帕米尔构造结及邻区的晚新生代构造与现今变形

doi:10.3969/j.issn.0253-4967.2011.02.001

摘要/Abstract

摘要：

帕米尔构造结是中国大陆受板块动力作用和地震活动最强烈的地区之一。晚新生代帕米尔构造结北部向北楔入推移了约300km,但对这一变形过程至今未能很好的限定。帕米尔构造结的晚新生代构造变形在空间上是不对称的。帕米尔西缘表现为NW向的径向逆冲,伴随着塔吉克盆地东部块体绕垂直轴的逆时针旋转。在帕米尔东部,构造变形的方式、空间分布和机制是随时间变化的。在渐新世末至约11Ma,帕米尔东部以喀什-叶城转换带(KYTS)的右旋走滑作用为主,同时帕米尔前缘沿主帕米尔逆断层(MPT)发生强烈缩短作用,塔里木向南俯冲,帕米尔中、下地壳相对于上地壳向北俯冲并加厚、熔融。弧形弯曲或径向逆冲作用以及中、下地壳的加厚、弱化致使公格尔山拉张系北部于7～8Ma开始EW向拉张作用,并向南扩展。至3～5Ma,构造格局发生了巨变,喀喇昆仑右旋走滑断裂北段停止活动; KYTS右旋走滑由早期的11～15mm/a明显减小至1.7～5.3mm/a; 帕米尔构造结与塔里木块体间的相对运动明显减弱,两者可能已拼接在一起作为一个整体以(21±1)mm/a的速率向北推挤,变形前锋向北迁移至克孜勒苏河一线。帕米尔构造结及邻区晚第四纪及现今的活动变形主要集中在公格尔拉张系、帕米尔前缘褶皱-逆断层带(PFT)与南天山南缘的阿图什-喀什褶皱带上。

关键词: 帕米尔构造结, 晚新生代构造, 拉张作用, 径向逆冲, 弧形弯曲

Abstract:

The northern margin of the Pamir salient indented northward by ～300km during the late Cenozoic,however,the spatiotemporal evolution of this process is still poorly constrained.Regional deformation within the Pamir salient is asymmetric.Previous work has shown that deformation along the western flank of the Pamir was accommodated by northwest-directed radial thrusting and associated anticlockwise vertical axis rotation of the Pamir over the eastern margin of the Tajik Basin,along with a component of left-slip faulting along the Darvaz Fault.In contrast,subduction of the Tajik-Tarim Basin beneath the Pamir along the MPT was absorbed along the eastern margin of the salient by dextral-slip along the Kashgar-Yecheng transfer system,accompanied with Oligocene-Miocene northward underthrusting, thickening and widespread melting of the middle and lower crust beneath the Pamir,eventually led to east-west extension along the Kongur Shan extensional system at ～7～8Ma.The slip rate of the KYTS decreased substantially from 11～15mm/a to 1.7～5.3mm/a since at least 3～5Ma,termination of slip along the northern segment of the Karakorum Fault occurred almost at the same time.Late Quaternary and present active deformation in the Pamir is dominated by east-west extension along the Kongur Shan extensional system and north-south contraction along the PFT and the Atux-Kashi fold belts in the southern margin of Tianshan.

Key words: Pamir salient, late Cenozoic deformation, east-west extension, radial thrusting, oroclinal bending

中图分类号:

P315.2

陈杰, 李涛, 李文巧, 袁兆德. 帕米尔构造结及邻区的晚新生代构造与现今变形[J]. 地震地质, 2011, 33(2): 241-259.

CHEN Jie, LI Tao, LI Wen-qiao, YUAN Zhao-de. LATE CENOZOIC AND PRESENT TECTONIC DEFORMATION IN THE PAMIR SALIENT,NORTHWESTERN CHINA[J]. SEISMOLOGY AND GEOLOGY, 2011, 33(2): 241-259.

