引文
1 Molnar P,Tapponn ier P.Cenozoic tecton ics of Asia:E ffects of acontinental collision.Science,1975,189:419~426
2 M eyer B,Tapponn ier P,Bourjot Let a.l C rustal th icken ing inGansu-Q inghai,lithospheric mantle subduction,and ob lique,strike-slip controlled growth of the Tibetan P lateau.GeophysicalJournal Internationa,l 1998,135:1~47
3 Tapponn ier P,Xu Z Q,Roger Fet a.l Ob lique stepw ise rise andgrowth of the Tibet P lateau.Science,2001,294:1671~1677
4 Molnar P,Burchfiel B C,L iang Ket al.Geomorph ic evidence foractive fau lting in the A ltyn Tagh and Northern Tibet and qualitativeestimates of its contribution to the convergence of Ind ia and Eurasia.Geology,1987,15:249~253
5 Avouac J P,Tapponn ier P.K inematic model of active deformationin CentralAsia.Geophysical Research Letters,1993,20:895~898
6 Y in A,Rum elhart P E,ButlerRet a.l Tecton ic h istory of the A ltynTagh fau lt system in Northern Tibet inferred from Cenozoicsed im entation.Geological Society ofAm erica Bulletin,2002,114:1257~1295
7张志德,李嵩龄,杨德朴.康西瓦断裂的地质特征及形成和发展.新疆地质,1987,5(3):52~59Zhang Zh ide,L i Songling,Yang D epu.The geologic characteristicsof Kangxiwar fau lt and its formation and developm ent.XinjiangGeology,1987,5(3):52~59
8国家地震局编.阿尔金活动断裂带.地震出版社,1992.1~319Ch ina Seismological Bureau ed.The A ltun Active Fau lt Zone.Beijing:Seismological Press,1992.1~319
9 Sobel E R,Arnaud N.A possib le M idd le Paleozoic suture in theA ltyn Tagh,NW Ch ina.Tectonics,1999,18:64~74
10 W ittlinger G,Vergne J,Tapponn ier Pet al.Teleseim ic imaging ofsubducting lithosphere and Moho offsets beneath W estern Tibet.Earth and Planetary Science Letters,2004,221(1~4):117~130
11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):316~321YangW anzh i,Zhang W eizhou,Qu Xun.Geochem ical evidence ofthe relation between the Kuyake fau lt of east part of west Kun lunMountains and the Kangxiwar and A ltyn Tagh fau lts.GeologicalBulletin ofChina,2005,24(4):316~321
12 Peltzer G,Tapponn ier P,Arm ijo R.Magn itude of Late Quaternaryleft-lateral d isplacem ent along the north edge of Tibet.Science,1989,246:1285~1289
13 W right T J,Parsons B,England P Cet a.l InSAR observations oflow slip rates on the major fau lts ofW estern Tibet.Science,2004,305:236~239
14 Burtman V S,Molnar P.Geological and geophysical evidence fordeep subduction of continental crust beneath the Pam ir.GeologicalSociety ofAm erica Special Paper,1993,281:76
15崔军文,唐哲民,邓晋福等著.阿尔金断裂系.地质出版社,1999.1~249Cu i Junwen,Tang Zem in,D eng Jinfuet a.l A ltun Fau lt System.Beijing:Geological Pub lish ing House,1999.1~249
16 M eng Q R,Hu J M,Yang F Z.Tim ing and magn itude ofd isplacem ent on the A ltyn Tagh fau lt:Constraints from stratigraph iccorrelation of ad join ing Tarim and Qaidam basins,NW Ch ina.TerraNova,2001,13:86~91
17 Yue Y,L iou J G.A tow-stage evolution model for the A ltyn Taghfau lt,Ch ina.Geology,1999,27:227~230
18 Yue Y,R itts B D,G raham A S Aet a.l In itiation and long-termslip h istory of the A ltyn Tagh fau lt.International Geology Review,2001,43:1087~1093
19 Sun Jim in,Zhu R ixiang,An Zh isheng.Tecton ic uplift in thenorthern Tibetan P lateau since 13.7Ma ago inferred from molassedeposits along the A ltyn Tagh fau lt.Earth and Planetary ScienceLetters,2005,235(3~4):641~653
20 Yue Y J,R itts B D,G raham S Aet a.l Slow ing extrusion tecton ics:Lowered estimate of post-EarlyM iocene slip rate for the A ltyn Taghfau lt.Earth and Planetary Science Letter,s 2003,217(1~2):111~122
21 W ang Erch ie.D isplacem ent and tim ing along the northern strand ofthe A ltyn Tagh fau lt zone,Northern Tibet.Earth and PlanetaryScience Letters,1997,150(1~2):55~64
22 Zheng J.S ign ificance of the A ltun Tagh fau lt of Ch ina.Episodes,1991,14:307~312
23丁国瑜.阿尔金活断层的古地震与分段.第四纪研究,1995,(2):97~106D ing Guoyu.Paleoearthquakes along the A ltun active fau lt and itssegm entation.Quaternary Sciences,1995,(2):97~106
