吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (1): 261-272.doi: 10.13278/j.cnki.jjuese.20190016

• 地球探测与信息技术 • 上一篇    

地球物理资料揭示的嫩江—八里罕断裂中段深浅构造特征

张鹏辉1,2, 张小博1,2, 方慧1,2, 王小江1,2, 刘建勋1,2   

  1. 1. 国家现代地质勘查技术研究中心, 河北 廊坊 065000;
    2. 中国地质科学院地球物理地球化学勘查研究所, 河北 廊坊 065000
  • 收稿日期:2019-01-23 发布日期:2020-02-11
  • 作者简介:张鹏辉(1987-),男,工程师,主要从事应用地球物理工作,E-mail:zhangpenghui@igge.cn
  • 基金资助:
    中国地质调查局地质调查项目（DD20160164，DD20190030）；中央级公益性科研院所基本科研业务费专项（AS2019Y02）

Deep and Shallow Structural Characteristics of Middle Segment of Nenjiang-Balihan Fault Based on Geophysical Data

Zhang Penghui1,2, Zhang Xiaobo1,2, Fang Hui1,2, Wang Xiaojiang1,2, Liu Jianxun1,2   

  1. 1. National Center for Geological Exploration Technology, Langfang 065000, Hebei, China;
    2. Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, Hebei, China
  • Received:2019-01-23 Published:2020-02-11
  • Supported by:
    Supported by Geological Survey Project of China Geological Survey (DD20160164, DD20190030) and Fundamental Research Funds for the Central Public Research Institutes (AS2019Y02)

PDF (PC)

298

摘要： 嫩江-八里罕断裂是松辽盆地西缘的一条重要断裂，对区域中-新生代盆地的形成演化至关重要。由于该断裂中段地表覆盖厚层第四系，其深部构造特征研究程度较弱。本文通过对横跨嫩江-八里罕断裂的1条大地电磁测深测线和1条地震测线进行处理和解译，结合区域钻井结果解译了该断裂深部、浅部构造特征。结果表明，深部电性结构横向上以"八"字型低阻条带为界与地质单元具有较好的对应关系；结合已有地质认识推断东倾的L3低阻条带是嫩江-八里罕断裂的电性响应。该断裂是1条东倾的超壳断裂，浅部产状较陡、向深部逐渐趋缓，整体上由2条东倾的反"Y"字型断裂和1条西倾的断裂组成，呈花状构造样式，指示断裂曾历经强烈的挤压应力环境。

关键词: 嫩江—八里罕断裂, 大地电磁测深, 壳内低阻层, 构造特征, 松辽盆地

Abstract: The Nenjiang-Balihan fault is an important fault on the western margin of Songliao basin. It is of great significance to study the formation and evolution of the Meso and Cenozoic basins in the region. The previous research on the deep structural characteristics of the Nenjiang-Balihan fault is relatively inadequate, as it is covered by thick sediments. In this study, one MT (magnetotelluric sounding) line and one seismic profile across the Nenjiang-Balihan fault were processed and interpreted, and in combination with the regional drilling data, the structural characteristics of the deep and shallow parts of the fault were obtained. The results show that the deep electrical structures along the MT profile are horizontally bounded by an "eight-shaped" low resistance band and corresponded well to the geological units. It is inferred that the east-dipping low-resistivity strip L3 represents the Nenjiang-Balihan fault with the characteristics of concealment, ultra-crust, shallow high angle, etc. The whole fault is composed of two east-dipping anti-Y-type faults and one west-dipping fault, in a flower-like structural style, indicating that the faults have experienced a strong compressive stress environment.

