阿尔金断裂南侧弧形地貌单元成因及其构造意义
|
摘要
巨型左旋走滑的阿尔金断裂是青藏高原的北部边界,在印度-欧亚板块碰撞过程中起重要的调节作用,控制着青藏高原东北部的构造演化,认识其活动演化对理解青藏高原的构造变形过程和机制具有重要意义。阿尔金断裂南侧存在一系列弧形地貌单元,知晓这些弧形带是原始弧形弯曲还是后期由于阿尔金断裂左旋走滑拖曳而形成的,对认识阿尔金断裂的构造演化具有重要意义。文中在前期阿尔金断裂南侧柴西英雄岭和柴北缘2条弧形带不同部位已开展的精细古地磁旋转变形研究的基础上,综合研究区和阿尔金断裂附近已有的古地磁旋转变形研究结果和弧形带几何形态学等其它地质证据,分析发现这2条弧形带的几何学特征是由其不同部位发生旋转变形所导致的,且旋转变形与该时段阿尔金断裂的快速左旋走滑活动密切相关。通过上述工作,更加全面地了解了阿尔金断裂新生代2阶段的走滑特征,进一步限定了阿尔金断裂早渐新世以来左旋滑移量,以柴西段为参照系滑移量至少约350～430km,以柴北缘段为参照系至少约380～460km,平均滑移速率至少约10. 6～13. 9mm/a。
The giant sinistral Altyn Tagh Fault(ATF) is the northern boundary of the Tibetan Plateau. It has been playing important role in adjusting the India-Eurasia collision and the tectonic evolution of the northeastern Tibetan Plateau. Knowledge of the evolution of the ATF can provide comprehensive understanding of the processes and mechanisms of the deformation of the Tibetan Plateau. However,its timing of commencement,amount of displacement and strike-slip rate,as well as the tectonic evolution of the region are still under debate. South of the ATF,there exist a series of oroclinal-like arcuate structures. Knowledge of whether these curved geometries represent original curvatures or the bending of originally straight/aligned geological units has significant tectonic implications for the evolution of the ATF. The Yingxiongling arcuate belt in the western Qaidam Basin and the northern Qaidam marginal thrust belt(NQMTB) north of the Qaidam Basin are the two typical arcuate thrust belts,where the former has a "7-types"structure,and the latter has a reverse "S-type"structure.Successive Cenozoic sediments are well exposed and magnetostratigraphically dated in both belts.Paleomagnetic declination has great advantage to reveal vertical-axis rotations of geological bodies since they become magnetized. Recently conducted paleomagnetic rotation studies in different parts of these two thrust belts revealed detailed Cenozoic rotation patterns and magnitudes of the region. By integrating these paleomagnetic rotation results with regional geometric features and lines of geological evidence,we propose that these two arcuate thrust belts were most likely caused by different rotations in different parts of these curvatures,due to the sinistral strike-slip faulting along the ATF,rather than originally curved ones. The Yingxiongling arcuate belt was shaped by the significant counterclockwise(CCW) rotations of its northwestern half(the Akatengnengshan anticline) near the ATF during ～ 16 ～ 11 Ma BP,while its southeastern half(the Youshashan anticline) had no significant rotations since at least ～ 20 Ma BP. The geometry of the NQMTB was developed firstly by remarkable clockwise rotations of its middle part during ～ 33 ～ 14 Ma BP,and later possibly CCW rotations of its northwestern part during the Middle to Late Miocene,similar to that of the northwestern part of the Yingxiongling arcuate belt. The characteristics of two-stage strike-slip evolution of the ATF since the Early Oligocene were enriched: 1) During the Early Oligocene to mid-Miocene,fast strike-slip faulting along the ATF was proposed to accommodate the eastward extrusion of the northern Tibetan Plateau with its sinistral shear confined to the fault itself. While in the NQMTB and farther east area in the Qilian Shan, its sinistral shear was transferred to the interior of the plateau and was accommodated by deformation of differential crustal shortenings and block rotations in these regions.Thus,the displacement along the ATF west of the NQMTB is larger than that east of the NQMTB. 2)Since the mid-late Miocene,sinistral shear of the ATF was widespread distributed within the northern Tibetan Plateau,instead of concentrated to the fault itself. Its sinistral offsets were partially absorbed by the shortening deformation within the Qaidam Basin and the Qilian Shan,leading the offsets along the ATF decreasing to the east. With the sinistral frictional drag of blocks(the Tarim Basin and the Altyn Tagh Range) on the other side during the second stage evolution of the ATF,a transitional zone south of the ATF was likely developed by remarkable CCW rotations during the Middle to Late Miocene,which is probably confined to east of the Tula syncline. Combining the sinistral offsets along the ATF derived from the paleomagnetic rotations during the Early Oligocene to mid-late Miocene and that by piercing points since the Late Miocene,the post Oligocene strike-slip offsets were constrained as at least ～ 350 ～ 430 km for the reference in the western Qaidam Basin and ～ 380 ～ 460 km for the reference in the NQMTB,with an average slip rate of at least ～ 10. 6 ～ 13. 9 mm/a. The post Early Oligocene offsets are consistent with the widely accepted offsets of ～ 300 ～ 500 km obtained by piercing point analyses.
