松辽盆地北部反转构造的几何特征、变形机制及其地震地质意义——以大安-德都断裂为例
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
松辽盆地北部发育的中-新生代反转构造代表着盆地继伸展裂陷阶段、热冷却拗陷阶段之后的第3个构造演化阶段。系统收集了布设在覆盖大安-德都断裂及其附近的14个3维地震工区,30条区域地震反射大剖面,在此基础上准确追踪解释了T06、T1、T11、T2、T3、T4、T5等7个地震反射层位。同时基于52口钻孔的资料对重点反射层的地质年代进行了重新厘定,分析了不同时期断层展布特征及分布规律,重点就松辽盆地中新生代反转构造的几何学形态、变形特征与机制进行了研究。研究结果认为,该反转构造为大安-德都断裂在中生代末期和新生代早期的主要变形模式,符合"逆断层-褶皱"构造的几何形态和变形机制。松辽盆地内部的构造变形主要集中在该构造反转带上。此外,重点选择了2条典型剖面开展了野外实验性浅层人工地震勘探。根据勘探结果并结合该地区第四纪地层厚度分析认为,广泛发育在背斜顶部且断错T06界面的小断裂可能代表了大安-德都断裂强变形带的最新活动性,勘探剖面揭示的上断点断错最年轻地层为中更新统,并据此初步判定该断裂最新活动时代可能为中更新世。此外,综合人工地震勘探结果、现代地震活动性和震源机制解研究结果认为,大安-德都断裂的"逆断层-褶皱"构造反转带最新的活动已明显影响到了近地表的反射层,清楚断错了早-中更新世地层,控制着断裂附近中强地震的发生,是松辽盆地内部或整个东北地区重要和典型的发震构造之一。
Meso-Cenozoic inversion structures developed in northern Songliao Basin represent the third tectonic evolution stage of the basin following the rifting stage and the depression stage of thermal cooling. The paper collects systematically 30 regional seismic reflection profiles laid out to cover the Da'an-Dedu Fault and its adjacent14 3-D seismic projects,and on this basis,accurately tracks and interprets a total of seven seismic reflection horizons of T06,T1,T11,T2,T3,T4 and T5. At the same time,geological age of key reflection horizons is re-determined based on 52 boreholes data,the distribution characteristics and pattern of different periods are analyzed,and the geometric configuration and deformation characteristics and mechanisms of Meso-Cenozoic inversion structures developed in the northern Songliao Basin are discussed in particular. The study concludes that the inversion structure is the main deformation model of Da' anDedu Fault in the late Mesozoic and early Cenozoic,which coincides to the geometric shape and deformation mechanism of the "thrust-fold"structures.Based on the experimental shallow seismic exploration results of section line No. 10 and No. 11 in the research area,we find that the small faults,which are widely developed on the top of anticline and disconnect the reflection interface of T06,represent the latest activity of Da'an-Dedu Fault,and the deformed layer formed in mid-Pleistocene may indicate the latest activity time of Da' an-Dedu Fault,which is mid-Pleistocene.In addition,according to the study on shallow seismic exploration results,modern earthquake activity and focal mechanism solutions,we strongly believe that the latest activity of "thrust-fold "inversion structures of the Da'an-Dedu Fault has an obvious effect on the near surface reflection layers,which offsets the lower-middle Pliocene and controls the moderate-strong earthquake activity of the research area and the adjacent areas. These structures should be regarded as one of the most important and typical seismogenic structures in the interior of Songliao Basin and in the Northeast China region. Based on this,we can understand scientifically the deformation process of the interior of Songliao tectonic block through the research of structural deformation of Da'an-Dedu Fault developed inside the block after the late Cenozoic era,and the future earthquake activities controlled by the Da'an-Dedu Fault.
引文
陈娟,张庆龙,王良书,等.2008.松辽盆地长岭断陷盆地断陷期构造转换及油气地质意义[J].地质学报,82(8):1—9.CHEN Juan,ZHANG Qing-long,WANG Liang-shu,et al.2008.Tectonic transformation of Changling fault depressionin the southern Songliao Basin and its significance of hydrocarbon accumulation[J].Acta Geologica Sinica,82(8):1—9(in Chinese).
