天山北麓活动背斜带的变形特征
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:TECTONIC DEFORMATION OF ACTIVE FAULT-RELATED FOLD BELTS IN THE NORTH PIEDMONT OF THE CENTRAL TIANSHAN MOUNTAINS,NW CHINA
  • 作者:吕红华 ; 李有利
  • 英文作者:Lu Honghua~① Li Youli~② (①State Key Laboratory of Marine Geology,Tongji University,Shanghai 200092; ②Laboratory for Earth Surface Processes,Ministry of Education,College of Urban and Environmental Sciences,Peking University,Beijing 100871)
  • 关键词:活动褶皱 ; 地壳缩短 ; 构造迁移 ; 晚新生代 ; 天山北麓
  • 英文关键词:active fold;;crustal shortening;;tectonic migration;;Late Cenozoic;;north piedmont of the Tianshan Mountains
  • 中文刊名:DSJJ
  • 英文刊名:Quaternary Sciences
  • 机构:同济大学海洋地质国家重点实验室;北京大学城市与环境学院地表过程与模拟教育部重点实验室;
  • 出版日期:2010-09-30
  • 出版单位:第四纪研究
  • 年:2010
  • 期:v.30
  • 基金:国家自然科学基金项目(批准号:40971001);; 中国博士后科学基金项目(批准号:20090450727)资助
  • 语种:中文;
  • 页:DSJJ201005021
  • 页数:9
  • CN:05
  • ISSN:11-2708/P
  • 分类号:151-159
摘要
天山中段北麓发育有3排受逆断裂控制的背斜带,对这些构造带的研究有助于认识天山及其前陆盆地晚新生代构造变形的机理。基于地层变形分析,并结合前人的研究成果,从整体上探讨了这3排构造带的变形时间与基本模式。分析表明,天山北麓第Ⅰ排构造带的托斯台背斜自中新世褶皱作用明显;第Ⅱ排构造带吐谷鲁背斜于约6.0Ma开始生长,伴随发育同构造沉积即生长地层;第Ⅲ排构造带独山子背斜发育时间应晚于约2.6Ma。这一变形时间序列揭示天山北麓3排逆断裂-褶皱带的构造变形具有向前陆盆地逐步扩展的特征,并伴随产生幅度不等的地壳缩短。天山北麓约8~15km的地壳缩短总量表明,晚新生代以来构造驱动沿约130km宽的山麓带是相对均一的。
        In the north piedmont of the Tianshan Mountains, there are three sub-parallel reverse fault-controlled fold belts. They are products of Late Cenozoic tectonic deformation. In fold belt Ⅰ, the Tuositai anticline is a typical structure we studied. It has risen since the Miocene, although it sprouted in the Late Mesozoic. In fold belt Ⅱ,we studied the Tugulu anticline. It began deforming in about. 6.0Ma, accompanied with syntectonic deposition, and then experienced two times of obvious deformation,respectively in 5.2Ma and 3.5Ma. In fold belt Ⅲ,the Dushanzi anticline was studied. It should began deforming after about 2.6Ma because Neogene-Pleistocene strata were folded. That the Middle Pleistocene strata unconformably overlie the Lower Pleistocene Xiyu conglomerate indicates that its significant deformation should be in Early to Middle Pleistocene. The deformation sequence of these Late Cenozoic anticlines shows that tectonic deformation has progressively migrated northward. At the same time, a significant crustal shortening occurred in the north piedmont of the Tianshan Mountains. It was estimated that the total magnitude of shortening there should range from 8km to 15km.
