引文
1 Tapponnier P,Xu Z Q,Roger Fet al.Oblique stepwise rise andgrowth of the Tibet Plateau.Science,2001,294:1671~1677
2 Yin A,Rumelhart P E,Butler Ret al.Tectonic history of the AltynTagh fault system in Northern Tibet inferred from Cenozoicsedimentation.Geological Society of America Bulletin,2002,114(10):1257~1295
3 Avouac J P,Tapponnier P.Kinematic model of active deformation inCentral Asia.Geophysical Research Letters,1993,20(10):895~898
4 Molnar P,Tapponnier P.Cenozoic tectonics of Asia:Effects of acontinental collision.Science,1975,189:419~426
5 Tapponnier P,Molnar P.Active faulting and tectonics of China.Journal ofGeophysical Research,1977,82:2905~2930
6 Tapponnier P,Molnar P.Active faulting and Cenozoic tectonics ofthe Tien Shan,Mongolia,and Baikal regions.Journal ofGeophysicalResearch,1979,84:3425~3459
7 Meyer B,Tapponnier P,Bourjot Let al.Crustal thickening inGansu-Qinghai,lithospheric mantle subduction,and oblique,strike-slip controlled growth of the Tibet Plateau.Geophysical JournalInternational,1998,135(1):1~47
8 Burchfiel B C,Deng Q,Molnar Pet al.Intracrustal detachmentwithin zones of continental deformation.Geology,1989,17(8):748~752
9 Molnar P,Burchfiel B C,Liang K uangyiet al.Geomorphic evidencefor active faulting in the Altyn Tagh and Northern Tibet andqualitative estimates of its contribution to the convergence of Indiaand Eurasia.Geology,1987,15(3):249~253
10 Peltzer G,Tapponnier P,Armijo R.Magnitude of Late Quaternaryleft-lateral displacement along the north edge of Tibet.Science,1989,246:1285~1289
11国家地震局《阿尔金活动断裂带》课题组编.阿尔金活动断裂带.北京:地震出版社,1992.1~319Research Team“The Altun Active Fault Zone”of ChinaSeismological Bureau ed.The Altun Active Fault Zone.Beijing:Seismological Press,1992.1~319
12 Van der Woerd J,Xu Xiwei,Li Haibinget al.Rapid active thrustingalong the northwestern range front of the Tanghe Nan Shan(WesternGansu,China).Journal ofGeophysical Research,2001,106(B12):30475~30504
13李海兵,杨经绥,许志琴等.阿尔金断裂带印支期走滑活动的地质及年代学证据.科学通报,2001,46(16):1333~1338Li Haibing,Yang Jingsui,Xu Zhiqinet al.Geological andchronological evidence of Indo-Chinese strike-slip movement in theAltyn Tagh fault zone.Chinese Science Bulletin,2001,46(16):1333~1338
14 Mriaux A S,Ryerson F J,Tapponnier Pet al.Rapid slip along thecentral Altyn Tagh fault:Morphochronologic evidence fromCherchenHe and Sulamu Tagh.Journal ofGeophysical Research,2004,109(B6):B06401,doi:10.1029/2003JB002558
15 Mriaux A S,Tapponnier P,Ryerson F Jet al.The Aksay segmentof the northern Altyn Tagh fault:Tectonic geomorphology,landscapeevolution,and Holocene slip rate.Journal ofGeophysical Research,2005,110:B04404,doi:04410,01029/02004JB003210
16徐锡伟,Tapponnier P,Van der Woerd J等.阿尔金断裂带晚第四纪左旋走滑速率及其构造运动转换模式讨论.中国科学(D辑),2003,33(10):967~974Xu Xiwei,Tapponnier P,Van der Woerd Jet al.Late Quaternarysinistral slip rate along the Altyn Tagh fault and its structuraltransformation model.Science in China(Series D),2005,48(3):384~397
17王峰,徐锡伟,郑荣章等.阿尔金断裂带西段车尔臣河以西晚第四纪以来的滑动速率研究.地震地质,2004,26(2):200~208Wang Feng,Xu Xiwei,Zheng Rongzhanget al.Late Quaternary slip-rate on the Altyn fault west to the Qarqan River.Seismology andGeology,2004,26(2):200~208
18王峰,徐锡伟,郑荣章.用阶地测量方法探讨阿尔金断裂中段全新世滑动速率.地震地质,2004,26(1):61~70Wang Feng,Xu Xiwei,Zheng Rongzhang.Study on Holocene strike-slip rates of the middle Altyn Tagh fault by terraces offsetmeasurement.Seismology and Geology,2004,26(1):61~70
19 Cowgill E.Impact of riser reconstructions on estimation of secularvariation in rates of strike-slip faulting:Revisiting the CherchenRiver site along the Altyn Tagh fault,NW China.Earth andPlanetary Science Letters,2007,254(3~4):239~255