    迟元林,云金表,蒙启安.2002.松辽盆地深部结构及成盆动力学与油气聚集[M].北京:石油工业出版社.CHI Yuan-lin,YUN Jin-biao,MENG Qi-an.2002.Deep Structure and Dynamics and Oil and Gas Gathering ofSongliao Basin[M].Petroleum Industry Press,Beijing(in Chinese).
    邓起东,陈社发,赵小麟.1994.龙门山及其邻区的构造和地震活动及动力学[J].地震地质,16(4):387—403.DENG Qi-dong,CHEN She-fa,ZHAO Xiao-lin.1994.Tectonics,seismicity and dynamics of Longmenshan Mountainsand its adjacent regions[J].Seismology and Geology,16(4):387—403(in Chinese).
    邓起东,张培震,冉勇康,等,2002.中国活动构造基本特征[J].中国科学(D辑),32(12):1020—1030.DENG Qi-dong,ZHANG Pei-zhen,RAN Yong-kang,et al.2003.Basic characteristics of active tectonics of China[J].Science in China(Ser D),46(4):356—372.
    方立敏,李玉喜,陈均亮,等.2003.松辽盆地断陷末期构造特征与形成机制[J].石油地球物理勘探,38(2):190—193.FANG Li-min,LI Yu-xi,CHEN Jun-liang,et al.2003.The formation mechanism and tectonic characteristics of downfaulted Songliao Basin[J].Geophysical Prospecting for Petroleum,38(2):190—193(in Chinese).
    方石,张志强,刘招君,等.2007.松辽盆地新生代热演化及地层定年[J].吉林大学学报(地球科学版),37(5):923—928.FANG Shi,ZHANG Zhi-qiang,LIU Zhao-jun,et al.2007.Cenozoic thermal evolution and stratigraphic dating ofSongliao Basin[J].Journal of Jilin University(Earth Sciences),37(5):923—928(in Chinese).
    葛荣峰,张庆龙,王良书,等.2010.松辽盆地构造演化与中国东部构造体制转换特征[J].地质评论报,56(2):182—195.GE Rong-feng,ZHANG Qing-long,WANG Liang-shu,et al.2010.Tectonic evolution of Songliao Basin and theprominent tectonic regime transition in eastern China[J].Geological Review,56(2):182—195(in Chinese).
    黑龙江省地质矿产局.1993.黑龙江区域地质志[M].北京:地质出版社.115—145.Geology and Mineral Resources Bureau of Heilongjiang Province.1993.Regional Geology of Heilongjiang Province[M].Geological Publishing House,Beijing.115—145(in Chinese).
    韩国卿,刘永江,Franz Neubauer,等.2012.松辽盆地西缘边界断裂带中南段走滑性质、时间及其位移量[J].中国科学(D辑),42(4):471—482.HAN Guo-qing,LIU Yong-jiang,Franz Neubauer,et al.2012.Characteristics,timing,and offsets of the middlesouthern segment of the western boundary strike-slip fault of the Songliao Basin in Northeast China[J].Sciencein China(Ser D),42(4):471—482(in Chinese).
    李安,冉勇康,徐良鑫,等.2011.西南天山东柯坪推覆系古地震初步研究[J].地震地质,33(4):752—764.doi:10.3969/j.issn.0253-4967.2011.04.002.LI An,RAN Yong-kang,XU Liang-xin,et al.2011.A preliminary study on paleoearthquakes in the eastern Kalpinnappe system,southwestern Tianshan,China[J].Seismology and Geology,33(4):752—764(in Chinese).
    李娟,舒良树.2002.松辽盆地中-新生代构造特征及其演化[J].南京大学学报(自然科学版),38(4):525—531.LI Juan,SHU Liang-shu.2002.Cenozoic tectonic characteristics and evolution of Songliao Basin[J].Journal ofNanjing University(Natural Science Edition),38(4):525—531(in Chinese).
    李思田,杨士恭,吴冲龙.1987.等.中国东北部晚中生代裂陷作用和东北亚断陷盆系[J].中国科学(B辑),(2):185—195.LI Si-tian,YANG Shi-gong,WU Chong-long,et al.1987.Late Mesozoic rifting in Northeast China and Northeast Asiafault basin system[J].Science in China(Ser B),(2):185—195(in Chinese).