引文
1 张培震,邓起东,杨晓平等.天山的晚新生代构造变形及其地球动力学问题.中国地震,1996,12(2) :127-140 Zhang Peizhen,Deng Qidong,Yang Xiaoping et al.Late Cenozoic tectonic deformation and mechanism along the Tianshan Mountain,North Western China.Earthquake Research in China,1996,12(2) :127-140
    2 张培震.天山及其前陆盆地的晚新生代构造变形.科学通报,2003,48(24) :2499-2500 Zhang Peizhen.Late Cenozoic tectonic deformation in the Tianshan Mountain and its foreland basins.Chinese Science Bulletin,2004,49(4) :311-313
    3 邓起东,冯先岳,张培震等.天山活动构造.北京:地震出版社,2000. 339 Deng Qidong,Feng Xianyue,Zhang Peizhen et al.Active Tectonics of the Tian Shan Mountains.Beijing:Seismology Press,2000. 399
    4 陈杰,WyrwoH K H,卢演俦等.祁连山北缘玉门砾岩的磁性地层年代与褶皱过程.第四纪研究,2006,26(1) :20-31 Chen Jie,Wyrwoll K H,Lu Yanchou et al.Magnetochronology of the Yumen conglomerates and multi-pulsed folding and thrusting in the northern Qilianshan.Quaternary Sciences,2006,26(1) :20-31
    5 陈杰,卢演俦,丁国瑜.塔里木西缘晚新生代造山过程的记录-磨拉石建造及生长地层和生长不整合.第四纪研究,2001,21(6) :528-539 Chen Jie,Lu Yanchou,Ding Guoyu.Records of Late Cenozoic mountain building in Western Tarim Basin:Molasses,growth strata and growth unconformity.Quaternary Sciences,2001,21(6) :528-539
    6 张培震,邓起东,徐锡伟等.天山北麓玛纳斯活动逆断裂-褶皱带的变形特征与构造演化.见:活动断裂研究编辑委员会编.动断裂研究(3) .北京:地震出版社,1994. 18-32 Zhang Peizhen,Deng Qidong,Xu Xiwei et al.Tectonic deformation,crustal shortening,and slip rate estimation along the Manas reverse fault-fold zone in the north flank of the Tian Shan Mountains.In:Committee of the Research of Active Fault ed.Research of Active Fault(3) .Beijing:Seismology Press,1994. 18-32
    7 李军,冯先岳,陈杰等.霍尔果斯活动逆断裂-褶皱构造研究.见:活活动断裂研究编辑委员会编.活动断裂研究(2) .北京:地震出版社,1992. 105-116 Li Jun,Feng Xianyue,Chen Jie et al.Thrusting and folding of Huoerguos anticline in Xinjiang.In:Committee of the Research of Active Fault ed.Research of Active Fault(2) .Beijing:Seismology Press,1992. 105-116
    8 徐锡伟,邓起东,张培震等.新疆玛纳斯-霍尔果斯逆断裂-褶皱带河流阶地的变形及其构造含义.见:活动断裂研究编辑委员会编.活动断裂研究(2) .北京:地震出版社,1992. 117-127 Xu Xiwei,Deng Qidong,Zhang Peizhen et al.Deformation of river terraces across the Manas-Huoerguos reverse fault and fold zone and its neotectonic implication in Xinjiang.In:Committee of the Research of Active Fault ed.Research of Active Fault(2) .Beijing:Seismology Press,1992. 117-127
    9 Avouac J-P,Tapponnier P,Bai M et al.Active thrusting and folding along the northern Tien Shan and Late Cenozoic rotation of the Tarim relative to Dzungaria and Kazakhstan.Journal of Geophysical Research,1993,98(B4) :6755-6804
    10 Molnar P,Brown E T,Burchfiel B C et al.Quaternary climate change and the formation of river terraces across growing anticlines on the north flank of the Tien Shan,China.The Journal of Geology,1994,102:583-602
    11 杨晓平,邓起东,张培震等.利用阶地变形数据研究北天山吐谷鲁逆断裂-背斜带晚更新世以来的褶皱变形特征.见:活动断裂研究编辑委员会编.活动断裂研究(4) .北京:地震出版社,1995. 46-62 Yang Xiaoping,Deng Qidong,Zhang Peizhen et al.Fold deformation along the Tugulu reverse fault-fold zone since Late Pleistocene,North Tianshan.In:Committee of the Research of Active Fault ed.Research of Active Fault (4) .Beijing:Seismology Press,1995. 46-62
    12 杨晓平,邓起东,冯先岳.北天山吐谷鲁活动逆断裂-背斜几何学运动学特征研究.见:活动断裂研究编辑委员会编.活动断裂研究(5) .北京:地震出版社,1996. 42-53 Yang Xiaoping,Deng Qidong,Feng Xianyue.Research on geometry,kinematics of Tugulu active reverse fault-fold in the north flank of the Tian Shan Mountains.In:Committee of the Research of Active Fault ed.Research of Active Fault(5) .Beijing:Seismology Press,1996. 42-53
    13 杨晓平,邓起东.新疆独山子背斜的断裂扩展褶皱作用.见:活动断裂研究编辑委员会编.活动断裂研究(3) .北京:地震出版社,1998. 66-73 Yang Xiaoping,Deng Qidong.The fault-propagation foldingof the Dushanzi anticline,Northern Tianshan,Xinjiang.In:Committee of the Research of Active Fault ed.Research of Active Fault (3) .Beijing:Seismology Press,1998. 66-73
    14 Burchfiel B,Brown E,Deng Qidong et al.Crustal shortening on the margins of the Tien Shan,Xinjiang,China.International Geology Review,1999,41(8) :665-700