The giant sinistral Altyn Tagh Fault(ATF) is the northern boundary of the Tibetan Plateau. It has been playing important role in adjusting the India-Eurasia collision and the tectonic evolution of the northeastern Tibetan Plateau. Knowledge of the evolution of the ATF can provide comprehensive understanding of the processes and mechanisms of the deformation of the Tibetan Plateau. However,its timing of commencement,amount of displacement and strike-slip rate,as well as the tectonic evolution of the region are still under debate. South of the ATF,there exist a series of oroclinal-like arcuate structures. Knowledge of whether these curved geometries represent original curvatures or the bending of originally straight/aligned geological units has significant tectonic implications for the evolution of the ATF. The Yingxiongling arcuate belt in the western Qaidam Basin and the northern Qaidam marginal thrust belt(NQMTB) north of the Qaidam Basin are the two typical arcuate thrust belts,where the former has a "7-types"structure,and the latter has a reverse "S-type"structure.Successive Cenozoic sediments are well exposed and magnetostratigraphically dated in both belts.Paleomagnetic declination has great advantage to reveal vertical-axis rotations of geological bodies since they become magnetized. Recently conducted paleomagnetic rotation studies in different parts of these two thrust belts revealed detailed Cenozoic rotation patterns and magnitudes of the region. By integrating these paleomagnetic rotation results with regional geometric features and lines of geological evidence,we propose that these two arcuate thrust belts were most likely caused by different rotations in different parts of these curvatures,due to the sinistral strike-slip faulting along the ATF,rather than originally curved ones. The Yingxiongling arcuate belt was shaped by the significant counterclockwise(CCW) rotations of its northwestern half(the Akatengnengshan anticline) near the ATF during ～ 16 ～ 11 Ma BP,while its southeastern half(the Youshashan anticline) had no significant rotations since at least ～ 20 Ma BP. The geometry of the NQMTB was developed firstly by remarkable clockwise rotations of its middle part during ～ 33 ～ 14 Ma BP,and later possibly CCW rotations of its northwestern part during the Middle to Late Miocene,similar to that of the northwestern part of the Yingxiongling arcuate belt. The characteristics of two-stage strike-slip evolution of the ATF since the Early Oligocene were enriched: 1) During the Early Oligocene to mid-Miocene,fast strike-slip faulting along the ATF was proposed to accommodate the eastward extrusion of the northern Tibetan Plateau with its sinistral shear confined to the fault itself. While in the NQMTB and farther east area in the Qilian Shan, its sinistral shear was transferred to the interior of the plateau and was accommodated by deformation of differential crustal shortenings and block rotations in these regions.Thus,the displacement along the ATF west of the NQMTB is larger than that east of the NQMTB. 2)Since the mid-late Miocene,sinistral shear of the ATF was widespread distributed within the northern Tibetan Plateau,instead of concentrated to the fault itself. Its sinistral offsets were partially absorbed by the shortening deformation within the Qaidam Basin and the Qilian Shan,leading the offsets along the ATF decreasing to the east. With the sinistral frictional drag of blocks(the Tarim Basin and the Altyn Tagh Range) on the other side during the second stage evolution of the ATF,a transitional zone south of the ATF was likely developed by remarkable CCW rotations during the Middle to Late Miocene,which is probably confined to east of the Tula syncline. Combining the sinistral offsets along the ATF derived from the paleomagnetic rotations during the Early Oligocene to mid-late Miocene and that by piercing points since the Late Miocene,the post Oligocene strike-slip offsets were constrained as at least ～ 350 ～ 430 km for the reference in the western Qaidam Basin and ～ 380 ～ 460 km for the reference in the NQMTB,with an average slip rate of at least ～ 10. 6 ～ 13. 9 mm/a. The post Early Oligocene offsets are consistent with the widely accepted offsets of ～ 300 ～ 500 km obtained by piercing point analyses.
引文
常宏.2004.阿尔金山索尔库里盆地晚第三系磁性地层研究与青藏高原北部隆升[D].北京:中国科学院研究生院.CHANG Hong.2004.The magnetostratigraphy study on the Neogene sediments in Suerkal Basin,Altyn Tagh Mountains and the uplift of the northern Tibetan Plateau[D].Graduate University of the Chinese Academy of Sciences,Beijing(in Chinese).
陈正乐,张岳桥,王小凤,等.2001.新生代阿尔金山脉隆升历史的裂变径迹证据[J].地球学报,22(5):413-418.CHEN Zheng-le,ZHANG Yue-qiao,WANG Xiao-feng,et al.2001.Fission track dating of apatite constrains on the Cenozoic uplift of the Altyn Tagh Mountain[J].Acta Geosicientia Sinica,22(5):413-418(in Chinese).
方小敏,吴福莉,韩文霞,等.2008.上新世-第四纪亚洲内陆干旱化过程:柴达木中部鸭湖剖面孢粉和盐类化学指标证据[J].第四纪研究,28(5):874-882.FANG Xiao-min,WU Fu-li,HAN Wen-xia,et al.2008.Plio-Pleistocene drying process of the Asian inlandsporopollen and salinity records from Yahu section in the Central Qaidam Basin[J].Quaternary Sciences,28(5):874-882(in Chinese).
黄宝春,陈军山,易治宇.2010.再论印度与亚洲大陆何时何地发生初始碰撞[J].地球物理学报,53(9):2045-2058.HUANG Bao-chun,CHEN Jun-shan,YI Zhi-yu.2010.Paleomagnetic discussion of when and where India and Asia initially collided[J].Chinese Journal of Geophysics,53(9):2045-2058(in Chinese).