    刘德来,陈发景,关德范.1996.松辽盆地形成、发展与岩石圈动力学[J].地质科学,31(4):397—405.LIU De-lai,CHEN Fa-jing,GUAN De-fan.1996.Formation,development and lithospheric dynamics of SongliaoBasin[J].Chinese Journal of Geology,31(4):397—405(in Chinese).
    刘德来,马莉.1997.中生代东亚大陆边缘构造演化[J].现代地质,11(4):444—451.LIU De-lai,MA Li.1997.Mesozoic tectonic evolution of the East Asian continental margin[J].Modern Geology,11(4):444—451(in Chinese).
    刘德来,张兴洲,杨宝俊.1999.张广才岭岩石圈结构及盆岭构造[J].长春科技大学学报,29(1):26—28.LIU De-lai,ZHANG Xing-zhou,YANG Bao-jun.1999.The lithosphere structure and basin and range tectonics ofZhangguangcai Mountain[J].Journal of Changchun University of Science and Technology,29(1):26—28(inChinese).
    刘东生.1963.松辽平原的第四纪[A].见:中国地质学会编.中国地质学会第32届学术年会论文选集.北京:地质出版社.146—165.LIU Dong-sheng.1963.The Quaternary of Songliao Basin[A].In:Chinese Geological Society(ed).Proceedings ofthe 32th Annual Meeting of the Chinese Geological Society.Geological Publishing House,Beijing.146—165(inChinese).
    刘见宝,夏斌,吕宝凤,等.2010.反转构造与其易混淆构造的对比分析[J].现代地质,4:744—748.LIU Jian-bao,XIA Bin,LBao-feng,et al.2010.Comparison analysis of inversion and its confusing structure[J].Geoscience,4:744—748(in Chinese).
    刘招君,孙平昌,贾建亮,等.2011.陆相深水环境层序识别标志及成因解释:以松辽盆地青山口组为例[J].地学前缘,18(4):171—180.LIU Zhao-jun,SUN Ping-chang,JIA Jian-liang,et al.2011.Distinguishing features and their genetic interpretation ofstratigraphic sequences in continental deep water setting:A case from Qingshankou Formation in Songliao Basin[J].Earth Science Frontiers,18(4):171—180(in Chinese).
    刘俊来,Gregory A,纪沫,等.2008.地壳的拆离作用与华北克拉通破坏:晚中生代伸展构造约束[J].地学前缘,15(3):72—81.LIU Jun-lai,Gregory A,JI Mo,et al.2008.Crustal detachment and destruction of the North China craton:Constraints from Late Mesozoic structures[J].Earth Science Frontiers,15(3):72—81(in Chinese).
    裴福萍,许文良,杨德彬,等.2006.松辽盆地基底变质岩中锆石U-Pb年代学及其地质意义[J].科学通报,51(24):2881—2887.PEI Fu-ping,XU Wen-liang,YANG De-bin,et al.2006.The U-Pb chronology in basement metamorphic zircon andits geological significance of Songliao Basin[J].Chinese Science Bulletin,51(24):2881—2887(in Chinese).
    裘善文.2008.中国东北地貌第四纪研究与应用[M].长春:吉林科学技术出版社.115—165.QIU Shan-wen.2008.Quaternary Geomorphology Study and Application in Northeast China[M].Jilin Science andTechnology Press,Changchun.115—165(in Chinese).
    裘善文,王锡魁,张淑琴,等.2012.松辽平原古大湖演变及其平原的形成[J].第四纪研究,32(5):1011—1019.QIU Shan-wen,WANG Xi-kui,ZHANG Shu-qin,et al.2012.The formation and evolution of ancient large lakes inthe Songliao plain[J].Quaternary Sciences,32(5):1011—1019(in Chinese).
    裘善文,夏玉梅,李风华,等.1984.松辽平原第四纪中期古地理研究[J].科学通报,29(3):172—174.QIU Shan-wen,XIA Yu-mei,LI Feng-hua,et al.1984.Palaeogeographical study on the Songliao Plain in the middleQuaternary[J].Chinese Science Bulletin,29(3):172—174(in Chinese).