    15 方世虎,贾承造,郭召杰等.准噶尔盆地南缘前陆冲断带形成时 间的初步厘定.地学前缘,2005,12(3) :66 Fang Shihu,Jia Chengzao,Guo Zhaojie et al.Ages of the foreland thrust-fault belts along southern edge of Junggar Basin.Earth Science Frontiers,2005,12(3) :66
    16 郭召杰,方世虎,张锐等.生长地层及其在判断天山北缘前陆冲断褶皱带形成时间上的应用.石油与天然气地质,2006,27(4) :475-481 Guo Zhaojie,Fang Shihu,Zhang Rui et al.Growth strata and their application in timing deformation of foreland thrust-fold belts in the north margin of Tianshan.Oil & Gas Geology,2006,27(4) :475-481
    17 王胜利,Chen Yan,卢华复.天山北麓霍尔果斯背斜晚中新世以来翼旋转方式的生长.科学通报,2008,53(12) :1414-1421 Wang Shengli,Chen Yan,Lu Huafu.Growth of the Huoerguosi anticline (North Tianshan Mountains)by limb rotation since Late Miocene.Chinese Science Bulletin,2008,53 (19) :3028-3036
    18 Charreau J,Sun Jimin,Chen Yan et al.Addendum to "Late Cenozoic magnetochronology and paleoenvironmental changes in the northern foreland basin of the Tian Shan Mountains" by Jimin Sun,Qinghai Xu,and Baochun Huang.Journal of Geophysical Research,2008,113:B06103,doi:10. 1029/2007JB005489
    19 Charreau J,Chen Yah,Gilder S et al.Neogene uplift of the Tian Shan Mountains observed in the magnetic record of the Jingou River section (North West China).Tectonics,2009,28(2) :TC2008,doi:10. 1029/2007TC002137
    20 Ji Junliang,Luo Pan,White P et al.Episodic uplift of the Tianshan Mountains since the Late Oligocene constrained by magnetostratigraphy of the Jingou River section,in the southern margin of the Junggar Basin,China.Journal of Geophysical Research,2008,113(B5) :B05102,doi:10. 1029/2007JB005064
    21 Sun Jimin,Zhang Zhenqing.Syntectonic growth strata and implications for Late Cenozoic tectonic uplift in the Northern Tian Shan,China.Tectonophysics,2009,463:60-68
    22 Daeron M,Avouac J-P,Charreau J.Modeling the shortening history of a fault tip fold using structural and geomorphic records of deformation.Journal of Geophysical Research,2007,112:B03S13,doi:10. 1029/2006JB004460
    23 Charreau J,Avouac J-P,Chen Yan et al.Miocene to present kinematics of fault-bend folding across the Huerguosi anticline,Northern Tianshan (China),derived from structural,seismic,and magnetostratigraphic data.Geology,2008,36(11) :871-874
    24 Fu Bihong,Lin Aiming,Kano K-I et al.Quaternary folding of the eastern Tian Shan,North West China.Tectonophysics,2003,369:79-101
    25 吕红华,李有利,刘运明等.新疆塔西河地区8Ma以来沉积环境演化及其构造意义.第四纪研究,2008,28(2) :243-252 Lu Honghua,Li Youfi,Liu Yunming et al.Sedimentary environment evolution since 8MaB.P.in the Taxihe area,Xingjiang,North West China and its tectonic significance.Quaternary Sciences,2008,28(2) :243-252
    26 史兴民,杨景春,李有利等.天山北麓玛纳斯河河流阶地变形与新构造运动.北京大学学报(自然科学版),2004,40(6) :971- 978 Shi Xingmin,Yang Jingchun,Li Youli et al.Deformation of Manas River terraces and Neotectonics in northern front of the Tianshan Mountains.Acta Scientiarum Naturalium Universitatis Pekinesis,2004,40(6) :971-978
    27 袁庆东,郭召杰,张志诚等.天山北缘河流阶地形成及构造变形定量分析.地质学报,2006,80(2) :210-216 Yuan Qingdong,Guo Zhaojie,Zhang Zhicheng et al.The Late Cenozoic deformation of terraces on the north flank of the Tianshan Mt.and the tectonic evolution.Acta Geologica Sinica,2006,80(2) :210-216
    28 Bullen M E,Burbank D W,Garver J I et al.Late Cenozoic tectonic evolution of the north Western Tien Shan:New age estimates for the initiation of mountain building.Geological Society of America Bulletin,2001,113(12) :1544-1559
    29 Allen M B,Windley B F,Chi Zheng et al.Basin evolution within and adjacent to the Tien Shan Range,NW China.Journal of the Geological Society,1991,148:369-378
    30 Abdrakhmatov K Y,Weldon R J,Thompson S C et al.Onset,style and current rate of shortening in the Central Tien Shan,Kyrgyz Republic.Russian Geology and Geophysics,2001,42:1585-1609
    31 Bullen M E,Burbank D W,Garver J.Building the northern Tien Shan:Integrated thermal,structural,and topographic constraints.Journal of Geology,2003,111:149-165