Key words: Nenjiang-Balihan fault, magnetotelluric sounding, low-resistivity layer in crust, structural characteristics, Songliao basin

中图分类号: 

  • P319.2
[1] 陈洪洲,余中元,许晓艳,等. 嫩江断裂构造及其与地震活动的关系[J]. 东北地震研究, 2004, 20(4):43-49. Chen Hongzhou, Yu Zhongyuan, Xu Xiaoyan, et al. Characteristics of Nenjiang Fracture Structure and the Relation Between This Fracture and Earthquake Activity[J]. Seismological Research of Northeast China, 2004, 20(4):43-49.
[2] 张凤旭,张兴洲,张凤琴,等. 中国东北地区重力场研究:利用改进的三方向小子域滤波划分主构造线及大地构造单元[J].地球物理学报,2010,53(6):1475-1485. Zhang Fengxu, Zhang Xingzhou, Zhang Fengqin, et al. Study of Gravity Field in Northeastern China Area:Classification of Main Structure Lines and Tectonic Units Using the Improved Three-Directional Small Subdomain Filtering[J]. Chinese Journal of Geophysics, 2010, 53(6):1475-1485.
[3] 熊小松,高锐,侯贺晟,等. 深地震反射剖面揭示嫩江断裂带中段的深部几何形态与地壳形变[J].地质科学, 2016, 51(3):694-705. Xiong Xiaosong, Gao Rui, Hou Hesheng, et al. Deep Structure Geometry Features of Nenjiang Deformation Revealed by Deep Seismic Fault Zone and Crustal Reflection Profile[J]. Journal of Geology, 2016, 51(3):694-705.
[4] 韩国卿,刘永江,温泉波,等. 嫩江-八里罕断裂带岭下韧性剪切带变形特征[J]. 吉林大学学报(地球科学版), 2009, 39(3):397-405. Han Guoqing, Liu Yongjiang, Wen Quanbo, et al. The Characteristics of Structural Deformation for the Lingxia Ductile Shear Zone of Nenjiang-Balihan Fault Belt in Northeastern China[J]. Journal of Jilin University (Earth Science Edition), 2009, 39(3):397-405.
[5] 韩国卿. 嫩江-八里罕断裂带构造变形特征研究[D]. 长春:吉林大学, 2008. Han Guoqing. The Study on Characteristics of Structural Deformation of the Nenjiang-Balihan Fault Belt in Northeastern China[D]. Changchun:Jilin University, 2008.
[6] 韩国卿,刘永江, Franz Neubauer,等. 松辽盆地西缘边界断裂带中北段尼尔基L型构造岩构造年代学及其构造意义[J]. 岩石学报, 2013, 30(7):1922-1934. Han Guoqing, Liu Yongjiang, Franz Neubauer, et al. Chronology of L-Type Tectonite from Nierji Area in the Northern-Middle Segment of the Western Boundary Fault of the Songliao Basin and Its Tectonic Implications[J]. Acta Petrologica Sinica, 2013, 30(7):1922-1934.
[7] Wang Xinshe,Zheng Yadong,Wang Tao. Strain and Shear Types of the Louzidian Ductile Shear Zone in Southern Chifeng, Inner Mongolia, China[J]. Science in China:Series D:Earth Sciences, 2007, 50(4):487-495.
[8] Zhang Xiaohui, Li Tiesheng, Pu Zhiping, et al. 40Ar-39Ar Ages of the Louzidian-Dachengzi Ductile Shear Zone near Chifeng, Inner Mongolia and Their Tectonic Significance[J]. Chinese Science Bulletin, 2002, 47(15):1292.
