莱州湾地区郯庐断裂带的构造特征及其新生代演化

吴时国; 余朝华; 邹东波; 张海英

莱州湾地区郯庐断裂带的构造特征及其新生代演化

1 中国石油大学地球资源与信息学院, 青岛 266555;
2 中国科学院海洋研究所地质与环境重点实验室, 青岛 266071;
3 中国科学院研究生院, 北京 100039;
4 胜利油田物探研究院, 东营 257022

基金项目:

中国科学院创新工程项目(KZCX3-SW-219

山东省泰山学者建设工程基金

KZCX1-SW-18-06)

详细信息

作者简介:
吴时国(1963-),男,研究员,从事海底构造、海洋地球物理和天然气水合物研究,E-mail:swu@ms.qdio.ac.cn

中图分类号: P738
计量
- 文章访问数: 2015
- HTML全文浏览量: 185
- PDF下载量: 23
出版历程
- 收稿日期: 2006-02-17
- 修回日期: 2006-07-14

STRUCTURAL FEATURES AND CENOZOIC EVOLUTION OF THE TAN-LU FAULT ZONE IN THE LAIZHOU BAY,BOHAI SEA

1 College of Geo-Resources and Information, Petroleum University of China(Huadong), Qingdao 266555, China;
2 Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;
3 Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;
4 Geophysical Research Institute of Shengli Oil Field, Dongying 257022, China

摘要

摘要: 郯庐断裂带中段分东西两支从莱州湾进入渤海,在莱州湾地区的构造特征与演化历史一直鲜为人知。通过对横穿研究区的两条地震测线的解释和分析,揭示了该区郯庐断裂带中段在研究区的构造差异,研究表明郯庐断裂带东西两支在该研究区表现出不同的断裂性质,西支断裂表现为正断层,东支断裂表现为走滑断层。郯庐断裂是本研究区的主控断裂,通过对本地区地层形态及其组合、断层的剖面形态和空间展布规律的深入研究,揭示了郯庐断裂带在莱州湾地区新生代以来的构造演化历史:古新世-始新世的伸展阶段、渐新世-中新世早期的挤压和右行走滑阶段、中新世中晚期至今的稳定发展阶段,这几个不同时期的演化阶段主要受太平洋板块运动的方向和速度变化的控制。
- 走滑断裂 /
- 构造特征 /
- 构造演化 /
- 郯庐断裂带 /
- 莱州湾
Abstract: The middle portion of Tan-Lu fault zone is divided into two branches(the east and west faults) and enters the Laizhou Bay of the Bohai Sea, according to the interpretation and analysis results of the seismic lines across the study area. The structural characters of the middle portion of the Tan-Lu fault zone are little reported due to lack of seismic data. During this study, we discuss the tectonics and evolution of the Tan-Lu fault in the Laizhou Bay by using the latest seismic data. The research result shows that the two faults are different in kinematical characters in the study area:the west fault is a normal fault while the east is a strike-slip one. The Tan-Lu fault zone is the main fault in the study area. After careful researches on the stratigraphic distribution and combination, sectional shape and dimensional distribution features of the faults in the study area, the Cenozoic tectonic evolution history of the middle portion of the Tan-Lu fault zone is divided into three stages:Paleocene-Eocene extension, Oligocene-early Miocene extrusion and dextral strike-slip, middle Miocene to the present stable depression, which are mainly controlled by direction and velocity changes of the Pacific plate.
- strike-slip fault /
- structural feature /
- tectonic evolution /
- Tan-Lu fault zone /
- Laizhou Bay

HTML全文

参考文献(36)