    32 Sobel E R,Oskin M,Burbank D et al.Exhumation of basementcored uplifts:Example of the Kyrgyz Range quantified with apatite fission track thermochronology.Tectonics,2006,25:TC2008,doi:10. 1029/2005TC001809
    33 Windley B F,Alien M B,Zhang C et al.Paleozoic accretion and Cenozoic redeformation of the Chinese Tien Shan Range,Central Asia.Geology,1990,18:128-131
    34 Chen Jie,Burbank D W,Scharer K M et al.Magnetochronology of the Upper Cenozoic strata in the South Western Chinese Tian Shan:Rates of Pleistocene folding and thrusting.Earth and Planetary Science Letters,2002,195:113-130
    35 Chen Jie,Heermance R,Burbank D W et al.Quantification of growth and lateral propagation of the Kashi anticline,South West Chinese Tian Shan.Journal of Geophysical Research,2007,112:B03S16,doi:10. 1029/2006JB004345
    36 Suppe J,Chou G T,Hook S C.Rate of folding and faulting determined from growth strata.In:McClay K R ed.Thrust Tectonics.New York:Champman & Hi11,1992. 105-122
    37 Poblet J,McClay K,Storti F et al.Geometries of syntectonic sediments associated with single-layer detachment folds.Journal of Structural Geology,1997,19(3-4) :369-381
    38 张广良,张培震,阂伟等.逆冲-褶皱造山过程中生长地层的识别及应用.地震地质,2006,28(2) :299-311 Zhang Guangliang,Zhang Peizhen,Min Wei et al.The identification and application of growth strata linked to the foreland fold-and-thrust belt during mountain building.Seismology and Geology,2006,28(2) :299-311
    39 许春明,贺晓苏,吴晓智等.准噶尔盆地托斯台地区构造分析及 油气勘探前景.新疆石油地质,1992,13(3) :197-205 Xu Chunming,He Xiaosu,Wu Xiaozhi et al.Structure analysis and petroleum exploration prospect of Tostai area in Junggar Basin.Xinjiang Petroleum Geology,1992,13(3) :197-205
    40 Lu Honghua,Burbank D W,Li Youli et al.Late Cenozoic structural and stratigraphic evolution of the northern Chinese Tian Shan foreland.Basin Research,2009,22(3) :249-269,doi:10. 1111/j.1365-2117. 2009. 00412
    41 Heermanee R V,Chen Jie,Burbank D W et al.Chronology and tectonic controls of Late Tertiary deposition in the south Western Tian Shan foreland,NW China.Basin Research,2007,19:599-632
    42 陈杰,Heermance R V,Burbank D W et al.中国西南天山西域砾岩的磁性地层年代与地质意义.第四纪研究,2007,27(4) :576-578 Chen Jie,Heermance R V,Burbank D W et al.Magnetochronology and its implications of the Xiyu conglomerate in the south Western Chinese Tian Shan foreland.Quaternary Sciences,2007,27(4) :576-578
    43 Sun J M,Zhu R X,Bowler J.Timing of the Tianshan Mountains uplift constrained by magnetostratigraphie analysis of molasses deposits.Earth and Planetary Science Letters,2004,219:239-253
    44 Sun Jimin,Xu Qinghai,Huang Baochun.Late Cenozoic magnetochronology and paleoenvironmental changes in the northern foreland basin of the Tian Shan Mountains.Journal of Geophysical Research,2007,112:B04107. 1-B04107. 14,doi:10. 1029/2006JB004653
    45 Rafini S,Mercier E.Forward modelling of foreland basins progressive unconformities.Sedimentary Geology,2002,146(1-2) :75-89
    46 邓起东,冯先岳,尤惠川等.新疆独山子-安集海活动逆断裂-褶皱带的变形特征及其形成机制.见:活活动断裂研究编辑委员会编.活动断裂研究(1) .北京:地震出版社.1991. 17-36 Deng Qidong,Feng Xianyue,You Huichuan et al.Characteristics and mechanism of deformation along the Dushanzi-Anjihai active reverse fault and fold zone,Xinjiang.In:Committee of the Research of Active Fault ed.Research of Active Fault(1) .Beijing:Seismology Press,1991. 17-36
    47 Charreau J,Chen Yah,Gilder S et al.Magnetostratigraphy and rock magnetism of the Neogene Kuitun He section(North West China):Implications for Late Cenozoic uplift of the Tianshan mountains.Earth and Planetary Science Letters,2005,230:177-192
    48 孙继敏,朱日祥.天山北麓晚新生代沉积及其新构造与古环境指示意义.第四纪研究,2006,26(1) :14-19 Sun Jimin,Zhu Rixiang.Cenozoic deposits in the northern Tianshan Mountains and its implications for neotectonics and environmental changes.Quaternary Sciences,2006,26(1) :14-19

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700