[9] 刘伟,杨进辉,李潮峰. 内蒙赤峰地区若干主干断裂带的构造热年代学[J]. 岩石学报, 2003,19(4):717-728. Liu Wei, Yang Jinhui, Li Chaofeng. Thermo-Chronology of Three Major Faults in the Chifeng Area, Inner Mongolia of China[J]. Acta Petrologica Sinica, 2003, 19(4):717-728.
[10] 于清水,张凤旭,曾昭发. 大兴安岭北段的地球物理场研究[J]. 世界地质, 2015, 34(1):187-193. Yu Qingshui, Zhang Fengxu, Zeng Zhaofa. Research on Geophysical Field in Northern Part of Da Hinggan Mountains[J]. Global Geology, 2015, 34(1):187-193.
[11] 内蒙古自治区地质矿产局.内蒙古自治区区域地质志[M]. 北京:地质出版社, 1991. Bureau of Geology and Mineral Resources of Inner Mongolia Autonomous Region. Regional Geology of Inner Mongolia Autonomous Region[M]. Beijing:Geological Publishing House, 1991.
[12] 刘财,杨宝俊,王兆国,等. 松辽盆地西边界带深部构造:地电学证据[J].地球物理学报,2011,54(2):401-406. Liu Cai, Yang Baojun, Wang Zhaoguo, et al. The Deep Structure of the Western Boundary Belt of the Songliao Basin:The Geoelectric Evidence[J]. Chinese Journal of Geophysics, 2011, 54(2):401-406.
[13] Liu Yongjiang, Li Weimin, Feng Zhiqiang. A Review of the Paleozoic Tectonics in the Eastern Part of Central Asian Orogenic Belt[J]. Gondwana Research, 2017(43):123-148.
[14] Xu Wenliang, Pei Fuping, Wang Feng, et al. Spatial-Temporal Relationships of Mesozoic Volcanic Rocks in NE China:Constraints on Tectonic Overprinting and Transformations Between Multiple Tectonic Regimes[J]. Journal of Asian Earth Sciences, 2013, 74(18):167-193.
[15] Tang Jie, Xu Wenliang, Wang Feng, et al. Geochronology and Geochemistry of Early-Middle Triassic Magmatism in the Erguna Massif, NE China:Constraints on the Tectonic Evolution of the Mongol-Okhotsk Ocean[J]. Lithos, 2014, 184/185/186/187:1-16.
[16] 王五力,李永飞,郭胜哲. 中国东北地块群及其构造演化[J].地质与资源, 2014, 23(1):4-24. Wang Wuli,Li Yongfei,Guo Shengzhe. The Northeast China Block Group and Its Tectonic Evolution[J]. Geology and Resources, 2014,23(1):4-24.
[17] 李春昱. 中国板块构造的轮廓[J].中国地质科学院院报,1980, 2(1):11-22. Li Chunyu. A Preliminary Study of Plate Tectonics of China[J]. Acta Geoscientia Sinica, 1980, 2(1):11-22.
[18] 谢鸣谦. 拼贴板块构造及其驱动机理:中国东北及邻区的大地构造演化[M]. 北京:科学出版社, 2000:1-260. Xie Mingqian. Amalgamating Plate Tectonic and Its Droved Mechanism-Tectonic Evolution of Northeast China and Ddjacent Area[M]. Beijing:Science Press, 2000:1-260.
[19] 任纪舜, 王作勋, 陈炳蔚, 等. 从全球看中国大地构造:中国及邻区大地构造图简要说明[M].北京:地质出版社, 1999:1-50. Ren Jishun, Wang Zuoxun, Chen Bingwei, et al. The Tectonics of China from a Global View:A Guide to the Tectonic Map of China and Adjacent Regions[M]. Beijing:Geological Publishing House, 1999:1-50.
