): 123～129. (in Chinese with English abstract)
Zhou Bin, DengZhihui, Chao Hongtai, Xu Huaming, Yang Zhuzhuan, Xiao Lanxi, Wang Zhicai, Zhang Yongxiang. 2008. Strike-slip tectonic characteristics evolution and dynamic mechanism of Yingwei fault zone. Northwestern Seismological Journal, 30(2): 117～121. (in Chinese with English abstract)
晁洪太,李家灵,赵清玉,崔昭文.1998. 沂沭断裂带活动褶皱及其与活动断层的关系. 地震研究,21(3):261～267.
晁洪太,邓起东,李家灵,王志才,满洪敏.2001. 活动断裂带内第四纪松散沉积物的变形类型. 地震地质,23(3):399～406.
晁洪太,于慎谔,李家灵,王錡,王志才.2001. 山东半岛地区活断层研究. 东北地震研究,17(4):2～8.
丁国瑜.1990. 全新世断层活动的不均匀性. 中国地震,6(1):1～9.
范军,翟正宏,管延新,刘世友,李栋梁,熊玮. 2015. 安丘—莒县断裂与昌邑-大店断裂朱里以北段空间位置及活动性研究. 华北地震科学,33(1):39～45.
方仲景,计凤桔,向宏发,丁梦麟. 1976. 郯庐带中段第四纪断裂活动特征与地震地质条件述评. 地质科学,(4):354～365.
方仲景,丁梦麟,向宏发,计凤桔,李如成. 1986. 郯庐断裂带的基本特征. 科学通报,(1):52～55.
高战武,徐杰,赵铁虎,张进,计凤桔,周本刚. 2017. 营口—潍坊断裂带新构造和新构造活动的再认识. 地震地质,39(1):43～53.
国家地震局地质研究所. 1987. 郯庐断裂. 北京: 地震出版社.
侯建华,任天龙,朱学强,刘银,黄永波,杨仕鹏. 2015. 山东安丘—莒县断裂朱里段新构造活动初探. 地质论评,61(增刊):647～650.
胡惟,朱光,宋利宏,严乐佳,刘备. 2013. 郯庐断裂带渤海段第四纪活动规律探讨. 地学前缘,20(4):137～150.
姜文亮,张景发,陈丁,路晓翠,张鹏,李丽梅. 2011. 利用遥感、重力多源信息研究郯—庐断裂带苏—鲁段构造特征. 地球学报,32(2):143～153.
李家灵,晁洪太,崔昭文,赵清玉. 1994. 郯庐活断层的分段及其大震危险性分析. 地震地质,16(2):121～126.
李西双,赵月霞,刘宝华,刘晨光,裴彦良,韩国忠,华清峰. 2010a.郯庐断裂带渤海段晚更新世以来的浅层构造变形和活动性. 科学通报,55(8):684～692.
李西双,刘宝华,赵月霞,刘晨光,吴金光. 2010b.渤海海域晚更新世—全新世的活动构造. 海洋学报,32(5):52～59.
刘备,朱光,胡红雷,宋利宏. 2015. 郯庐断裂带江苏段新构造活动规律分析. 地质学报,89(8):1352～1366.
宋方敏,杨晓平,何宏林,李传友,张兰凤. 2005. 山东安丘—莒县断裂小店子—茅埠段新活动及其定量研究. 地震地质,27(2):200～211.
郯庐活动断裂带地质填图课题组. 2013. 郯庐活动断裂带地质图(1∶50000)说明书. 北京: 地震出版社.
唐新功,陈永顺,唐哲. 2006. 应用布格重力异常研究郯庐断裂构造. 地震学报,28(6):603～610.
万桂梅,汤良杰,金文正,余一欣. 2009. 郯庐断裂带研究进展及存在问题探讨. 地质论评,55(2):251～259.
王应斌,黄雷. 2013. 渤海海域营潍断裂带展布特征及新生代控盆模式. 地质学报,87(12):1811～1818.
王鑫,张景发,付萍杰,高敏. 2015. 沂沭断裂带重力场及地壳结构特征. 地震地质. 37(3):731～746.
王鑫,张景发,姜文亮,高敏,付萍杰. 2015. 基于布格重力数据研究郯庐断裂带江苏段深部构造. 地球物理学进展. 30(4):1516～1525.
王志才,贾荣光,孙昭民,石荣会,晁洪太. 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. 地震地质. 27(2):212～220.