李海兵,杨经绥,许志琴,等.2001.阿尔金断裂带印支期走滑活动的地质及年代学证据[J].科学通报,46(16):1333-1338.LI Hai-bing,YANG Jing-sui,XU Zhi-qin,et al.2002.Geological and chronological evidence of Indo-Chinese strikeslip movement in the Altyn Tagh fault zone[J].Chinese Science Bulletin,47(1):28-33.
李海兵,杨经绥,许志琴,等.2006.阿尔金断裂带对青藏高原北部生长、隆升的制约[J].地学前缘,13(4):59-79.LI Hai-bing,YANG Jing-sui,XU Zhi-qin,et al.2006.The constraint of the Altyn Tagh fault system to the growth and rise of the northern Tibetan Plateau[J].Earth Science Frontiers,13(4):59-79(in Chinese).
李相博,王新民,袁剑英,等.2001.青藏高原东北部旋卷(扭)构造变形遥感探测及其地球动力学与油气地质意义[J].沉积学报,19(3):433-439.LI Xiang-bo,WANG Xin-min,YUAN Jian-ying,et al.2001.Remote sensing findings of vortex structure deformation in the northwest of Qinghai-Tibet Plateau and its significance of geodynamics and oil and gas geology[J].Acta Sedimentologica Sinica,19(3):433-439(in Chinese).
刘永江,葛肖虹,Genser J,等.2003.阿尔金断裂带构造活动的40Ar/39Ar年龄证据[J].科学通报,48(12):1335-1341.LIU Yong-jiang,GE Xiao-hong,Genser J,et al.2003.40Ar/39Ar chronological evidence for movement of the Altyn Tagh fault system[J].Chinese Science Bulletin,48(12):1335-1341(in Chinese).
刘永江,葛肖虹,叶慧文,等.2001.晚中生代以来阿尔金断裂的走滑模式[J].地球学报,22(1):23-28.LIU Yong-jiang,GE Xiao-hong,YE Hui-wen,et al.2001.Strike-slip model for Altyn Tagh Fault developed since Late Mesozoic[J].Acta Geoscientica Sinica,22(1):23-28(in Chinese).
刘永江,Neubauer F,葛肖虹,等.2007.阿尔金断裂带年代学和阿尔金山隆升[J].地质科学,42(1):134-146.LIU Yong-jiang,Neubauer F,GE Xiao-hong,et al.2007.Geochronology of the Altun fault zone and rising of the Altun Mountains[J].Chinese Journal of Geology,42(1):134-146(in Chinese).
裴军令,周在征,李海兵,等.2016.中中新世以来阿尔金断裂走滑未造成柴达木盆地整体旋转[J].吉林大学学报(地球科学版),46(1):163-174.PEI Jun-ling,ZHOU Zai-zheng,LI Hai-bing,et al.2016.Strike-slip of Altyn Tagh didn't result in Qaidam Basin rotation since Middle-Miocene[J].Journal of Jilin University(Earth Science Edition),46(1):163-174(in Chinese).
青海省地质矿产局.1991.青海省区域地质志[M].北京:地质出版社.Qinghai Bureau of Geology and Mineral Resources.1991.Regional Geology of Qinghai Province[M].Geological Publishing House,Beijing(in Chinese).
苏庆达,聂军胜,Saylor J E,等.2016.柴达木盆地大红沟剖面新生代地层磁组构特征及构造意义[J].第四纪研究,36(4):859-869.SU Qing-da,NIE Jun-sheng,Saylor J E,et al.2016.An anisotropy of magnetic susceptibility study of the Cenozoic Dahonggou section in northern Qaidam Basin and its tectonic implications[J].Quaternary Sciences,36(4):859-869(in Chinese).
孙殿卿,段万倜,邓乃公,等.1956.从柴达木盆地旋卷构造现象来探讨这个区域的地质构造[J].地质学报,36(4):417-442.SUN Dian-qing,DUAN Wan-ti,DENG Nai-gong,et al.1956.The Tsaidam vortex structure and its tectonic significance[J].Acta Geological Sinica,36(4):417-442(in Chinese).
孙知明,李海兵,裴军令,等.2012.阿尔金断裂走滑作用对青藏高原东北缘山脉形成的古地磁证据[J].岩石学报,28(6):1928-1936.SUN Zhi-ming,LI Hai-bing,PEI Jun-ling,et al.2012.Strike-slip movement of the Altyn Tagh Fault and implications for mountain formation inferred from paleomagnetic data in northeastern Tibetan Plateau[J].Acta Petrologica Sinica,28(6):1928-1936(in Chinese).
万景林,郑德文,郑文俊,等.2011.MDD法和裂变径迹法相结合模拟样品的低温热历史:以柴达木盆地北缘赛什腾山中新生代构造演化为例[J].地震地质,33(2):369-382.doi:10.3969/j.issn.0253-4967.2011.02.010.WAN Jing-lin,ZHENG De-wen,ZHENG Wen-jun,et al.2011.Model thermal history during low temperature by K-Feldspar MDD and fission track:Example from Meso-Cenozoic tectonic evolution in Saishitengshan in the northern margin of Qaidam Basin[J].Seismology and Geology,33(2):369-382(in Chinese).
王萍,卢演俦,陈杰.2004.阿尔金断裂东端的旋转构造及其动力学意义[J].中国地震,20(2):134-142.WANG Ping,LU Yan-chou,CHEN Jie.2004.Tectonic transformation in the eastern part of the Altun Fault[J].Earthquake Research in China,20(2):134-142(in Chinese).