参考文献

陈汉林,张芬芬,程晓敢,等.2010.帕米尔东北缘地区构造变形特征与盆山构造［J］.地质科学,45(1): 102-112.
CHEN Han-lin,ZHANG Fen-fen,CHENG Xiao-gan,et al.2010.The deformation features and basin-range coupling structure in the northeastern Pamir tectonic belt ［J］.Chinese Journal of Geology,45(1): 102-112(in Chinese).
陈杰,曲国胜,胡军,等.1997.帕米尔北缘弧形推覆构造带东段的基本特征与现代地震活动［J］.地震地质,19(4): 301-312.
CHEN Jie,QU Guo-sheng,HU Jun,et al.1997.Arcuate thrust tectonics and its contemporary seismicity in the eastern section of the external zone of the Pamir ［J］.Seismology and Geology,19(4): 301-312(in Chinese).
陈杰,Heermance R,Burbank D W,et al.2007.中国西南天山西域砾岩的磁性地层年代与地质意义［J］.第四纪研究,27(4): 576-587.
CHEN Jie, Heermance R,Burbank D W,et al. 2007. Magnetochronology and implications of the Xiyu conglomerate in the southwestern Chinese Tianshan foreland ［J］.Quaternary Sciences,27(4):576-587(in Chinese).
冯先岳.1997.新疆古地震［M］.新疆: 新疆科技卫生出版社.33-34.
FENG Xian-yue.1997.The Paleoearthquakes in Xinjiang Region,China ［M］.Xinjiang Science,Technology and Health Publishing House,Urumchi.33-34(in Chinese).
柯珊,罗照华,莫宣学,等.2008.帕米尔构造结塔什库尔干碱性杂岩同位素年代学研究［J］.岩石学报,24(2): 315-324.
KE Shan,LUO Zhao-hua,MO Xuan-xue,et al.2008.The geochronology of Taxkorgan alkalic complex,Pamir syntax ［J］.Acta Petrologica Sinica,24(2): 315-324(in Chinese).
李涛,陈杰,肖伟鹏,等.2011a.利用变形河流阶地限定帕米尔北缘木什背斜的缩短、隆升和侧向扩展［J］.地震地质,33(2): 308-322.
LI Tao,CHEN Jie,XIAO Wei-peng,et al.2011a.Using deformation terraces to confine the shortening,uplift and lateral propagation of the Mushi anticline,northern margin of the Pamir ［J］.Seismology and Geology,33(2): 308-322(in Chinese).
李涛,陈杰,肖伟鹏,等.2011b.西南天山前缘乌拉根背斜南翼逆断层的发现及其地质意义［J］.地震地质,33(2): 277-288.
LI Tao,CHEN Jie,XIAO Wei-peng,et al.2011b.The discovery and geological significance of the thrust at the south limb of Wulagen anticline, south margin of the southwestern Tianshan ［J］.Seismology and Geology,33(2): 277-288(in Chinese).
李文巧,陈杰,袁兆德,等.2011.帕米尔高原1895年塔什库尔干地震地表多段同震破裂与发震构造［J］.地震地质,33(2): 260-276.
LI Wen-qiao,CHEN Jie,YUAN Zhao-de,et al.2011.Coseismic surface ruptures of multi segments and seismogenic fault of the Tashkorgan earthquake in Pamir,1895 ［J］.Seismology and Geology,33(2): 260-276(in Chinese).
罗照华,莫宣学,柯珊,等.2003.塔什库尔干碱性杂岩体形成时代及其地质意义［J］.新疆地质,21(1): 46-50.
LUO Zhao-hua,MO Xuan-xue,KE Shan,et al.2003.Ages of Taxkorgan alkakine intrusive complex and their geological implications ［J］.Xinjiang Geology,21(1): 46-50(in Chinese).
牛之俊,游新兆,杨少敏.2007.利用GPS分析天山现今地壳形变特征［J］.大地测量与地球动力学,27(2): 1-9.
NIU Zhi-jun,YOU Xin-zhao,YANG Shao-min.2007.Analysis of contemporary crustal deformation characteristics with GPS data of Tianshan Mountain ［J］.Journal of Geodesy and Geodynamics,27(2): 1-9(in Chinese).
曲国胜,李亦纲,张宁,等.2004.塔里木西南缘(齐姆根弧)前陆构造及形成机理［J］.地质论评,50(6): 567-576.
QU Guo-sheng,LI Yi-gang,ZHANG Ning,et al.2004.A study on the foreland structure of the Qimugen Arc in southwest Tarim and its genetic mechanism ［J］.Geological Review,50(6): 567-576(in Chinese).
尚新璐,陈新卫,吴超,等.2004.塔里木盆地西部喀什地区的新生代冲断构造［J］.地质科学,39(4): 543-550.
SHANG Xin-lu,CHEN Xin-wei,WU Chao,et al.2004.Cenozoic thrust structures in the Kashi area,western Tarim Basin ［J］.Chinese Journal of Geology,39(4): 543-550(in Chinese).