王志才,邓起东,杜宪宋,晁洪太,吴子泉,肖兰喜,孙昭民,闵伟,凌宏,杨希海,李长川. 2006. 莱州湾海域郯庐断裂带活断层探测. 地震学报. 28(5):493～503.
魏光兴,刁守中,周翠英. 郯庐带地震活动性研究. 1993. 北京:地震出版社.
吴时国,余朝华,邹东波,张海英.2006. 莱州湾地区郯庐断裂带的构造特征及其新生代演化. 海洋地质与第四纪地质,26(6):101～110.
向宏发,方仲景,张晚霞,贾三发,李如成. 1994. 平原区隐伏断裂的综合探测研究.见:中国地震学会地震专业委员会编. 中国活动断层研究. 北京:地震出版社,205～214.
徐建国,徐华,张涛,张卓,祁晓凡,纪汶龙. 2018.山东半岛莱州湾滨海地区黑土湖组地层特征、时代及指示的全新世海岸带变化. 地球学报,29(2):133～143.
严乐佳,朱光,林少泽,赵田. 2014. 沂沭断裂带新构造活动规律与机制. 中国科学:地球科学,44(7):1452～1467.
杨一冲. 1993. 沂沭活断层分段特征及地震趋势的预测. 地震,1:45～48.
张鹏,王良书,石火生,李利梅,谭慧明. 2010. 郯庐断裂带山东段的中新生代构造演化特征. 地质学报,84(9):1316～1323.
赵大升,肖增岳,王艺芬. 1983. 郯庐断裂带及其邻近地区新生代火山岩岩石特征及成因探讨. 地质学报,2:128～141.
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. 中国地震,4(3):123～129.
周斌,邓志辉,晁洪太,许华明,杨竹转,肖兰喜,王志才,张永祥. 2008. 营潍断裂带走滑构造特征、演化及动力学机制. 西北地震学报,30(2):117～121.
? 山东省国土资源厅. 2014. 山东省地层侵入岩构造单元划分方案(未出版).
Chao Hongtai, Deng Qidong, Li Jialing, Wang Zhicai, Man Hongmin. 2001. Deformation styles of unconsolidated Quaternary sediments on active faults. Seismology and Geology, 23(3):399～406. (in Chinese with English abstract)
Chao Hongtai, Yu Shen’e, Li Jialing, Wang Qi, Wang Zhicai. 2001. Research on active faults in the Shandong Peninsula. Seismological Research of Northeast China, 17(4): 2～8. (in Chinese with English abstract)
Ding Guoyu. 1990. The inhomogeneity of faulting in Holocene. Earthquake Research in China, 6(1): 1～9. (in Chinese with English abstract)
Fan Jun,Zhai Zhenghong, Guan Yanxin, Liu Shiyou, Li Dongliang, Xiong Wei. 2015. Spatial location and activity research on the north section of Anqiu-Juxian fault and Changyi-Dadian fault from Zhuli. North China Earthquake Sciences, 33(1): 39～45. (in Chinese with English abstract)
Fang Zhongjing, Ji Fengju, Xiang Hongfa, Ding Menglin. 1976. The characteristics of Quaternary movements along the middle segment of the old Tancheng-Lujiang fracture-zone and their seismogeologic conditions. Scientia Geologica Sinica, (4): 354～365. (in Chinese with English abstract)
Fang Zhongjing, Ding Menglin, Xiang Hongfa, Ji Fengju, Li Rucheng. 1986. The basic characteristics of the Tanlu Fault Zone. Chinese Science Bulletin, (1):52～55. (in Chinese without English abstract)
Gao Zhanwu, Xu Jie, Zhao Tiehu, Zhang Jin, Ji Fengju, Zhou Bengang. 2017. Re-cognition of the neotectonics and activities of the Yingkou-Weifang fault zone. Seismology and Geology, 39(1): 43～53. (in Chinese with English abstract)
Hou Jianhua, Ren Tianlong, Zhu Xueqiang, Liu Yin, Huang Yongbo, Yang Shipeng. 2015. Preliminary study on new tectonic activity of Zhuli section of Anqiu-Juxian fault in Shandong Province. Geological Review, 61(Supplement): 647～650. (in Chinese without English abstract)
Hu Wei, ZhuGuang, Song Lihong, Yan Lejia, Liu Bei. 2013. Analysis of Quaternary activity along the Bohai segment of the Tan-Lu fault zone. Earth Science Frontiers, 20(4): 137～150. (in Chinese with English abstract)
Jiang Wenliang, ZhangJingfa, Chen Ding, Lu Xiaocui, Zhang Peng, Li Limei. 2011. Tectonic characteristics of Su-Lu segment of the Tan-Lu fault zone derived from RS and gravity multi-source information. Acta Geoscientica Sinica, 32(2): 143～153. (in Chinese with English abstract)