杨用彪,孟庆泉,宋春晖,等.2009.柴达木盆地东北部新近纪构造旋转及其意义[J].地质论评,55(6):775-784.YANG Yong-biao,MENG Qing-quan,SONG Chun-hui,et al.2009.Neogene tectonic rotation of the NE Qaidam Basin and its implication[J].Geological Review,55(6):775-784(in Chinese).
张伟林.2006.柴达木盆地新生代高精度磁性地层与青藏高原隆升[D].兰州:兰州大学.ZHANG Wei-lin.2006.The high precise Cenozoic magnetostratigraphy of the Qaidam Basin and uplift of the northern Tibetan Plateau[D].Lanzhou University,Lanzhou(in Chinese).
Besse J,Courtillot V.2002.Apparent and true polar wander and the geometry of the geomagnetic field over the last 200million years[J].Journal of Geophysical Research:Solid Earth,107(B11):101029-101060.
Burchfiel B C,Deng Q D,Molnar P,et al.1989.Intracrustal detachment within zones of continental deformation[J].Geology,17(8):748-752.
Butler R F.1992.Paleomagnetism:Magnetic Domains to Geologic Terranes[M].Blackwell Scientific,Malden,Mass.
Chang H,Li L Y,Qiang X K,et al.2015.Magnetostratigraphy of Cenozoic deposits in the western Qaidam Basin and its implication for the surface uplift of the northeastern margin of the Tibetan Plateau[J].Earth and Planetary Science Letters,430:271-283.
Chen J S,Huang B C,Sun L S.2010.New constraints to the onset of the India-Asia collision:Paleomagnetic reconnaissance on the Linzizong Group in the Lhasa Block,China[J].Tectonophysics,489(1):189-209.
Chen Y,Gilder S,Halim N,et al.2002.New paleomagnetic constraints on central Asian kinematics:Displacement along the Altyn Tagh Fault and rotation of the Qaidam Basin[J].Tectonics,21(5):1042.
Chen Z L,Wang X F,Yin A,et al.2004.Cenozoic left-slip motion along the Central Altyn Tagh Fault as inferred from the sedimentary record[J].International Geology Review,46(9):839-856.
Cheng F,Guo Z J,Jenkins H S,et al.2015.Initial rupture and displacement on the Altyn Tagh Fault,northern Tibetan Plateau:Constraints based on residual Mesozoic to Cenozoic strata in the western Qaidam Basin[J].Geosphere,11(3):921-942.
Cheng F,Jolivet M,Fu S T,et al.2014.Northward growth of the Qimen Tagh Range:A new model accounting for the Late Neogene strike-slip deformation of the SW Qaidam Basin[J].Tectonophysics,632:32-47.
Cheng F,Jolivet M,Fu S T,et al.2016.Large-scale displacement along the Altyn Tagh Fault(North Tibet)since its Eocene initiation:Insight from detrital zircon U-Pb geochronology and subsurface data[J].Tectonophysics,677-678:261-279.
CognéJ P,Besse J,Chen Y,et al.2013.A new Late Cretaceous to present APWP for Asia and its implications for paleomagnetic shallow inclinations in Central Asia and Cenozoic Eurasian plate deformation[J].Geophysical Journal International,192(3):1000-1024.
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:Solid Earth,108(B7):2346.
Dai S,Dai W,Zhao Z B,et al.2017.Timing,displacement and growth pattern of the Altyn Tagh Fault:A review[J].Acta Geologica Sinica,91(2):669-687.
Demarest H H.1983.Error analysis for the determination of tectonic rotation from paleomagnetic data[J].Journal of Geophysical Research:Solid Earth,88(B5):4321-4328.
Dupont-Nivet G,Butler R F,Yin A,et al.2002.Paleomagnetism indicates no Neogene rotation of the Qaidam Basin in northern Tibet during Indo-Asian collision[J].Geology,30(3):263.
Dupont-Nivet G,Bulter R F,Yin A,et al.2003.Paleomagnetism indicates no Neogene vertical axis rotations of the northeastern Tibetan Plateau[J].Journal of Geophysical Research:Solid Earth,108(B8):503-518.
Dupont-Nivet G,Robinson D,Butler R F,et al.2004.Concentration of crustal displacement along a weak Altyn Tagh Fault:Evidence from paleomagnetism of the northern Tibetan Plateau[J].Tectonics,23:TC1020.
Fang X M,Zhang W L,Meng Q Q,et al.2007.High-resolution magnetostratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau,Qinghai Province,China and its implication on tectonic uplift of the NE Tibetan Plateau[J].Earth and Planetary Science Letters,258(1-2):293-306.
Gehrels G E,Yin A,Wang X F.2003.Detrital-zircon geochronology of the northeastern Tibetan Plateau[J].Geological Society of America Bulletin,115(7):881-896.
Gilder S,Chen Y,Sen S.2001.Oligo-Miocene magnetostratigraphy and rock magnetism of the Xishuigou section,Subei(Gansu Province,western China)and implications for shallow inclinations in central Asia[J].Journal of Geophysical Research:Solid Earth,106(B12):30505-30521.
He J K,Vernant P,Chéry J,et al.2013.Nailing down the slip rate of the Altyn Tagh Fault[J].Geophysical Research Letters,40(20):5382-5386.
Ji J L,Zhang K X,Clift P D,et al.2017.High-resolution magnetostratigraphic study of the Paleogene-Neogene strata in the northern Qaidam Basin:Implications for the growth of the northeastern Tibetan Plateau[J].Gondwana Research,46:141-155.