    冉勇康,陈立春,陈文山,等.2012.中国大陆古地震研究的关键技术与案例解析(2):汶川地震地表变形特征与褶皱逆断层古地震识别[J].地震地质,34(3):387—403.doi:10.3969/j.issn.0253-4967.2012.03.001.RAN Yong-kang,CHEN Li-chun,CHEN Wen-shan,et al.2012.Key techniques and several cases analysis inpaleoseismic studies in mainland China(2):Surface deformation characteristics of Wenchuan earthquake andpaleoseismic indicators on fold-reverse fault[J].Seismology and Geology,34(3):387—403(in Chinese).
    冉勇康,陈立春,沈军,等.2007.乌鲁木齐西山断裂组与地表破裂型逆断层古地震识别标志[J].地震地质,29(2):218—234.RAN Yong-kang,CHEN Li-chun,SHEN Jun,et al.2007.Xishan Fault group near Urumqi City and paleoearthquakeidentification on reverse fault[J].Seismology and Geology,29(2):218—234(in Chinese).
    单伟,刘少峰,吴键.2009.松辽盆地南缘长岭凹陷断陷层的构造特征与应变模式[J].地质通报,28(4):431—438.SHAN Wei,LIU Shao-feng,WU Jian.2009.Tectonic feature and strain pattern of Changling sag on the southern edgeof Songliao Basin,China[J].Geological Bulletin of China,28(4):431—438(in Chinese).
    邵济安,唐克东.1996.中国东北地体与东北亚大陆边缘演化[M].北京:地震出版社.SHAO Ji-an,TANG Ke-dong.1996.Terranes in Northeast China and Evolution of Northeast Asia Continent Margin[M].Seismological Press,Beijing(in Chinese).
    孙晓猛,王书琴,王英德,等.2010.郯庐断裂带北段构造特征及构造演化序列[J].岩石学报,(1):165—176.SUN Xiao-meng,WANG Shu-qin,WANG Ying-de,et al.2010.The structural feature and evolutionary series in thenorthern segment of Tancheng-Lujiang Fault zone[J].Acta Petrologica Sinica,(1):165—176(in Chinese).
    孙晓猛,朱德丰,郑常青,等.2007.松辽盆地东缘中新生代断裂构造特征、形成期次及其储层意义[J].吉林大学学报(地球科学版),6:1055—1063.SUN Xiao-meng,ZHU De-feng,ZHENG Chang-qing,et al.2007.Feature,epoch and reservoir formation significanceof the Mesozoic faults on the eastern margin at the Songliao Basin[J].Journal of Jilin University(Earth ScienceEdition),6:1055—1063(in Chinese).
    水谷申治郎,邵济安,张庆龙.1989.那丹哈达地体与东亚大陆中生代构造的关系[J].地质学报,63:204—215.Mizutani Shinjiro,HAO Ji-an,ZHANG Qing-long.1989.The Nadanhada terrane in relation to Mesozoic tectonics oncontinental margins of East Asia[J].Acta Geologica Sinica,63:204—215(in Chinese).
    唐大卿,何生,陈红汉,等.2009.伊通盆地新近纪以来的反转构造特征[J].石油学报,30(4):506—512.TANG Da-qing,HE Sheng,CHEN Hong-han,et al.2009.Characterisitcs of inversion structures in Yitong Basinsince Neogene[J].Acta Petrolei Sinica,30(4):506—512(in Chinese).
    唐克东,邵济安,李永飞,2011.松嫩地块及其研究意义[J].地学前缘,18(3):57—63.TAGN Ke-dong,SHAO Ji-an,LI Yong-fei.2011.Songnen massif and its research significance[J].Earth ScienceFrontiers,18(3):57—63(in Chinese).
    王书琴,孙晓猛,杜继宇,等.2012.郯庐断裂带北段构造样式解析[J].地质论评,(3):414—425.WANG Shu-qin,SUN Xiao-meng,DU Ji-yu,et al.2012.Analysis of structural styles in northern segment oTancheng-Lujiang Fault zone[J].Geological Review,(3):414—425(in Chinese).