王琪,丁国瑜,乔学军,等.2000.天山现今地壳快速缩短与南北地块的相对运动［J］.科学通报,45(14): 1543-1547.
WANG Qi,DING Guo-yu,QIAO Xue-jun,et al.2000.Present-day crustal shortening and relative movement of northsouthern block in Tianshan ［J］.Chinese Science Bulletin,45(14): 1543-1547(in Chinese).
肖序常,王军.2004.西昆仑-喀喇昆仑及其邻区岩石圈结构、演化中几个问题的探讨［J］.地质论评,50(3): 285-294.
XIAO Xu-chang,WANG Jun.2004.Discussion on the lithospheric structure and evolution of the West Kunlun Mountains-Karakorum Mountains and their adjacent areas ［J］.Geological Review,50(3): 285-294(in Chinese).
肖伟鹏,陈杰,李涛,等.2011.帕米尔北缘木什背斜第四纪滑脱褶皱作用与北翼逆断裂的生长［J］.地震地质,23(3): 289-307.
XIAO Wei-peng,CHEN Jie,LI Tao,et al.2011.Quaternary detachment folding and propagation of north limb fault of Mushi anticline,northern margin of the Pamir ［J］.Seismology and Geology,33(2): 289-307(in Chinese).
谢毓寿,蔡美彪主编.1987.中国地震历史资料汇编(第三卷)［Z］.北京: 科学出版社.
XIE Yu-shou,CAI Mei-biao(eds).1987. Collection of Historical Materials of Chinese Earthquake Vol.3 ［Z］.Science Press,Beijing(in Chinese).
张家声,单新建,李建华,等.2005.帕米尔地区现今大陆深俯冲-地震构造和动力学解释［J］.岩石学报,21(4): 1215-1227.
ZHANG Jia-sheng,SHAN Xin-jian,LI Jian-hua,et al.2005.Recent deep subducting of continental crust in Pamir: An interpretation on seismotectonics and geodynamics ［J］.Acta Petrologica Sinica,21(4): 1215-1227(in Chinese).
Amidon W H,Hynek S A.2010.Exhumational history of the north central Pamir ［J］.Tectonics,29: TC5017.doi: 10.1029/2009TC002589.
Arnaud N O,Brunel M,Cantagrel J M,et al.1993.High cooling and denudation rates at Kongur Shan,eastern Pamir(Xinjiang,China)revealed by ⁴⁰ Ar/³⁹ Ar alkali feldspar thermochronology ［J］.Tectonics,12: 1335-1346.
Arrowsmith J R,Strecker M R.1999.Seismotectonic range-front segmentation and mountain-belt growth in the Pamir-Alai region,Kyrgyzstan(India-Eurasia collision zone)［J］.Geological Society of America Bulletin,111: 1665-1683.doi: 10.1130/0016-7606(1999)111<1665: SRFSAM>2.3.CO; 2.
Avouac J P,Peltzer G.1993.Active tectonics in southern Xinjiang,China: Analysis of terrace riser and normal fault scarp degradation along the Hotan-Qira Fault system ［J］.Journal of Geophysical Research,98(21): 773-807.doi: 10.1029/93JB02172.
Blisniuk P M,Strecker M R.1996.Kinematics of Holocene normal faulting in the Northern Pamir ［J］.Eos(Transactions,American Geophysical Union),77(46): F693.
Brookfield M,Hashma A.2001.The geology and petroleum potential of the North Afghan platform and adjacent areas(northern Afghanistan,with parts of southern Turkmenistan,Uzbekistan and Tajikistan)［J］.Earth Sci Rev,55: 41-71.
Brown E T,Molnar P,Bourlés D L.2005.Comment on "Slip-rate measurements on the Karakorum Fault may imply secular variations in fault motion" ［J］.Science,309: 1326b.
Brunel M,Arnaud N,Tapponnier P,et al.1994.Kongur Shan normal fault: Type example of mountain building assisted by extension(Karakoram Fault,eastern Pamir)［J］.Geology,22: 707-710.
Burtman V S.2000.Cenozoic crustal shortening between the Pamir and Tien Shan and a reconstruction of the Pamir-Tian Shan transition zone for the Cretaceous and Palaeogene ［J］.Tectonophysics,319: 69-92.