Li Jialing, ChaoHongtai, Cui Zhaowen, Zhao Qingyu. 1994. Segmentation of active fault along the Tancheng-Lujiang fault zone and evaluation of strong earthquake risk. Seismology and Geology, 16(2): 121～126. (in Chinese with English abstract)
Liu Bei, Zhu Guang, Hu Honglei, Song Lihong. 2015. Analysis on new tectonic activity of the Jiangsu part of the Tan-Lu fault zone. Acta Geologica Sinica, 89(8):1352～1366. (in Chinese with English abstract)
Li Xishuang, Zhao Yuexia, Liu Baohua, Liu Chenguang, Pei Yanliang, Han Guozhong, Hua Qingfeng. 2010a. Structural deformation and fault activity of the Tan-Lu Fault zone in the Bohai Sea since the Late Pleistocene. Chinese Science Bulletin, 55(8): 684～692.
Li Xishuang, Liu Baohua, Zhao Yuexia, Liu Chenguang, Wu Jingung. 2010b. Late Pleistocene-Holocene submarine active structures in the Bohai Sea. Acta Oceanologica Sinica, 32(5):52～59. (in Chinese with English abstract)
Song Fangmin, Yang Xiaoping, He Honglin, Li Chuanyou, Zhang Lanfeng. 2005. Quantitative analysis of recent activity of the Xiaodianzi-Maobu segment of the Anqiu-Juxian fault, Shangdong Province. Seismology and Geology, 27(2): 200～211. (in Chinese with English abstract)
Tang Xingong, Chen Yongshun, Tang Zhe. 2006. Bouguer gravity study of middle section of Tanlu fault. Acta Seismologica Sinica, 28(6):603～610. (in Chinese with English abstract)
Wan Guimei, Tang Liangjie, Jin Wenzheng, Yu Yixin. 2009. Progresses and problems in the study of Tancheng-Lujiang fault zone. Geological Review,55(2):251～259. (in Chinese with English abstract)
Wang Yingbin, Huang Lei. 2013. Distribution characteristic of the Ying-Wei fault zone offshore the Bohai Sea and Cenozoic basin-controlling model. Acta Geologica Sinica, 87(12):1811～1818. (in Chinese with English abstract)
Wang Xin, ZhangJingfa, Fu Pingjie, Gao Min. 2015. Deep structures of Yishu fault zone derived from gravity data. Seismology and Geology, 37(3): 731～746. (in Chinese with English abstract)
Wang Xin, ZhangJingfa, Jiang Wenliang, Gao Min, Fu Pingjie. 2015. Deep structures of Jiangsu segment of Tan-Lu fault zone derived from bouguer gravity data. Progress in Geophysics, 30(4): 1516～1525. (in Chinese with English abstract)
Wang Yuye, Zhu Xueqiang, Ren Tianlong, Tao Youbing, Zhang Zhigang, Guo Jing. 2017. Significance of Holocene activity on the north part of Yishu fault. Shandong Land and Resources, 33(4): 1～5. (in Chinese with English abstract)
Wang Zhicai, Jia Rongguang, Sun Shaomin, Shi Ronghui, Chao Hongtai. 2005. Geometry and activity of the Anqiu-Zhuli segment of the Anqiu-Juxian fault in the Yishu fault zone. Seismology and Geology, 27(2): 212～220. (in Chinese with English abstract)
Wang Zhicai, Deng Qidong, Du Xianrong, Chao Hongtai, Wu Ziquan, Xiao Lanxi, Sun Shaomin, Min Wei, Ling Hong, Yang Xihai, Li Changchuan. 2006. Active fault survey on the Tanlu fault zone in Laizhou Bay. Acta Seismologica Sinica, 28(5): 493～503. (in Chinese with English abstract)