[1]	Gao W M, Li J L, Sun Z Y. Formation and evolution of the Yi-Shu continental rift[J]. Seismol. Geol., 1980, 2:11-18.
[2]	Zhang Y Q, Dong S W, Shi W. Cretaceous deformation history of the middle Tan-Lu fault zone in Shangdong Province, eastern China[J]. Tectonophysics, 2003, 363:243-258.
[3]	施炜, 张岳桥, 董树文. 郯庐断裂带中段第四纪活动及其分段特征[J]. 地球学报, 2003, 24(1):11-18. [SHI Wei, ZHANG Yue-qiao,DONG Shu-wen. Quaternary activity and segmentation behavior of the middle portion of the Tan-Lu Fault Zone[J]. Acta Geoscientia Sinica, 2003, 24(1):11-18.]
[4]	徐嘉炜. 郯庐断裂带的平移运动及其地质意义[C]//第26届国际地质大会论文集. 北京:地质出版社, 1980:129-142.[XU Jia-wei. The horizontal displacement of Tancheng-Lujiang fault zone and its geological significance[C]//The 26^th Geological Paper Collection for International Exchange. Beijing:Geological Publishing House, 1980 :129-142.]
[5]	徐嘉炜. 郯城庐江平移断裂系统[J]. 构造地质论丛, 1984, 3:18-32.[XU Jia-wei. The Tancheng-Lujiang wrench fault system[J]. Structural Geology Review, 1984 , 3:18-32.]
[6]	Grimmer J C, Jonckheere R, Enkelmann E, et al. Cretaceous-Cenozoic history of the southern Tan-Lu fault zone:apatite fission-track and structural constraints from the Dabie Shan (eastern China)[J]. Tectonophysics, 2002, 359:225-253.
[7]	Watson M P, Hayward A B, Parkinson D N, et al. Plate tectonic history, basin development and petroleum source rock deposition onshore China[J]. Marine and Petroleum Geology, 1987, 4(3):205-225.
[8]	Xu J W, Zhu G, Tong W X, et al. Formation and evolution of the Tancheng-Lujiang wrench fault system:a major shear system to the northern of the Pacific Ocean[J]. Tectonophysics, 1987, 134:273-310.
[9]	Okay A I, Sengor A M. Evidence for intracontinental thrust-related exhumation of the ultra-high-pressure rocks in China[J]. Geology, 1992, 20:411-414.
[10]	Zhang K J. North and South China collision along the eastern and southern North China margins[J]. Tectonophysics, 1997, 270:145-156.
[11]	Yin A, Nie S Y. An indendation model for the North and South China collision and the development of the Tan-Lu and Honam fault system, eastern Asia[J]. Tectonics, 1993, 12:801-813.
[12]	万天丰, 朱鸿. 郯庐断裂带的最大左行走滑断距及其形成时期[J]. 高校地质学报, 1996, 2(1):14-27. [WAN Tian-feng, ZHU Hong. The maximum sinistral strike-slip displacement and formation time of the Tan-Lu fault zone[J]. Geological Journal of China Universities, 1996, 2(1):14-27.]
[13]	Zhu G, Liu G S, Niu M L. Transcurrent movement and genesis of the Tan-Lu fault zone[J]. Geological Bulletin of China, 2003, 22:201-207.
[14]	Xu J W, Zhu G. Tectonic models of the Tan-Lu fault zone, eastern China[J]. International Geology Review, 1994, 36:771-784.
[15]	Zhu G, Xu J W, Shun S J. Isotopic age evidence for the timing of strike-slip movement of the Tan-Lu fault zone[J]. Geological Review, 1995, 4:452-461.
[16]	Li Z X. Collsion between the North and South China blocks:a crust-detachment model for suturing in the region east of Tan-Lu fault[J]. Geology, 1994, 22:739-742.
[17]	许志琴. 郯庐裂谷系概述[J]. 构造地质论丛, 1984, 3:39-46.[XU Zhi-qin. General of the Tancheng-Lujiang rift system[J]. Structural Geology Review, 1984 , 3:39-46.]
[18]	蔡东升. 渤海莱州湾走滑拉分凹陷的构造研究及其石油勘探意义[J]. 石油学报, 2001, 22(3):19-24. [CAI Dong-sheng.Strike-slip and pull-apart structure study and its significance to petroleum exploration on Laizhouwan Sag, Bohai area[J]. Acta Petroleum Sinica, 2001, 22(3):19-24.]
[19]	程有义, 李晓清,汪泽成,等. 潍北拉分盆地形成演化及其对成油气条件的控制[J]. 石油勘探与开发, 2004, 31(6):32-35. [CHENG You-yi, LI Xiao-qing, WANG Ze-cheng, et al. Tectonic evolution and its controlling on petroleum generation in Weibei Basin[J]. Petroleum Exploration and Development, 200431(6):32-35.]
[20]	Engebretson D C, Cox A,Gordon R G. Relative motions between oceanic and continental plates in the Pacific basin[J]. The Geological Society of America, Special Paper, 1985, 206:1-59.