Burtman V S,Molnar P.1993.Geological and geophysical evidence for deep subduction of continental crust beneath the Pamir ［J］.Special Paper Geol Soc Am,281: 76.
Chen Y,Cogné J,Courtillot V.1992.New Cretaceous paleomagnetic poles from Tarim Basin,Northwestern China ［J］.Earth and Planetary Science Letters,114: 17-38.doi: 10.1016/0012-821X(92)90149-P.
Coutand Ⅰ,Strecker M R,Arrowsmith J R,et al.2002.Late Cenozoic tectonic development of the intramontane Alai Valley,(Pamir-Tien Shan region,central Asia): An example of intracontinental deformation due to the Indo-Eurasia collision ［J］.Tectonics.21.doi: 10.1029/2002TC001358.
Cowgill E.2001.Tectonic evolution of the Altyn Tagh-Western Kunlun Fault System,Northwestern China .Ph D thesis.University of California,Los Angeles.311p.
Cowgill E.2010.Cenozoic right-slip faulting along the eastern margin of the Pamir salient,northwestern China ［J］.Geol Soc Am Bull,122: 145-161. doi: 10.1130/B26520.1.
Cowgill E,Yin A,Harrison T M,et al.2003.Reconstruction of the Altyn Tagh Fault based on U-Pb geochronology: Role of back thrusts,mantle sutures,and heterogeneous crustal strength in forming the Tibetan Plateau ［J］.Journal of Geophysical Research,108(B7): 2346.doi: 10.1029/2002JB002080.
Ding G,Chen J,Tian Q,et al.2004.Active faults and magnitudes of left-lateral displacement along the northern margin of the Tibetan Plateau ［J］: Tectonophysics,380: 243-260.doi: 10.1016/j.tecto.2003.09.022.
Ducea M N,Lutkov V,Minaev V T,et al.2003.Building the Pamirs: The view from the underside ［J］.Geology,31(10): 849-852.doi: 10.1130/G19707.1.
Fan G,Ni J F,Wallace T C.1994.Active tectonics of the Pamirs and Karakoram ［J］.J Geophys Res,99: 7l3-7160.
Fu B,Ninomiya Y,Guo J.2010.Slip partitioning in the northeast Pamir-Tian Shan convergence zone ［J］.Tectonophysics,483: 344-364.
Hamburger M W,Sarewitz D R,Pavlis T L,et al.1992.Structural and seismic evidence for intracontinental subduction in the Peter, the First Range Central Asia ［J］.Geol Soc Am Bull,104: 397-408.
Heermance R V,Chen J,Burbank D W,et al.2008.Temporal constraints and pulsed Late Cenozoic deformation during the structural disruption of the active Kashi foreland,northwest China ［J］.Tectonics,27:TC6012. doi: 10.1029/2007TC002226.
Jackson J,Molnar P,Patton H,et al.1979.Seismotectonic aspects of the Markansu Valley,Tajikstan,earthquake of August 11,1974 ［J］.J Geophys Res,84: 8157-9187.
Lin A,Kano Ken-ichi,Guo J,et al.2008.Late Quaternary activity and dextral strike-slip movement on the Karakax Fault Zone,northwest Tibet ［J］.Tectonophysics,453: 44-62.
Murphy M A,Yin A,Kapp P,et al.2000.Southward propagation of the Karakoram Fault system,southwest Tibet: Timing and magnitude of slip ［J］.Geology,28(5): 451-454.
Negredo A M,Replumaz A,Villaseor A,et al. 2007.Modeling the evolution of continental subduction processes in the Pamir-Hindu Kush region ［J］.Earth Planet Sci Lett,259: 212-225.
Pavlis T L,Hamburger M W,Pavlis G L.1997.Erosional processes as a control on the structural evolution of an actively deforming fold and thrust belt: An example from the Pamir-Tien Shan region,Central Asia ［J］.Tectonics,16: 810-822.