Wei Guangxing, Diao Shouzhong, Zhou Cuiying. 1993. Study of Seismicity along the Tancheng-Lujang Seismic Zone. Beijing: Seismological Press. (in Chinese)
Wu Shiguo, Yu Zhaohua, Zou Dongbo, Zhang Haiying. 2006. Structural features and Cenozoic evolution of the Tan-Lu fault zone in the Laizhou Bay, Bohai Sea. Marine Geology & Quaternary Geology, 26(6): 101～110. (in Chinese with English abstract)
Xiang Hongfa, Fang Zhongjing, Zhang Wanxia, Jia Sanfa, Li Rucheng. 1994. Integrated investigation and study on buried faults of plain area. Seismological Committee, Seismological Society of China. Study on active faults in China. Seismological Press, 205～214. (in Chinese with English abstract)
Xu Jianguo, Xu Hua, Zhang Tao, Zhang Zhuo, Qi Xiaofan, Ji Wenlong. 2018. Stratigraphic characteristics age and indicated Holocene coastal variation of Heituhu Formation in Laizhou Bay coastal area, Shandong Peninsula. Acta Geoscientica Sinica, 29(2): 133～143. (in Chinese with English abstract)
Yan Lejia, Zhu Guang, Lin Shaoze, Zhaotian. 2014. Neotectonic activity and formation mechanism of the Yishu Fault Zone. Science China: Earth Sciences, 44(7): 1452～1467. (in Chinese with English abstract)
Yang Yichong. 1993. Segmentation characteristics of Yishu active faults and seismic tendency prediction. Earthquake, 1:45～48. (in Chinese with English abstract)
Zhang Peng, WangLiangshu, Shi Huosheng, Li Limei, Tan Huiming. 2010. The Mesozoic-Cenozoic tectonic evolution of the Shandong segment of the Tan-Lu fault zone. Acta Geologica Sinica, 84(9):1316～1323. (in Chinese with English abstract)
Zhao Dasheng, Xiao Zengyue, Wang Yifen. 1983. Petrological characteristics and genesis of the Cenozoic volcanic rocks in Tancheng-Lujiang fault belt and the adjacent areas. Acta Geologica Sinica, 2:128～141. (in Chinese with English abstract)
Zheng Langsun, Gao Weiming, Zheng Chuanbei. 1988. Division of Tan-Lu fault zone and activity of Yishu fault. Earthquake Research in China, 4(3): 123～129. (in Chinese with English abstract)
Zhou Bin, DengZhihui, Chao Hongtai, Xu Huaming, Yang Zhuzhuan, Xiao Lanxi, Wang Zhicai, Zhang Yongxiang. 2008. Strike-slip tectonic characteristics evolution and dynamic mechanism of Yingwei fault zone. Northwestern Seismological Journal, 30(2): 117～121. (in Chinese with English abstract)
晁洪太,李家灵,赵清玉,崔昭文.1998. 沂沭断裂带活动褶皱及其与活动断层的关系. 地震研究,21(3):261～267.
晁洪太,邓起东,李家灵,王志才,满洪敏.2001. 活动断裂带内第四纪松散沉积物的变形类型. 地震地质,23(3):399～406.
晁洪太,于慎谔,李家灵,王錡,王志才.2001. 山东半岛地区活断层研究. 东北地震研究,17(4):2～8.
丁国瑜.1990. 全新世断层活动的不均匀性. 中国地震,6(1):1～9.
范军,翟正宏,管延新,刘世友,李栋梁,熊玮. 2015. 安丘—莒县断裂与昌邑-大店断裂朱里以北段空间位置及活动性研究. 华北地震科学,33(1):39～45.
方仲景,计凤桔,向宏发,丁梦麟. 1976. 郯庐带中段第四纪断裂活动特征与地震地质条件述评. 地质科学,(4):354～365.
方仲景,丁梦麟,向宏发,计凤桔,李如成. 1986. 郯庐断裂带的基本特征. 科学通报,(1):52～55.
高战武,徐杰,赵铁虎,张进,计凤桔,周本刚. 2017. 营口—潍坊断裂带新构造和新构造活动的再认识. 地震地质,39(1):43～53.
国家地震局地质研究所. 1987. 郯庐断裂. 北京: 地震出版社.
侯建华,任天龙,朱学强,刘银,黄永波,杨仕鹏. 2015. 山东安丘—莒县断裂朱里段新构造活动初探. 地质论评,61(增刊):647～650.