20 Zhang Peizhen,Molnar P,Xu Xiwei.Late Quaternary and present-day rates of slip along the Altyn Tagh fault,northern margin of theTibetan Plateau.Tectonics,2007,26(5):TC5010,doi:10.1029/2006TC002014
21付碧宏,张松林,谢小平等.阿尔金断裂系西段———康西瓦断裂的晚第四纪构造地貌特征研究.第四纪研究,2006,26(2):228~235Fu Bihong,Zhang Songlin,Xie Xiaopinget al.Late Quaternarytectono-geomorphic features along the Kangxiwar fault,Altyn Taghfault system,Northern Tibet.Quaternary Sciences,2006,26(2):228~235
22 Ding G Y,Chen J,Tian Q Jet al.Active faults and magnitudes ofleft-lateral displacement along the northern margin of the TibetanPlateau.Tectonophysics,2004,380(3~4):243~260
23 Gaudemer Y,Tapponnier P,Turcotte D.River offsets across activestrike-slip faults.Annales Tectonicae,1989,3(2):55~76
24新疆维吾尔自治区地震局.新疆维吾尔自治区地震构造图(1∶200万).成都:成都地图出版社,1997Xinjiang Uygur Autonomous Region Seismological Bureau.Insturc-tion of Xinjiang Uygur Autonomous Region Seismotectonic Map(1∶2000000).Chengdu:Chengdu Map Publishing House,1997
25冯先岳.新疆古地震.乌鲁木齐:新疆科技卫生出版社,1997.1~250Feng Xianyue.Palaeo-earthquakes of Xinjiang.r櫣mqi:Science,Technology and Health Publishing House,1997.1~250
26李海兵,杨经绥,史仁灯等.阿尔金走滑断陷盆地的确定及其与山脉的关系.科学通报,2002,47(1):63~67Li Haibing,Yang Jingsui,Shi Rendenget al.Determination of theAltyn Tagh strike-slip fault basin and its relationship withmountains.Chinese Science Bulletin,2002,47(7):572~577
27 Li Haibing,Yang Jingsui,Wu Cailaiet al.Evidence for Triassicsinistral shear along the Altyn Tagh fault,Northern Tibet(China).EOS,2005,86(47):Abstract
28 Wang Yu,Zhang Xuemin,Wang Erchieet al.40Ar/39Ar thermo-chronological evidence for formation and Mesozoic evolution of thenorthern-central segment of the Altyn Tagh fault system in thenorthern Tibetan Plateau.Geological Society of America Bulletin,2005,117:1336~1346
29 Arnaud N,Delville N,Montel J Met al.Paleozoic to Cenozoicdeformation along the Altyn Tagh fault in the Altyn Shan massifarea,Eastern Qilian Shan,NE Tibet,China.American GeophysicalUnion Annual Meeting Abstracts,1999,F1018
30 Arnaud N,Tapponnier P,Francoise Ret al.Evidence for Mesozoicshear along the western Kunlun and Altyn-Tagh fault,Northern Tibet(China).Journal ofGeophysical Research,2003,108(B1):ETG12-1~12-27
31 Liu Yongjiang,Genser J,Ge Xiaohonget al.40Ar/39Ar age evidencefor Altyn fault tectonic activities in Western China.Chinese ScienceBulletin,2003,48(18):2024~2030
32 Liu Yongjiang,Ye Huiwen,Ge Xiaohonget al.Laser probe40Ar/39Ardating of mica on the deformed rocks fromAltyn fault and its tectonicimplications,Western China.Chinese Science Bulletin,2001,46(4):322~325
33 Li Haibing,Yang Jingsui,Zeng Lingsenet al.Evidence forCretaceous uplift of the northern Tibetan Plateau.EOS,2004,85(47):Fall Meet.Suppl.,Abstract
34李海兵,杨经绥,许志琴等.阿尔金断裂带对青藏高原北部生长、隆升的制约.地学前缘,2006,13(4):59~79Li Haibing,Yang Jingsui,Xu Ziqinet al.The constraint of the AltynTagh fault system to the growth and rise of the northern TibetanPlateau.Earth Science Frontiers,2006,13(4):59~79
35 Wittlinger G,Tapponnier P,Poupinet Get al.Tomographic evidencefor localized lithospheric shear along the Altyn Tagh fault.Science,1998,282:74~76
36 Wittlinger G,Vergne J,Tapponnier Pet al.Teleseismic imaging ofsubducting lithosphere and Moho offsets beneath Western Tibet.Earth and Planetary Science Letters,2004,221(1~4):117~130
37 Yang Jingsui,Meng Fancong,Zhang Jianxinet al.The shoshoniticvolcanic rocks at Hongliuxia:Pulses of the Altyn Tagh fault inCretaceous?Science in China(Series D),2001,31(Suppl.1):94~102