Peltzer G,Tapponnier P,Armijo R.1989.Magnitude of late Quaternary leftlateral displacement along the north edge of Tibet ［J］.Science,246: 1285-1289.
Phillips R J,Searle M P.2007.Macrostructural and microstructural architecture of the Karakoram Fault: Relationship between magmatism and strikes-slip faulting ［J］.Tectonics,26:TC3017.doi: 10.1029/2006TC001946.
Raterman N S,Cowgill E,Lin D.2007.Variable structural style along the Karakoram Fault explained using triple-junction analysis of intersecting faults ［J］.Geosphere,3: 71-85.doi: 10.1130/GES00067.1.
Ratschbacher L,Frisch W,Liu G,et al.1994.Distributed deformation in southern and western Tibet during and after the India-Asian collision ［J］.Journal of Geophysical Research,99(19): 917-945.doi: 10.1029/94JB00932.
Reigber C,Michel G W,Galas R,et al.2001.New space geodetic constraints on the distribution of deformation in Central Asia ［J］. Earth Planet Sci Lett,191: 157-165.doi: 10.1016/S0012-821X(01)00414-9.
Robinson A C,Yin A,Manning C E,et al.2004.Tectonic evolution of the northeastern Pamir: Constraints from the northern portion of the Cenozoic Kongur Shan extensional system,western China ［J］.Geological Society of America Bulletin,116: 953-973.
Robinson A C,Yin A,Manning C E,et al. 2007.Cenozoic evolution of the eastern Pamir: Implications for strain-accommodation mechanisms at the western end of the Himalayan-Tibetan orogen ［J］.Geological Society of America Bulletin,119: 882-896.
Robinson A C.2009a.Geologic offsets across the northern Karakorum Fault: Implications for its role and terrane correlations in the western Himalayan-Tibetan orogen ［J］.Earth Planet Sci Lett,279: 123-130.
Robinson A C.2009b.Evidence against Quaternary slip on the northern Karakorum Fault suggests kinematic reorganization at the western end of the Himalayan-Tibetan orogen ［J］. Earth and Planetary Science Letters,286(1-2): 158-170.
Robinson A C,Yin A,Lovera O M.2010.The role of footwall deformation and denudation in controlling cooling age patterns of detachment systems: An application to the Kongur Shan extensional system in the Eastern Pamir,China ［J］.Tectonophysics,496: 28-43.doi: 10.1016/j.tecto.1020.10.003.
Rumelhart P,Yin A,Cowgill E,et al.1999.Cenozoic vertical-axis rotation of the Altyn Tagh Fault system ［J］.Geology,27: 819-822.doi: 10.1130/0091-7613(1999)027<0819: CVAROT>2.3.CO; 2.
Ryerson F J,Finkel R,Meriaux A,et al.1997. Rapid slip on the Altyn Tagh Fault; Karakax Valley segment . In: Geological Society of America 1997. Abstracts with Programs.Salt Lake City,143.
Ryerson F J,Peltzer G,Tapponnier P,et al.1999 Active slip-rates on the Altyn Tagh Fault, Karakax valley segment: Constraints from surface exposure dating ［J］.Eos,Transactions,American Geophysical Union,80(46): F1008.
Schmalholz M.2004.The Amalgamation of the Pamirs and Their Subsequent Evolution in the Far Field of the India-Asia Collision ［M］.Univ of Tübingen,Tübingen,Germany.185pp.
Schwab M,Ratschbacher L,Siebel W,et al.2004.Assembly of the Pamirs: Age and origin of magmatic belts from the southern Tien Shan to the southern Pamirs and their relation to Tibet ［J］.Tectonics,23: TC4002. doi: 10.1029/2003TC001583.