    汪筱林,刘立,刘招君.1994.满洲里—绥芬河地学断面域中新生代盆地基底结构及构造演化[M].北京:地质出版社.27—37.WANG Xiao-lin,LIU Li,LIU Zhao-jun.1994.Basement Structure and Tectonic Evolution of Meso-Cenozoic Basins in theManzhouli-Suifenhe Geoscience Transect Region[M].Geological Publishing House,Beijing.27—37(in Chinese).
    吴福元,曹林.1999.东北亚若干重要基础地质问题[J].世界地质.18(2):1—8.WU Fu-yuan,CAO Lin.1999.Comment on several important basic geological problems in Northeast Asia[J].WorldGeology,18(2):1—8(in Chinese).
    吴福元,葛文春,孙德有,等.2003.中国东部岩石圈减薄研究中的几个问题[J].地学前缘,10(3):51—60.WU Fu-yuan,GE Wen-chun,SUN De-you,et al.2003.Discussins on the lithospheric thinning in eastern China[J].Earth Science Frontier,10(3):51—60(in Chinese).
    吴珍汉,吴中海,江万,等.2001.中国大陆及邻区新生代构造-地貌演化过程与机理[M].北京:地质出版社.203—204.WU Zhen-han,WU Zhong-hai,JIANG Wan,et al.2001.Evolution Process and Mechanism of Cenozoic TectonicLandforms of Chinese Continent and Its Adjacent Areas[M].Geological Publishing House,Beijing.203—204(in Chinese).
    向才富,冯志强,庞雄奇,等.2007.松辽盆地晚期热历史及其构造意义[J].中国科学(D辑),37(8):1024—1031.XIANG Cai-fu,FENG Zhi-qiang,PANG Xiong-qi,et al.2007.Thermal history and its tectonic significance oSongliao Basin during its late stage[J].Science in China(Ser D),37(8):1024—1031(in Chinese).
    夏玉梅,汪佩芳.1987.松嫩平原晚第三纪—更新世孢粉组合及古植被与古气候的研究[J].地理学报,42(2):165—178.XIA Yu-mei,WANG Pei-fang.1987.Research on late Tertiary-Pleistocene sporopollen assemblages,paleoflora andpaleoclimate in Songnen plain[J].Acta Geographica Sinica,42(2):165—178(in Chinese).
    徐嘉炜,马国锋.1992.郯庐断裂带研究的十年回顾[J].地质论评,38(4):316—324.XU Jia-wei,MA Guo-feng.1992.Review of ten-years research on the Tancheng-Lujiang Fault zone[J].GeologicaReview,38(4):316—324(in Chinese).
    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].Journaof Geology and Mineral Resources of North China,10(2):121—134(in Chinese).
    杨宝俊,穆石敏.1996.中国满洲里—绥芬河地学断面地球物理综合研究[J].地球物理学报,39(6):772—782.YANG Bao-jun,MU Shi-min.1996.Synthesized study on the geophysics of Manzhouli-Suifenhe Geoscience Transec[J].Chinese Journal of Geophysics,39(6):772—782(in Chinese).
    杨宝俊,唐建人.2003.松辽盆地隆起区地壳反射结构与“断开”莫霍界面[J].中国科学(D辑),33(2)170—176.YANG Bao-jun,TANG Jian-ren.2003.Crustal reflection structure in the uplifting zone of Songliao Basin andisconnecting Moho interface[J].Science in China(Ser D),33(2):170—176(in Chinese).
    杨秉庚,孙肇春,吕金福.1983.松辽水系的变迁[J].地理研究,2(1):48—56.YANG Bing-geng,SUN Zhao-chun,LJin-fu.1983.The change of Songliao drainage patterns[J].GeographicaResearch,2(1):48—56(in Chinese).
    杨文采.1989.地球物理反演和层析成像[M].北京:地质出版社.137—160.YANG Wen-cai.1989.Geophysical Inversion and Tomography[M].Geological Publishing House,Beijing.137—160(in Chinese).
    叶高峰,魏文博,金胜,等.2009.郯庐断裂带中段电性结构及其地学意义研究[J].地球物理学报,112818—2825.YE Gao-feng,WEI Wen-bo,JIN Sheng,et al.2009.Study of the electrical structure and its geological meanings othe middle part of Tancheng-Lujiang Fault zone[J]Chinese Journal of Geophysics,11:2818—2825(iChinese).