胡惟,朱光,宋利宏,严乐佳,刘备. 2013. 郯庐断裂带渤海段第四纪活动规律探讨. 地学前缘,20(4):137～150.
姜文亮,张景发,陈丁,路晓翠,张鹏,李丽梅. 2011. 利用遥感、重力多源信息研究郯—庐断裂带苏—鲁段构造特征. 地球学报,32(2):143～153.
李家灵,晁洪太,崔昭文,赵清玉. 1994. 郯庐活断层的分段及其大震危险性分析. 地震地质,16(2):121～126.
李西双,赵月霞,刘宝华,刘晨光,裴彦良,韩国忠,华清峰. 2010a.郯庐断裂带渤海段晚更新世以来的浅层构造变形和活动性. 科学通报,55(8):684～692.
李西双,刘宝华,赵月霞,刘晨光,吴金光. 2010b.渤海海域晚更新世—全新世的活动构造. 海洋学报,32(5):52～59.
刘备,朱光,胡红雷,宋利宏. 2015. 郯庐断裂带江苏段新构造活动规律分析. 地质学报,89(8):1352～1366.
宋方敏,杨晓平,何宏林,李传友,张兰凤. 2005. 山东安丘—莒县断裂小店子—茅埠段新活动及其定量研究. 地震地质,27(2):200～211.
郯庐活动断裂带地质填图课题组. 2013. 郯庐活动断裂带地质图(1∶50000)说明书. 北京: 地震出版社.
唐新功,陈永顺,唐哲. 2006. 应用布格重力异常研究郯庐断裂构造. 地震学报,28(6):603～610.
万桂梅,汤良杰,金文正,余一欣. 2009. 郯庐断裂带研究进展及存在问题探讨. 地质论评,55(2):251～259.
王应斌,黄雷. 2013. 渤海海域营潍断裂带展布特征及新生代控盆模式. 地质学报,87(12):1811～1818.
王鑫,张景发,付萍杰,高敏. 2015. 沂沭断裂带重力场及地壳结构特征. 地震地质. 37(3):731～746.
王鑫,张景发,姜文亮,高敏,付萍杰. 2015. 基于布格重力数据研究郯庐断裂带江苏段深部构造. 地球物理学进展. 30(4):1516～1525.
王志才,贾荣光,孙昭民,石荣会,晁洪太. 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. 地震地质. 27(2):212～220.
王志才,邓起东,杜宪宋,晁洪太,吴子泉,肖兰喜,孙昭民,闵伟,凌宏,杨希海,李长川. 2006. 莱州湾海域郯庐断裂带活断层探测. 地震学报. 28(5):493～503.
魏光兴,刁守中,周翠英. 郯庐带地震活动性研究. 1993. 北京:地震出版社.
吴时国,余朝华,邹东波,张海英.2006. 莱州湾地区郯庐断裂带的构造特征及其新生代演化. 海洋地质与第四纪地质,26(6):101～110.
向宏发,方仲景,张晚霞,贾三发,李如成. 1994. 平原区隐伏断裂的综合探测研究.见:中国地震学会地震专业委员会编. 中国活动断层研究. 北京:地震出版社,205～214.
徐建国,徐华,张涛,张卓,祁晓凡,纪汶龙. 2018.山东半岛莱州湾滨海地区黑土湖组地层特征、时代及指示的全新世海岸带变化. 地球学报,29(2):133～143.
严乐佳,朱光,林少泽,赵田. 2014. 沂沭断裂带新构造活动规律与机制. 中国科学:地球科学,44(7):1452～1467.
杨一冲. 1993. 沂沭活断层分段特征及地震趋势的预测. 地震,1:45～48.
张鹏,王良书,石火生,李利梅,谭慧明. 2010. 郯庐断裂带山东段的中新生代构造演化特征. 地质学报,84(9):1316～1323.
赵大升,肖增岳,王艺芬. 1983. 郯庐断裂带及其邻近地区新生代火山岩岩石特征及成因探讨. 地质学报,2:128～141.
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. 中国地震,4(3):123～129.
周斌,邓志辉,晁洪太,许华明,杨竹转,肖兰喜,王志才,张永祥. 2008. 营潍断裂带走滑构造特征、演化及动力学机制. 西北地震学报,30(2):117～121.
? 山东省国土资源厅. 2014. 山东省地层侵入岩构造单元划分方案(未出版).