38邓万明著.青藏高原北部新生代板内火山岩.北京:地质出版社,1998.180Deng Wanming.Cenozoic Intraplate Volcanic Rocks in the NorthernQinghai-Xizang Plateau.Beijing:Geological Publishing House,1998.180
39邓万明.中国西部新生代火山活动及其大地构造背景———青藏及邻区火山岩的形成机制.地学前缘,2003,10(2):471~478Deng Wanming.Cenozoic volcanic activity and its geotectonicbackground in West China———Formative excitation mechanism ofvolcanic rocks in Qinghai-Xizang and adjacent districts.EarthScience Frontiers,2003,10(2):471~478
40 Yin A,Rumelhart P E,Butler Ret al.Tectonic history of the AltynTagh fault system in Northern Tibet inferred from Cenozoicsedimentation.Geological Society of America Bulletin,2002,114(10):1257~1295
41 Ryerson F J,Peltzer G,Tapponnier Pet al.Active slip-rates on theAltyn Tagh fault Karakax valley segment:Constraints from surfaceexposure dating.EOS,1999,80(47):1008
42 Wright TJ,Parsons B,England P Cet al.InSAR observations of lowslip rates on the major faults of Western Tibet.Science,2004,305:236~239
43潘桂棠,焦淑沛,徐耀荣等.阿尔金山新生代构造及造山性质.见:地质矿产部青藏高原地质文集编委会编.青藏高原地质论文集(15).北京:地质出版社,1984.113~119Pan Guitang,Jiao Shupei,Xu Yaoronget al.The Cenozoic tectonicsand its orogeny in Altun.In:Editorial Committee of“Contributionto the Geology of the Qinghai-Xizang(Tibet)Plateau”,Ministry ofGeology and Mineral Resources ed.Contribution to the Geology ofthe Qinghai-Xizang(Tibet)Plateau(15).Beijing:GeologicalPublishing House,1984.113~119
44杨万志,张维洲,屈迅.西昆仑山东段库牙克断裂与康西瓦断裂、阿尔金断裂关系的地球化学证据.地质通报,2005,24(4):316~321Yang Wanzhi,Zhang Weizhou,Qu Xun.Geochemical evidence ofthe relation between the Kuyake fault of east part of west KunlunMountains and the Kangxiwar and Altyn Tagh faults.GeologicalBulletin ofChina,2005,24(4):316~321
45 Burtman V S,Molnar P.Geological and Geophysical Evidence forDeep Subduction of Continental Crust Beneath the Pamir.BoulderColo:Geological Society of America,1993.76
46车自成,孙勇.阿尔金麻粒岩相杂岩的时代及塔里木盆地的基底.中国区域地质,1996,(1):51~57Che Zicheng,Sun Yong.The age of the Altun granulite faciescomplex and the basement of the Tarim Basin.Regional Geology ofChina,1996,(1):51~57
47车自成,刘良,刘洪福等.阿尔金断裂的组成及相关中新生代含油气盆地的成因特征.中国区域地质,1998,17(4):377~384Che Zicheng,Liu Liang,Liu Hongfuet al.The constituents of theAltun fault system and genetic characteristics of related Meso-cenozoic petroleum bearing basin.Regional Geology of China,1998,17(4):377~384
48许志琴,杨经绥,张建新等.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制.地质学报,1999,73(3):193~205Xu Zhiqin,Yang Jingsui,Zhang Jianxinet al.Acomparison betweenthe tectonic units on the two sides of the Altun sinistral strike-slipfault and the mechanism of lithospheric shearing.Acta GeologicaSinica,1999,73(3):193~205
49 Yue Yongjun,Liou J G.Two-stage evolution model for the AltynTagh fault,China.Geology,1999,27(3):227~230
50 Yue Y,Ritts B D,Graham A S Aet al.Initiation and long-term sliphistory of the Altyn Tagh fault.International Geology Review,2001,43(12):1087~1093
51葛肖虹,刘俊来.北祁连造山带的形成与背景.地学前缘,1999,6(4):223~230Ge Xiaohong,Liu Junlai.Formation and tectonic background of thenorthern Qilian orogenic belt.Earth Science Frontiers,1999,6(4):223~230
52 Ritts B D,Biffi U.Magnitude of post-middle Jurassic(Bajocian)displacement on the central Altyn Tagh fault system,Northwest China.Geological SocietyofAmerica Bulletin,2000,112(1):61~74
53 Zhang JⅩ,Zhang Z M,Xu Z Qet al.Petrology and geochronologyof eclogites fromthe western segment of the Altyn Tagh,NorthwesternChina.Lithos,2001,56(2~3):189~208