Jolivet M,Brunel M,Seward D,et al.2001.Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan Plateau:Fission-track constraints[J].Tectonophysics,343(1-2):111-134.
Li B S,Yan M D,Zhang W L,et al.2017.New paleomagnetic constraints on Middle Miocene strike-slip faulting along the middle Altyn Tagh Fault[J].Journal of Geophysical Research:Solid Earth,122(6):4106-4122.
Li B S,Yan M D,Zhang W L,et al.2018.Paleomagnetic rotation constraints on the deformation of the northern Qaidam marginal thrust belt and implications for strike-slip faulting along the Altyn Tagh Fault[J].Journal of Geophysical Research:Solid Earth,123(9):7207-7224.
Li Z Y,Ding L,Song P P,et al.2015.Paleomagnetic constraints on the paleolatitude of the Lhasa block during the Early Cretaceous:Implications for the onset of India-Asia collision and latitudinal shortening estimates across Tibet and stable Asia[J].Gondwana Research,41:352-382.
Lu H J,Fu B H,Shi P L,et al.2016.Constraints on the uplift mechanism of northern Tibet[J].Earth and Planetary Science Letters,453:108-118.
Lu H J,Wang E,Shi X H,et al.2012.Cenozoic tectonic evolution of the Elashan range and its surroundings,northern Tibetan Plateau as constrained by paleomagnetism and apatite fission track analyses[J].Tectonophysics,580:150-161.
Lu H J,Xiong S F.2009.Magnetostratigraphy of the Dahonggou section,northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault[J].Earth and Planetary Science Letters,288(3-4):539-550.
Mao L G,Xiao A C,Wu L,et al.2014.Cenozoic tectonic and sedimentary evolution of southern Qaidam Basin,NETibetan Plateau and its implication for the rejuvenation of eastern Kunlun Mountains[J].Science in China:Earth Sciences,57(11):2726-2739.
Mao L G,Xiao A C,Zhang H W,et al.2016.Structural deformation pattern within the NW Qaidam Basin in the Cenozoic era and its tectonic implications[J].Tectonophysics,687:78-93.
Meyer B,Tapponnier P,Bourjot L,et al.1998.Crustal thickening in Gansu-Qinghai,lithospheric mantle subduction,and oblique,strike-slip controlled growth of the Tibet plateau[J].Geophysical Journal International,135(1):1-47.
Peltzer G,Tapponnier P.1988.Formation and evolution of strike-slip faults,rifts,and basins during the India-Asia Collision:An experimental approach[J].Journal of Geophysical Research:Solid Earth,93(B12):15085-15117.
Ritts B D,Biffi U.2000.Magnitude of post-Middle Jurassic(Bajocian)displacement on the central Altyn Tagh fault system,northwest China[J].Geological Society of America Bulletin,112(1):61-74.
Robinson D M,Dupont-Nivet G,Gehrels G E,et al.2003.The Tula uplift,northwestern China:Evidence for regional tectonism of the northern Tibetan Plateau during late Mesozoic-early Cenozoic time[J].Geological Society of America Bulletin,115(1):35-47.
Shen F,Royden L H,Burchfiel B C.2001.Large-scale crustal deformation of the Tibetan Plateau[J].Journal of Geophysical Research:Solid Earth,106(B4):6793-6816.
Sobel E R,Arnaud N,Jolivet M,et al.2001.Jurassic to Cenozoic exhumation history of the Altyn Tagh range,northwest China,constrained by40Ar/39Ar and apatite fission track thermochronology[J].Geological Society of America Memoir,194:247-267.
Song B W,Zhang K X,Chen R M,et al.2013.The sedimentary record in northern Qaidam Basin and its response to the uplift of the south Qilian Mountain at around 30Ma[J].Acta Geologica Sinica,87(2):528-539.
Song C H,Hu S H,Han W X,et al.2014.Middle Miocene to earliest Pliocene sedimentological and geochemical records of climate change in the western Qaidam Basin on the NE Tibetan Plateau[J].Palaeogeography,Palaeoclimatology,Palaeoecology,395:67-76.
Sun Z M,Jiang W,Li H B,et al.2010.New paleomagnetic results of Paleocene volcanic rocks from the Lhasa block:Tectonic implications for the collision of India and Asia[J].Tectonophysics,490(3-4):257-266.
Sun Z M,Yang Z Y,Pei J L,et al.2005.Magnetostratigraphy of Paleogene sediments from northern Qaidam Basin,China:Implications for tectonic uplift and block rotation in northern Tibetan Plateau[J].Earth and Planetary Science Letters,237(3-4):635-646.
Vandamme D.1994.A new method to determine paleosecular variation[J].Physics of the Earth and Planetary Interiors,85(1-2):131-142.
Wang E.1997.Displacement and timing along the northern strand of the Altyn Tagh fault zone,Northern Tibet[J].Earth and Planetary Science Letters,150(1-2):55-64.
Wang E,Burchfiel B C.2004.Late Cenozoic right-lateral movement along the Wenquan Fault and associated deformation:Implications for the kinematic history of the Qaidam Basin,northeastern Tibetan Plateau[J].International Geology Review,46(10):861-879.
Wang E,Zhou J X,Wang S F,et al.2008.Vertical-axis bending of the Altyn Tagh belt along the Altyn Tagh Fault:Evidence from late Cenozoic deformation within and around the Xorkol Basin[G].Geological Society of America Special Paper,444:25-44.