[20] 彭玉鲸,纪春华,辛玉莲. 中俄朝毗邻地区古吉黑造山带岩石及年代纪录[J].地质与资源, 2002, 11(2):65-75. Peng Yujing, Ji Chunhua, Xin Yulian. Petrology and Geo-Chronology of the Paleo-Jilin-Heilongjiang Orogenic Belt in the Adgecent Areas of China, Russion and Korea[J]. Geology and Resources, 2002, 11(2):65-75.
[21] 王成文,金巍,张兴洲,等. 东北及邻区晚古生代大地构造属性新认识[J]. 地层学杂志, 2008, 32(2):119-136. Wang Chengwen, Jin Wei, Zhang Xingzhou, et al. New Understanding of the Late Paleozoic Tectonics in Northeastern China and Adjacent Areas[J]. Journal of Stratigraphy, 2008, 32(2):119-136.
[22] Li Jinyi. Permian Geodynamic Setting of Northeast China and Adjacent Regions:Closure of the Paleo-Asian Ocean and Subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26(3/4):207-224.
[23] Xiao Wenjiao, Windley F B, Sun S, et al. A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia:Oroclines, Sutures, and Terminal Accretion[J]. Annual Review of Earth and Planetary Sciences, 2015, 43(1):477-507.
[24] 刘永江,张兴洲,迟效国,等. 大兴安岭地区上古生界变形特征及构造层划分[J]. 吉林大学学报(地球科学版), 2011, 41(5):1304-1313. Liu Yongjiang, Zhang Xingzhou, Chi Xiaoguo, et al. Deformation and Tectonic Layer Division of the Upper Paleozoic in Daxing'anling Area[J]. Journal of Jilin University (Earth Science Edition), 2011, 41(5):1304-1313.
[25] 邵济安,张履桥,牟保磊,等. 大兴安岭的隆起与地球动力学背景[M]. 北京:地质出版社, 2007. Shao Ji'an, Zhang Lüqiao, Mu Baolei, et al. Upwelling of Da Hinggan Mountains and Its Geodynamic Background[M]. Beijing:Geological Publishing House, 2007.
[26] 张兴洲,马玉霞,迟效国,等. 东北及内蒙古东部地区显生宙构造演化的有关问题[J]. 吉林大学学报(地球科学版), 2012, 42(5):1269-1285. Zhang Xingzhou, Ma Yuxia, Chi Xiaoguo, et al. Discussion on Phanerozoic Tectonic Evolution in Northeastern China[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(5):1269-1285.
[27] 万天丰.中国大地构造学纲要[M].北京:地质出版社2011. Wan Tianfeng. The Tectonics of China:Data, Maps, Evolution[M]. Beijing:Geological Publishing House, 2011.
[28] 李三忠,索艳慧, 李玺瑶, 等. 西太平洋中生代板块俯冲过程与东亚洋陆过渡带构造-岩浆响应[J].科学通报, 2018, 63(16):1550-1593. Li Sanzhong, Suo Yanhui, Li Xiyao, et al. Mesozoic Plate Subduction in West Pacific and Tectono-Magmatic Response in the East Asian Ocean-Continent Connection Zone[J]. Chin Sci Bull, 2018, 63(16):1550-1593.
[29] 韩江涛, 郭振宇, 刘文玉, 等. 松辽盆地岩石圈减薄的深部动力学过程[J]. 地球物理学报, 2018,61(6):95-109. Han Jiangtao, Guo Zhenyu, Liu Wenyu, et al. Deep Dynamic Process of Lithosphere Thinning in Songliao Basin[J]. Chinese Journal of Geophysics, 2018, 61(6):95-109.