54 Meng Q R,Hu J M,Yang F Z.Timing and magnitude ofdisplacement on the Altyn Tagh fault:Constraints from stratigraphiccorrelation of adjoining Tarimand QaidamBasins,NWChina.TerraNova,2001,13:86~91
55李海兵,许志琴,杨经绥等.阿尔金断裂带最大累积走滑位移量———900km?地质通报,2007,26(10):1288~1298Li Haibing,Xu Zhiqin,Yang Jingsuiet al.The maximal cumulativestrike-slip displacement of the Altyn Tagh fault—900km(?).Geological Bulletin ofChina,2007,26(10):1288~1298
56 Meyer B,Tapponnier P,Gaudemer Yet al.Rate of left-lateralmovement along the easternmost segment of the Altyn Tagh Fault,east of 96°E(China).Geophysical Journal International,1996,124(1):29~44
57李海兵.阿尔金断裂带对青藏高原北部隆升的贡献.北京:中国地质科学院博士论文,2001.1~161Li Haibing.Formation Era of Altyn Tagh Fault Zone andContribution of its Strike-Slip to the Uplift of North Tibetan Plateau.PhD Thesis,Institute of Geology,Chinese Academy of GeologicalSciences,Beijing,2001.1~161
58 Meriaux A S.Dtermination par datation cosmoge′nique desvariations de la vitesse de glissement sur la faille de l Atlyn Taghdepuis 100ka.Ph.D.Thesis,University ParisⅦ,Paris,2002
59 Wang Q,Zhang P,Freymueller J Tet al.Present-day crustaldeformation in China constrained by global positioning systemmeasurements.Science,2001,294:574~577
60 Chen Zhenle,Zhang Yueqiao,Chen Xuanhuaet al.Late Cenozoicsedimentary process and its response to the slip history of the centralAltyn Tagh fault,NW China.Science in China(Series D),2001,44:103~111
61向宏发,虢顺民,张晚霞等.阿尔金断裂带东段第四纪以来的水系位错与滑动速率.地震地质,2000,22(2):129~138Xiang Hongfa,Guo Shunmin,Zhang Wanxiaet al.River offset andslip rate of the east segment of Altyn Tagh fault zone sinceQuaternary.Seismology and Geology,2000,22(2):129~138
62张培震,王琪,马宗晋.青藏高原现今构造变形特征与GPS速度场.地学前缘,2002,9(2):442~450Zhang Peizhen,Wang Qi,Ma Zongjin.GPS velocity field and activecrustal deformation in and around the Qinghai-Tibet Plateau.EarthScience Frontiers,2002,9(2):442~450
63 Shen Z K,Wang M,Li Yet al.Crustal deformation along the AltynTagh fault system,Western China,fromGPS.Journal ofGeophysicalResearch,2001,106(B12):30607~30621
64 Bendick R,Bilham R,Freymueller Jet al.Geodetic evidence for alow slip rate in the Altyn Tagh fault system.Nature,2000,404:69~72
65崔军文,张晓卫,李朋武.阿尔金断裂:几何学、性质和生长方式.地球学报,2002,23(6):509~516Cui Junwen,Zhang Xiaowei,Li Penwu.The Altun fault:Itsgeometry,nature and mode of growth.Acta Geoscientia Sinica,2002,23(6):509~516
66 Van der Woerd J,Tapponnier P,Ryerson F Jet al.Uniformpostglacial slip-rate along the central 600km of the Kunlun fault(Tibet),from26Al,10Be and14C dating of riser offsets,and climaticorigin of the regional morphology.Geophysical Journal International,2002,148(3):356~388
67 Wells D L,Coppersmith K J.New empirical relationships amongmagnitude,rupture length,rupture width,rupture area,and surfacedisplacement.Bulletin ofthe Seismological SocietyofAmerica,1994,84(4):974~1002
68 Xu Xiwei,Chen Wenbin,Ma Wentaoet al.Surface rupture of theKunlunshan earthquake(MS8.1),Northern Tibetan Plateau,China.Seismological Research Letters,2002,73:884~892
69陈杰,陈宇坤,丁国瑜等.2001年昆仑山口西8.1级地震地表破裂带.第四纪研究,2003,23(6):629~639Chen Jie,Chen Yukun,Ding Guoyuet al.Surface rupture zones ofthe 2001 earthquakeMS8.1 west of Kunlun pass,Northern Qinghai-Xizang Plateau.Quaternary Sciences,2003,23(6):629~639
70丁国瑜.阿尔金活断层的古地震与分段.第四纪研究,1995,(2):97~106Ding Guoyu.Paleoearthquakes along the Altun active fault and itssegmentation.Quaternary Sciences,1995,(2):97~106
71 Washburn Z,Arrowsmith J R,Forman S Let al.Late Holoceneearthquake history of the central Altyn Tagh fault,China.Geology,2001,29(11):1051~1054