Wang F,Lo C H,Li Q,et al.2004.Onset timing of significant unroofing around Qaidam Basin,northern Tibet,China:Constraints from40Ar/39Ar and FT thermochronology on granitoids[J].Journal of Asian Earth Sciences,24(1):59-69.
Wang W T,Zhang P Z,Pang J Z,et al.2016.The Cenozoic growth of the Qilian Shan in the northeastern Tibetan Plateau:A sedimentary archive from the Jiuxi Basin[J].Journal of Geophysical Research:Solid Earth,121(4):2235-2257.
Wang W T,Zheng W J,Zhang P Z,et al.2017.Expansion of the Tibetan Plateau during the Neogene[J].Nature Communications,8:15887.
Wang X M,Wang B Y,Qiu Z X,et al.2003.Danghe area(western Gansu,China)biostratigraphy and implications for depositional history and tectonics of northern Tibetan Plateau[J].Earth and Planetary Science Letters,208(3):253-269.
Wang Y D,Zheng J J,Zhang W L,et al.2012.Cenozoic uplift of the Tibetan Plateau:Evidence from the tectonicsedimentary evolution of the western Qaidam Basin[J].Geoscience Frontiers,3(2):175-187.
Wu L,Kravchinsky V A,Potter D K.2017.Apparent polar wander paths of the major Chinese blocks since the Late Paleozoic:Toward restoring the amalgamation history of east Eurasia[J].Earth-Science Reviews,171:492-519.
Wu L,Xiao A,Wang L,et al.2011.Late Jurassic-early Cretaceous northern Qaidam Basin,NW China:Implications for the earliest Cretaceous intracontinental tectonism[J].Cretaceous Research,32:552-564.
Wu L,Xiao A C,Wang L Q,et al.2012a.EW-trending uplifts along the southern side of the central segment of the Altyn Tagh Fault,NW China:Insight into the rising mechanism of the Altyn Mountain during the Cenozoic[J].Science in China:Earth Sciences,55(6):926-939.
Wu L,Xiao A,Yang S F,et al.2012b.Two-stage evolution of the Altyn Tagh Fault during the Cenozoic:New insight from provenance analysis of a geological section in NW Qaidam Basin,NW China[J].Terra Nova,24(5):387-395.
Yan M D,Fang X M,Van Der Voo R,et al.2013.Neogene rotations in the Jiuquan Basin,Hexi Corridor,China[J].Geological Society,London,Special Publications,373:173-189.
Yan M D,Van Der Voo R,Fang X M,et al.2006.Paleomagnetic evidence for a mid-Miocene clockwise rotation of about 25°of the Guide Basin area in NE Tibet[J].Earth and Planetary Science Letters,241(1-2):234-247.
Yi Z Y,Huang B C,Chen J S,et al.2011.Paleomagnetism of early Paleogene marine sediments in southern Tibet,China:Implications to onset of the India-Asia collision and size of Greater India[J].Earth and Planetary Science Letters,309(1):153-165.
Yin A,Dang Y Q,Wang L C,et al.2008a.Cenozoic tectonic evolution of Qaidam Basin and its surrounding regions(Part 1):The southern Qilian Shan-Nan Shan thrust belt and northern Qaidam Basin[J].Geological Society of America Bulletin,120(7-8):813-846.
Yin A,Dang Y Q,Zhang M,et al.2007.Cenozoic tectonic evolution of Qaidam Basin and its surrounding regions(part2):Wedge tectonics in southern Qaidam Basin and the eastern Kunlun Range[J].In:Sears J W,Harms T A,Evenchick C A,eds.Whence the Mountains?Inquiries into the Evolution of Orogenic Systems:A Volume in Honor of Raymond A Price.Geological Society of America Special Papers,433:369-390.
Yin A,Dang Y Q,Zhang M,et al.2008b.Cenozoic tectonic evolution of the Qaidam Basin and its surrounding regions(Part 3):Structural geology,sedimentation,and regional tectonic reconstruction[J].Geological Society of America Bulletin,120(7-8):847-876.
Yin A,Harrison T M.2000.Geologic evolution of the Himalayan-Tibetan Orogen[J].Annual Review of Earth and Planetary Sciences,28(1):211-280.
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(10):1257-1295.
Yu X J,Fu S T,Guan S W,et al.2014.Paleomagnetism of Eocene and Miocene sediments from the Qaidam Basin:Implication for no integral rotation since the Eocene and a rigid Qaidam block[J].Geochemistry Geophysics Geosystems,15(6):2109-2127.
Yue Y J,Graham S A,Ritts B D,et al.2005.Detrital zircon provenance evidence for large-scale extrusion along the Altyn Tagh Fault[J].Tectonophysics,406(3-4):165-178.
Yue Y J,Liou J G.1999.Two-stage evolution model for the Altyn Tagh Fault,China[J].Geology,27(3):227-230.
Yue Y J,Ritts B D,Graham S A,et al.2003.Slowing extrusion tectonics:Lowered estimate of post-early Miocene slip rate for the Altyn Tagh Fault[J].Earth and Planetary Science Letters,217(1-2):111-122.
Zhuang G S,Hourigan J K,Ritts B D,et al.2011.Cenozoic multiple-phase tectonic evolution of the northern Tibetan Plateau:Constraints from sedimentary records from Qaidam Basin,Hexi Corridor,and Subei Basin northwest China[J].American Journal of Science,311(2):116-152.