    余中和,李玉文,韩守华,等.2001.松辽盆地古生代构造演化[J].大地构造与成矿学,25(4):389—396.YU Zhong-he,LI Yu-wen,HAN Shou-hua,et al.2001.The Paleozoic tectonic evolution of Songliao Basin[J]Geotectonica et Metallogenia,25(4):389—396(in Chinese).
    尉迟正荣.1930,嫩江流域近况[J].地学杂志,(2):273—291.YUCHI Zheng-rong.1930.The recent situation of the Nenjiang drainage area[J].The Geographical Journal,(2)273—291.
    张培震,邓起东,徐锡伟,等.1994.盲断层“褶皱地震”与1906年玛纳斯地震[J].地震地质,16(3):193—204.ZHANG Pei-zhen,DENG Qi-dong,XU Xi-wei,et al.1994.Blind thrust,folding earthquake,and the 1906 Manaearthquake,Xinjiang[J].Seismology and Geology,16(3):193—204(in Chinese).
    张培震,邓起东,张国民,等.2003.中国大陆的强震活动与活动地块[J].中国科学(D辑),S1:12—20.ZHANG Pei-zhen,DENG Qi-dong,ZHANG Guo-min,et al.2003.Active tectonic blocks and strong earthquakes ithe continent of China[J].Science in China(Ser D),S1:12—20(in Chinese).
    张贻侠,孙运生,张兴洲,等.1999.中国满洲里—绥芬河地学断面[M].北京:地质出版社.ZHANG Yi-xia,SUN Yun-sheng,ZHANG Xing-zhou,et al.1999.The Manzhouli-Suifenhe Geoscience Transec[M].Geological Publishing House,Beijing(in Chinese).
    张庆龙,王良书,解国爱,等.2005.郯庐断裂带北延及中新生代构造体制转换问题的探讨[J].高校地质学报,11(4):577—584.ZHANG Qing-long,WANG Liang-shu,XIE Guo-ai,et al.2005.Discussion on northward extension of the Tanlu Faulzone and its tectonic regime transformation[J].Geological Journal of China Universities,11(4):577—584(iChinese).
    张庸,王锡魁.1995.满洲里—绥芬河地学断面域及邻区新构造运动[M].长春:吉林大学出版社.73—74.ZHANG Yong,WANG Xi-kui.1995.Research on Neotectonic Movement in the Manzhouli-Suifenhe GeoscienceTransect Region and Its Adjacent Areas[M].Jilin University Press,Changchun.73—74(in Chinese).
    赵越,杨振宇,马醒华.1994.东亚大地构造发展的重要转折[J].地质科学,29(2):105—119.ZHAO Yue,YANG Zhen-yu,MA Xing-hua.1994.An important turning point of the development of East Asiantectonics[J].Chinese Journal of Geology,29(2):105—119(in Chinese).
    Hu Wang-shui.1998.Structural style and its relation to hydrocarbon on exploration in the Songliao Basin,NortheastChina[J].Marine and Petroleum Geology,15(1):41—55.
    Liu Jun-lai,Davis G A,Wu Fu-yuan.2005.The Liaonan metamorphic core complex,southeastern Liaoning Province,North China:A likely contributor to Cretaceous rotation of eastern Liaoning,Korea and contiguous areas[J].Tectonophysics,407(1):65—80.
    Otsuki K.1997.Oblique subduction,collision of microcontinents and subduction of oceanic ridge:Their implicationson the Cretaceous tectonics of Japan[J].Island Arc,1(1):51—63.
    Song Tian-guang.1997.Inversion styles in the Songliao Basin(Northeast China)and estimation of the degree ofinversion[J].Tectonophysics,283(1-4):173—188.
    Wallis S R,Anczkiewicz R,Endo S,et al.2009.Plate movements,ductile deformation and geochronology of theSanbagawa belt,SW Japan:Tectonic significance of 89-88Ma Lu-Hf eclogite ages[J].Journal of MetamorphicGeology,27(2):93—105.
    Yin Wei,Fan Zi-fei,Zheng Jun-zhang,et al.2012.Characteristics of strike-slip inversion structures of the KaratauFault and their petroleum geological significances in the South Turgay Basin,Kazakhstan[J].PetroleumScience,9(4):444—454.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心