[30] 蔡军涛,陈小斌. 大地电磁资料精细处理和二维反演解释技术研究(二):反演数据极化模式选择[J]. 地球物理学报,2010,53(11):2703-2714. Cai Juntao, Chen Xiaobin. Refined Techniques for Data Processing and Two-Dimensional Inversion in Magnetotelluric (II):Which Data Polarization Mode Should Be Used in 2D Inversion[J]. Chinese Journal of Geophysics, 2010, 53(11):2703-2714.
[31] 陈小斌,蔡军涛,王立凤,等. 大地电磁资料精细处理和二维反演解释技术研究(四):阻抗张量分解的多测点-多频点统计成像分析[J]. 地球物理学报,2014,57(6):1946-1957. Chen Xiaobin, Cai Juntao, Wang Lifeng, et al. Refined Techniques for Data Processing and Two-Dimensional Inversion Magnetotelluric(IV):Statistical Image Method Based on Multi-Site, Multi-Frequency Tensor Decomposition[J]. Chinese Journal of Geophysics, 2014, 57(6):1946-1957.
[32] Rodi W, Mackie R L. Nonlinear Conjugate Gradients Algorithm for 2-D Magnetotelluric Inversion[J]. Geophysics, 2001, 66(1):174-187.
[33] 许文良,王枫,裴福萍,等. 中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J]. 岩石学报, 2012, 29(2):339-353. Xu Wenliang, Wang Feng, Pei Fuping, et al. Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations[J]. Acta Petrologica Sinica, 2012, 29(2):339-353.
[34] 张健, 卞雄飞, 陈树旺,等. 大兴安岭中南部上二叠统林西组页岩气资源前景[J]. 地质通报, 2013, 32(8):1297-1306. Zhang Jian, Bian Xiongfei, Chen Shuwang, et al. Shale Gas Resources Prospect of Late Permian Linxi Formation in the Middle-Southern Part of the Da Hinggan Mountains[J]. Geological Bulletin of China, 2013, 32(8):1297-1306.
[35] 方慧,钟清,陈树旺.内蒙古突泉盆地双低阻层的发现及其地质意义[J]. 地质通报, 2013, 32(8):1253-1259. Fang Hui, Zhong Qing, Chen Shuwang. The Discovery of Two Conductive Layers in Tuquan Basin, Inner Mongolia, and Its Geological Significance[J]. Geological Bulletin of China, 2013, 32(8):1253-1259.
[36] Liang Hongda, Gao Rui, Hou Hesheng, et al. Lithospheric Electrical Structure of the Great Xing'an Range[J]. Journal of Asian Earth Sciences, 2015, 113:501-507.
[37] 张贻侠,孙运生,张兴洲,等. 中国满洲里-绥芬河地学断面1:1000000说明书[M].北京:地质出版社,1998:1-53. Zhang Yixia, Sun Yunsheng, Zhang Xingzhou, et al. The 1:1000000 Specification of the Manzhouli-Suifenhe Geotransect[M]. Beijing:Geological Publishing House, 1994:1-53.
[38] 朱洪翔,田有,刘财,等. 中国东北地区高分辨率地壳结构:远震接收函数[J]. 地球物理学报,2017,60(5):1676-1689. Zhu Hongxiang, Tian You, Liu Cai, et al. High-Resolution Crustal Structure of Northeast China Revealed by Teleseismic Receiver Functions[J]. Chinese Journal of Geophysics, 2017, 60(5):1676-1689.
[39] 李英康,高锐,姚聿涛,等. 大兴安岭造山带及两侧盆地的地壳速度结构[J]. 地球物理学进展, 2014, 29(1):73-83. Li Yingkang, Gao Rui, Yao Yutao, et al. The Crust Velocity Structure of Da Hinggan Ling Orgenic Belt and the Basins on Both Side[J]. Progress in Geophysics, 2014, 29(1):73-83.