陈正乐,张岳桥,王小凤,等.2001.新生代阿尔金山脉隆升历史的裂变径迹证据[J].地球学报,22(5):413-418.CHEN Zheng-le,ZHANG Yue-qiao,WANG Xiao-feng,et al.2001.Fission track dating of apatite constrains on the Cenozoic uplift of the Altyn Tagh Mountain[J].Acta Geosicientia Sinica,22(5):413-418(in Chinese).
方小敏,吴福莉,韩文霞,等.2008.上新世-第四纪亚洲内陆干旱化过程:柴达木中部鸭湖剖面孢粉和盐类化学指标证据[J].第四纪研究,28(5):874-882.FANG Xiao-min,WU Fu-li,HAN Wen-xia,et al.2008.Plio-Pleistocene drying process of the Asian inlandsporopollen and salinity records from Yahu section in the Central Qaidam Basin[J].Quaternary Sciences,28(5):874-882(in Chinese).
黄宝春,陈军山,易治宇.2010.再论印度与亚洲大陆何时何地发生初始碰撞[J].地球物理学报,53(9):2045-2058.HUANG Bao-chun,CHEN Jun-shan,YI Zhi-yu.2010.Paleomagnetic discussion of when and where India and Asia initially collided[J].Chinese Journal of Geophysics,53(9):2045-2058(in Chinese).
李海兵,杨经绥,许志琴,等.2001.阿尔金断裂带印支期走滑活动的地质及年代学证据[J].科学通报,46(16):1333-1338.LI Hai-bing,YANG Jing-sui,XU Zhi-qin,et al.2002.Geological and chronological evidence of Indo-Chinese strikeslip movement in the Altyn Tagh fault zone[J].Chinese Science Bulletin,47(1):28-33.
李海兵,杨经绥,许志琴,等.2006.阿尔金断裂带对青藏高原北部生长、隆升的制约[J].地学前缘,13(4):59-79.LI Hai-bing,YANG Jing-sui,XU Zhi-qin,et al.2006.The constraint of the Altyn Tagh fault system to the growth and rise of the northern Tibetan Plateau[J].Earth Science Frontiers,13(4):59-79(in Chinese).
李相博,王新民,袁剑英,等.2001.青藏高原东北部旋卷(扭)构造变形遥感探测及其地球动力学与油气地质意义[J].沉积学报,19(3):433-439.LI Xiang-bo,WANG Xin-min,YUAN Jian-ying,et al.2001.Remote sensing findings of vortex structure deformation in the northwest of Qinghai-Tibet Plateau and its significance of geodynamics and oil and gas geology[J].Acta Sedimentologica Sinica,19(3):433-439(in Chinese).
刘永江,葛肖虹,Genser J,等.2003.阿尔金断裂带构造活动的40Ar/39Ar年龄证据[J].科学通报,48(12):1335-1341.LIU Yong-jiang,GE Xiao-hong,Genser J,et al.2003.40Ar/39Ar chronological evidence for movement of the Altyn Tagh fault system[J].Chinese Science Bulletin,48(12):1335-1341(in Chinese).
刘永江,葛肖虹,叶慧文,等.2001.晚中生代以来阿尔金断裂的走滑模式[J].地球学报,22(1):23-28.LIU Yong-jiang,GE Xiao-hong,YE Hui-wen,et al.2001.Strike-slip model for Altyn Tagh Fault developed since Late Mesozoic[J].Acta Geoscientica Sinica,22(1):23-28(in Chinese).
刘永江,Neubauer F,葛肖虹,等.2007.阿尔金断裂带年代学和阿尔金山隆升[J].地质科学,42(1):134-146.LIU Yong-jiang,Neubauer F,GE Xiao-hong,et al.2007.Geochronology of the Altun fault zone and rising of the Altun Mountains[J].Chinese Journal of Geology,42(1):134-146(in Chinese).
裴军令,周在征,李海兵,等.2016.中中新世以来阿尔金断裂走滑未造成柴达木盆地整体旋转[J].吉林大学学报(地球科学版),46(1):163-174.PEI Jun-ling,ZHOU Zai-zheng,LI Hai-bing,et al.2016.Strike-slip of Altyn Tagh didn't result in Qaidam Basin rotation since Middle-Miocene[J].Journal of Jilin University(Earth Science Edition),46(1):163-174(in Chinese).
青海省地质矿产局.1991.青海省区域地质志[M].北京:地质出版社.Qinghai Bureau of Geology and Mineral Resources.1991.Regional Geology of Qinghai Province[M].Geological Publishing House,Beijing(in Chinese).
苏庆达,聂军胜,Saylor J E,等.2016.柴达木盆地大红沟剖面新生代地层磁组构特征及构造意义[J].第四纪研究,36(4):859-869.SU Qing-da,NIE Jun-sheng,Saylor J E,et al.2016.An anisotropy of magnetic susceptibility study of the Cenozoic Dahonggou section in northern Qaidam Basin and its tectonic implications[J].Quaternary Sciences,36(4):859-869(in Chinese).
孙殿卿,段万倜,邓乃公,等.1956.从柴达木盆地旋卷构造现象来探讨这个区域的地质构造[J].地质学报,36(4):417-442.SUN Dian-qing,DUAN Wan-ti,DENG Nai-gong,et al.1956.The Tsaidam vortex structure and its tectonic significance[J].Acta Geological Sinica,36(4):417-442(in Chinese).
孙知明,李海兵,裴军令,等.2012.阿尔金断裂走滑作用对青藏高原东北缘山脉形成的古地磁证据[J].岩石学报,28(6):1928-1936.SUN Zhi-ming,LI Hai-bing,PEI Jun-ling,et al.2012.Strike-slip movement of the Altyn Tagh Fault and implications for mountain formation inferred from paleomagnetic data in northeastern Tibetan Plateau[J].Acta Petrologica Sinica,28(6):1928-1936(in Chinese).