[21]	Maruyama S, Isozaki Y, Kimura G, et al. Paleogeographic maps of the Japanese Islands:plate tectonic systhesis from 750 Ma to the present[J]. Island Arc, 1997, 6:121-142.
[22]	朱光, 王道轩, 刘国生,等. 郯庐断裂带的演化及其对西太平洋板块运动的响应[J].地质科学, 2004, 39(1):36-49. [ZHU Guang, WANG Dao-xuan, LIU Guo-sheng, et al. Evolution of the Tan-Lu fault zone and its responses to Plate Movements in West Pacific Basin[J]. Chinese Journal of Geology, 2004, 39(1):36-49.]
[23]	Zhou X M,Li X W. Origin of late Mesozoic igneous rocks in Southeastern China:implications for lithospere subduction and underplating of mafic magmas[J]. Tectonophysics, 2000, 326:269-287.
[24]	马杏垣, 刘和甫, 王维襄,等. 中国东部中、新生代裂谷作用和伸展构造[J]. 地质学报, 1983, 57(1):22-32. [MA Xing-yuan,LIU He-fu,WANG Wei-xiang,et al.Meso-Cenozoic rifting and extensional structure[J].Acta Geologia Sinica,1983,57(1):22-32.]
[25]	邓晋福, 赵海玲, 罗昭华,等. 新生代中国东部大陆岩石圈的伸展与减薄[C]//中国大陆构造论文集. 武汉:中国地质大学出版社,1992:165-172.[DENG Jin-fu, ZHAO Hai-ling, LUO ZHAO-hua, et al. Stretching and thinning of Mesozoic continental lithosphere in East China[C]//Proceeding of construction in China mainland. Wuhan:Publishing House of China University of Geosciences, 1992:165 -172.]
[26]	孙继源, 邢集善, 叶志光,等. 华北地区板块内构造及深部过程初探[J]. 地质科技情报, 1992, 11(1):4-13. [SUN Ji-yuan, XING Ji-shan, Ye Zhi-guang,et al. Intraplate tectonics and deep-seated process in north China[J]. Geological Science and Technology Information, 1992, 11(1):4-13.]
[27]	Wan T F. Intraplate Deformation, Tectonic Stress Field and their Application for the Eastern China in the Meso-Cenozoic[M]. Wuhan:Press of China University of Geosciences, 1994.
[28]	任建业, 李思田. 西太平洋边缘海盆的扩张过程和动力学背景[J]. 地学前缘, 2000, 7(3):203-213. [REN Jian-ye,LI Si-tian. Spreading and dynamic setting of marginal basins of the Western Pacific[J]. Earth Science Frontiers, 2000, 7(3):203-213.]
[29]	胡望水, 吕炳全, 官大勇,等. 郯庐断裂带及其周缘中新生代盆地发育特征[J]. 海洋地质与第四纪地质, 2003, 23(4):51-58. [HU Wang-shu, LÜ Bing-quan, GUAN Da-yong,et al. Characteristics of Tanlu fault zone and development of Mesozoic and Cenozoic basins along it[J]. Marine Geology and Quaternary Geology, 2003, 23(4):51-58.]
[30]	Otofuji Y, Hayashida A,Torii M. When was the Japan Sea opened? Paleomagnetic evidence from southwest Japan[C]//Nasu N, Uyeda S, Kushiro I, et al(eds). Formation of Active Ocean Margins. Tokyo:Terra,1985:551-566.
[31]	Kaneoka I, Notsu K, Takigami Y, et al. Constraints on the evolution of the Japan Sea based on ⁴⁰Ar-³⁹Ar ages and Sr isotopic ratios for volcanic rocks of the Yamato Seamount chain in the Japan Sea[J]. Earth Planet. Sci. Lett., 1990, 97:211-225.
[32]	万天丰, 朱鸿, 赵磊. 郯庐断裂带的形成与演化综述[J]. 现代地质, 1996, 10(2):159-167. [WANG Tian-feng, ZHU Hong, ZHAO Lei, et al. Formation and evolution of Tancheng-Lujiang Fault Zone:A Review[J]. Geoscience, 1996, 10(2):159-167.]
[33]	李宏伟, 许坤. 郯庐断裂走滑活动与辽河盆地构造古地理格局[J]. 地学前缘, 2001, 8(4):15-18. [LI Hong-wei,XU Kun. The dextral strike-slip faulting of Tan-Lu fault zone and the structural oil fields distribution in Liaohe Basin[J]. Earth Science Frontiers, 2001, 8(4):15-18.]
[34]	侯明金, 王永敏, Jacques M,等. 郯庐断裂带(安徽部分)动力学演化及其构造意义[J]. 地质通报, 2003, 22(2):105-112. [HOU Ming-jin, WANG Yong-min, Jacques M,et al. Dynamic evolution and tectonic significance of the Tanlu fault zone (Anhui segment)[J]. Geological Bulletin of China, 2003, 22(2):105-112.]
[35]	王小凤, 李中坚, 陈柏林,等. 郯庐断裂带[M]. 北京:地质出版社, 2001:15-59.[WANG Xiao-feng, LI Zhong-jian, CHEN Bai-lin, et al. On Tan-Lu Fault Zone[M]. Beijing:Geological Publishing House, 2001:15 -59.]
[36]	李家灵, 高维明, 孙竹友. 沂沭裂谷消亡与华北裂谷新生代构造应力场[J]. 构造地质论丛, 1984, 3:318-327.[LI Jiao-ling, GAO Wei-ming, SUN Zhu-you, et al. The extinction of Yishu rift valley field of the rift valley in North China[J].1984 , 3:318-327.]