24王萍,卢演俦,丁国瑜等.甘肃疏勒河冲积扇发育特征及其对构造活动的影响.第四纪研究,2004,24(1):74~81W ang P ing,Lu Yanchou,D ing Guoyuet a.l Shu lehe alluvial fan:Characteristics of its developm ent and its response to tecton icactivity.Quaternary Sciences,2004,24(1):74~81
25王萍,王增光,雷生学等.阿尔金断裂东端破裂生长点的最新构造变形.第四纪研究,2006,26(1):108~116W ang P ing,W ang Zengguang,Lei Shengxueet al.The latesttecton ic deformation at the grow ing point of a new fracture on theeastern tip of the A ltyn Tagh Fau lt.Quaternary Science,s 2006,26(1):108~116
26 W ashburn Z,Arrowsm ith J R,Forman S Let a.l Late Holoceneearthquake h istory of the central A ltyn Tagh fau lt,Ch ina.Geology,2001,29:1051~1054
27 Bend ick R,B ilham R,Freymueller Jet a.l Geodetic evidence for alow slip rate in the A ltyn Tagh fau lt system.Nature,2000,404:69~72
28 W allace K,Y in G,B ilham R.Inescapab le slow slip on the A ltynTagh fau lt.Geophysical Research Letter,s 2004,31:L09613,doi:10.1029/2004GL019724
29 M eriaux A S,Ryerson F J,Tapponn ier Pet a.l Rap id slip along thecentralA ltyn Tagh fau lt:Morphochronologic evidence from CherchenHe and Su lamu Tagh.Journal ofGeophysicalResearch,2004,109:B06401,doi:10.1029/2003 JB002558
30 Fu B,L in A.Spatial d istribution of the surface rupture zoneassociated w ith the 2001Ms8.1 Central Kun lun earthquake,Northern Tibet,revealed by satellite remote sensing data.International Journal ofRem ote Sensing,2003,24:2191~2198
31 Gaudem er Y,Tapponn ier P,Turcotte D.R iver offsets across activestrike-slip fau lts.Annales Tectonicae,1989,3:55~76
32 D ing G Y,Chen J,Tian Q Jet al.Active fau lts and magn itudes ofleft-lateral d isplacem ent along the northern margin of the TibetanPlateau.Tectonophysics,2004,380(3~4):243~260
33 Clark D H,Gillespie A R,Keck W Met al.Glacial asynchrony inthe Kunlun Shan,Northwestern Tibet.Geological SocietyofAmericaAbstracts with Programs,2001,32(7):A-441
34 Zhang P,Sheng Z,Wang Met al.Continuous deformation of theTibetan Plateau fromglobal positioning systemdata.Geology,2004,32:809~812
35 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,andclimatic origin of the regional morphology.Geophysical JournalInternational,2002,148:356~388
36 Fu B,Awata Y,Du Jet al.Late Quaternary systematic streamoffsets caused by repeated large seismic events along the Kunlunfault,Northern Tibet.Geomorphology,2005,71(3~4):278~292
37 Stein R S,King G C P,Rundle J B.The growth of geologicalstructures by repeated earthquakes:2.Field examples of continentaldip-slip faults.Journal ofGeophysical Research,1988,93:13319~13331
38 Bilham R,King G C P.The morphology of strike-slip faults:Examples from the San Andreas Fault,California.Journal ofGeophysical Research,1989,94:10204~10216
39 Sylvester A G.Strike-slip faults.Geological Society of AmericaBulletin,1988,100:1666~1703
40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 ofQinghai-Xizang Plateau.Quaternary Sciences,2003,23(6):629~639
41任金卫,王敏.GPS观测的2001年昆仑山口西Ms8.1级地震地壳变形.第四纪研究,2005,25(1):34~44Ren Jinwei,Wang Min.GPS measured crustal deformation of theMs8.1 Kunlun earthquake on November 14th 2001 in Qinghai-Xizang Plateau.Quaternary Sciences,2005,25(1):34~44
42 Fu B,Awata Y,Du Jet al.Complex geometry and segmentation ofthe surface rupture associated with the 14 November 2001 greatKunlun earthquake,Northern Tibet,China.Tectonophysics,2005,407:43~63
43 Xu X,Chen W,Ma Wet al.Surface rupture of the Kunlunshanearthquake(Ms8.1),Northern Tibetan Plateau,China.Seismological Research Letters,2002,73:884~892
44 Wells D L,Coopersmith K J.New empirical relationships amongmagnitude,rupture length,rupture width,rupture area,and surfacedisplacement.Bulletin of the Seismological Society of America,1994,84:974~1002
45 Cowgill E,Arrowsmith J R,Yin Aet al.The Akato Tagh bendalong the Altyn Tagh Fault,Northwest Tibet 1:Smoothing byvertical-axis rotation and the effect of topographic stresses on bend-flanking faults.Geological Society ofAmerica Bulletin,2004,116:1423~1442