Shen Z K,Wang M,Li Y,et al.2001.Crustal deformation along the Altyn Tagh Fault system,western China,from GPS ［J］.Journal of Geophysical Research,106(12): 30607-30621.
Sobel E R,Dumitru T A.1997.Exhumation of the margins of the western Tarim Basin during the Himalayan orogeny ［J］.J Geophys Res,102: 5043-5064.
Sobel E R,Chen J,Heermance R V.2006.Late Oligocene-early Miocene initiation of shortening in the southwestern Chinese Tian Shan: Implications for Neogene shortening rate variations ［J］.Earth Planet Sci Lett,247: 70-81.
Sobel E R,Schoenbohm L,Chen J,et al.2011. Late Miocene-Pliocene deceleration of dextral slip between Pamir and Tarim: Implications for Pamir orogenesis ［J］.Earth and Planetary Science Letters,304: 369-378.
Strecker M R,Frisch W,Hamburger M W,et al. 1995.Quaternary deformation in the eastern Pamirs,Tadzhikistan and Kyrgyzstan ［J］.Tectonics,14: 1061-1079.
Tapponnier P,Mattauer M,Proust F,et al.1981.Mesozoic ophiolites,sutures,and large-scale tectonic movements in Afghanistan ［J］. Earth Planet Sci Lett,52: 355-371.
Tapponnier P,Molnar P.1977.Active faulting and tectonics in China ［J］.J Geophys Res,82: 2905-2930.
Thomas J C,Chauvin A,Gapais D,et al.1994.Paleomagnetic evidence for Cenozoic block rotations in the Tadjik depression(Central Asia)［J］.Journal of Geophysical Research,99(15): 141-15,160.doi: 10.1029/94JB00901.
Thomas J C,Cobbold P R,Wright A,et al.1996.Cenozoic tectonics of the Tadzhik depression,Central Asia .In Yin A and Harrison T M eds.The Tectonic Evolution of Asia. New York,Cambridge University Press.191-207.
Valli F,Leloup P,Paquette J L,et al.2008.New U/Pb constraints on timing of shearing and long-term slip-rate on the Karakorum Fault ［J］.Tectonics,27.doi: 10.1029/2007TC002184.
Waldhör M,Appel E,Frisch W,et al.2001.Palaeomagnetic investigation in the Pamirs and its tectonic implications ［J］.Journal of Asian Earth Sciences,19: 429-451.doi: 10.1016/S1367-9120(00)00030-4.
Windley B F,Allen M B,Zhang C,et al.1990.Paleozoic accretion and Cenozoic redeformation of the Chinese Tien Shan Range,central Asia ［J］.Geology,18: 128-131.
Yang S,Li J,Wang Q.2008.The deformation pattern and fault rate in the Tianshan Mountains inferred from GPS observation ［J］.Science in China Series D,51: 1064-1080.
Yin A,Yang Z,Butler R,Otofuji Y I,et al.2000.Correction: Cenozoic vertical axis rotation of the Altyn Tagh Fault system ［J］.Geology,28: 480.doi: 10.1130/0091-7613(2000)28<480: CVROTA>2.0.CO; 2.
Yin A,Robinson A,Manning C E.2001.Oroclinal bending and slab break-off causing coeval east-west extension and east-west contraction in the Pamir-Nanga Parbat syntaxis in the past 10My. ［J］. Eos(Transactions,American Geophysical Union),82(47): F1124.
Yin A,Rumelhart P E,Butler R,et al.2002.Tectonic history of the Altyn Tagh Fault system in northern Tibet inferred from Cenozoic sedimentation ［J］.Geological Society of America Bulletin,114: 1257-1295.doi: 10.1130/0016-7606(2002)114<1257: THOTAT>2.0.CO; 2.
Zubovich A V,Wang X Q,Scherba Y G,et al.2010.GPS velocity field of the Tien Shan and surrouding region ［J］.Tectonics,29: TC6014.doi: 10.1029/2010TC002772.

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