[40] 庞庆山,方德庆,翟培民,等. 松辽盆地北部基底石炭-二叠系的分布[J].大庆石油学院学报, 2002, 26(3):92-94. Pang Qingshan, Fang Deqing, Zhai Peimin, et al. Distribution of Carboniferous-Permian System on the North Base of Songliao Basin[J]. Journal of Daqing Petroleum Institute, 2002, 26(3):92-94.
[41] 张健,郑月娟,张德军,等. 松辽盆地西缘高力板断陷高D1井地层划分对比[J]. 东北石油大学学报, 2019, 43(1):22-29. Zhang Jian, Zheng Yuejuan, Zhang Dejun, et al. Stratigraphic Division and Correlation of the Borehole GD1 in the Gaoliban Fault Depression, Western Margin of Songliao Basin[J]. Journal of Northeast Petroleum University, 2019, 43(1):22-29.
[42] 陈树旺,张健,郑月娟,等. 松辽盆地西部斜坡区上古生界油气地质调查进展与发现[J].中国地质调查, 2019, 6(1):1-9. Chen Shuwang, Zhang Jian, Zheng Yuejuan, et al. Progresses and Discoveries of Geological Survey on Oil and Gas Resources Related to the Upper Paleozoic in the Western Slope of Songliao Basin[J]. Geological Survey of China, 2019, 6(1):1-9.
[1] 迟唤昭, 董福湘, 薛晓刚, 刘财, 司考. 松辽盆地南部地区营城组典型火山机构地质特征[J]. 吉林大学学报(地球科学版), 2019, 49(6): 1649-1657.
[2] 周翔. 松辽盆地北部营城组火山岩地球化学特征及地质意义[J]. 吉林大学学报(地球科学版), 2019, 49(4): 1001-1014.
[3] 侯方辉, 郭兴伟, 吴志强, 朱晓青, 张训华, 祁江豪, 王保军, 温珍河, 蔡来星, 庞玉茂. 南黄海有关地层与构造的研究进展及问题讨论[J]. 吉林大学学报(地球科学版), 2019, 49(1): 96-105.
[4] 薛林福, 祝铭, 李文庆, 刘文玉, 刘正宏, 刘泽宇. 岩浆泡破裂引发地震的模式——以吉林松原2013年地震群为例[J]. 吉林大学学报(地球科学版), 2018, 48(6): 1865-1875.
[5] 马国庆, 孟庆发, 黄大年. 基于重力异常的松辽盆地构造特征识别[J]. 吉林大学学报(地球科学版), 2018, 48(2): 507-516.
[6] 朱晓颖, 杨海, 匡星涛, 彭巍巍, 张洪瑞. 新疆东昆仑-阿尔金地区航磁反映的断裂构造特征[J]. 吉林大学学报(地球科学版), 2018, 48(2): 461-473.
[7] 姚刚, 董向欣, 李丽丽, 马国庆, 孟令顺. 东海陆架盆地构造划分的高精度重磁解释技术[J]. 吉林大学学报(地球科学版), 2018, 48(2): 517-524.
[8] 蔡来星, 卢双舫, 肖国林, 王蛟, 吴志强, 郭兴伟, 侯方辉. 论优质源储耦合关系的控藏作用:对比松南致密油与松北致密气成藏条件[J]. 吉林大学学报(地球科学版), 2018, 48(1): 15-28.
[9] 鲍新华, 张宇, 李野, 吴永东, 马丹, 周广慧. 松辽盆地增强型地热系统开发选区评价[J]. 吉林大学学报(地球科学版), 2017, 47(2): 564-572.
[10] 高翔, 刘志宏, 聂志阳, 姚勇, 贾卧, 王超, 宋健. 松辽盆地大庆长垣形成时间的厘定及其地质意义[J]. 吉林大学学报(地球科学版), 2017, 47(1): 74-83.
[11] 韩松, 刘国兴, 韩江涛. 华南地区进贤-柘荣剖面深部电性结构[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1837-1846.
[12] 林承焰, 曹铮, 任丽华, 张昌盛, 范瑞峰, 王叶, 邢新亚, 马晓兰. 松辽盆地南部大情字井向斜区葡萄花油层石油富集规律及成藏模式[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1598-1610.
[13] 刘财, 杨宝俊, 冯晅, 单玄龙, 田有, 刘洋, 鹿琪, 刘才华, 杨冬, 王世煜. 论油气资源的多元勘探[J]. 吉林大学学报(地球科学版), 2016, 46(4): 1208-1220.
[14] 温志良, 姜福平, 钟长林, 姜雪飞, 王果谦, 齐岩. 松辽盆地东南隆起超大型油页岩矿床特征及成因[J]. 吉林大学学报(地球科学版), 2016, 46(3): 681-691.
[15] 康健, 韦庆海, 周琳, 高研, 张永刚, 高峰. 利用地震台阵观测资料研究大庆地区深部构造[J]. 吉林大学学报(地球科学版), 2016, 46(3): 900-910.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发