万景林,郑德文,郑文俊,等.2011.MDD法和裂变径迹法相结合模拟样品的低温热历史:以柴达木盆地北缘赛什腾山中新生代构造演化为例[J].地震地质,33(2):369-382.doi:10.3969/j.issn.0253-4967.2011.02.010.WAN Jing-lin,ZHENG De-wen,ZHENG Wen-jun,et al.2011.Model thermal history during low temperature by K-Feldspar MDD and fission track:Example from Meso-Cenozoic tectonic evolution in Saishitengshan in the northern margin of Qaidam Basin[J].Seismology and Geology,33(2):369-382(in Chinese).
王萍,卢演俦,陈杰.2004.阿尔金断裂东端的旋转构造及其动力学意义[J].中国地震,20(2):134-142.WANG Ping,LU Yan-chou,CHEN Jie.2004.Tectonic transformation in the eastern part of the Altun Fault[J].Earthquake Research in China,20(2):134-142(in Chinese).
杨用彪,孟庆泉,宋春晖,等.2009.柴达木盆地东北部新近纪构造旋转及其意义[J].地质论评,55(6):775-784.YANG Yong-biao,MENG Qing-quan,SONG Chun-hui,et al.2009.Neogene tectonic rotation of the NE Qaidam Basin and its implication[J].Geological Review,55(6):775-784(in Chinese).
张伟林.2006.柴达木盆地新生代高精度磁性地层与青藏高原隆升[D].兰州:兰州大学.ZHANG Wei-lin.2006.The high precise Cenozoic magnetostratigraphy of the Qaidam Basin and uplift of the northern Tibetan Plateau[D].Lanzhou University,Lanzhou(in Chinese).
Besse J,Courtillot V.2002.Apparent and true polar wander and the geometry of the geomagnetic field over the last 200million years[J].Journal of Geophysical Research:Solid Earth,107(B11):101029-101060.
Burchfiel B C,Deng Q D,Molnar P,et al.1989.Intracrustal detachment within zones of continental deformation[J].Geology,17(8):748-752.
Butler R F.1992.Paleomagnetism:Magnetic Domains to Geologic Terranes[M].Blackwell Scientific,Malden,Mass.
Chang H,Li L Y,Qiang X K,et al.2015.Magnetostratigraphy of Cenozoic deposits in the western Qaidam Basin and its implication for the surface uplift of the northeastern margin of the Tibetan Plateau[J].Earth and Planetary Science Letters,430:271-283.
Chen J S,Huang B C,Sun L S.2010.New constraints to the onset of the India-Asia collision:Paleomagnetic reconnaissance on the Linzizong Group in the Lhasa Block,China[J].Tectonophysics,489(1):189-209.
Chen Y,Gilder S,Halim N,et al.2002.New paleomagnetic constraints on central Asian kinematics:Displacement along the Altyn Tagh Fault and rotation of the Qaidam Basin[J].Tectonics,21(5):1042.
Chen Z L,Wang X F,Yin A,et al.2004.Cenozoic left-slip motion along the Central Altyn Tagh Fault as inferred from the sedimentary record[J].International Geology Review,46(9):839-856.
Cheng F,Guo Z J,Jenkins H S,et al.2015.Initial rupture and displacement on the Altyn Tagh Fault,northern Tibetan Plateau:Constraints based on residual Mesozoic to Cenozoic strata in the western Qaidam Basin[J].Geosphere,11(3):921-942.
Cheng F,Jolivet M,Fu S T,et al.2014.Northward growth of the Qimen Tagh Range:A new model accounting for the Late Neogene strike-slip deformation of the SW Qaidam Basin[J].Tectonophysics,632:32-47.
Cheng F,Jolivet M,Fu S T,et al.2016.Large-scale displacement along the Altyn Tagh Fault(North Tibet)since its Eocene initiation:Insight from detrital zircon U-Pb geochronology and subsurface data[J].Tectonophysics,677-678:261-279.
CognéJ P,Besse J,Chen Y,et al.2013.A new Late Cretaceous to present APWP for Asia and its implications for paleomagnetic shallow inclinations in Central Asia and Cenozoic Eurasian plate deformation[J].Geophysical Journal International,192(3):1000-1024.
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:Solid Earth,108(B7):2346.
Dai S,Dai W,Zhao Z B,et al.2017.Timing,displacement and growth pattern of the Altyn Tagh Fault:A review[J].Acta Geologica Sinica,91(2):669-687.
Demarest H H.1983.Error analysis for the determination of tectonic rotation from paleomagnetic data[J].Journal of Geophysical Research:Solid Earth,88(B5):4321-4328.
Dupont-Nivet G,Butler R F,Yin A,et al.2002.Paleomagnetism indicates no Neogene rotation of the Qaidam Basin in northern Tibet during Indo-Asian collision[J].Geology,30(3):263.
Dupont-Nivet G,Bulter R F,Yin A,et al.2003.Paleomagnetism indicates no Neogene vertical axis rotations of the northeastern Tibetan Plateau[J].Journal of Geophysical Research:Solid Earth,108(B8):503-518.
Dupont-Nivet G,Robinson D,Butler R F,et al.2004.Concentration of crustal displacement along a weak Altyn Tagh Fault:Evidence from paleomagnetism of the northern Tibetan Plateau[J].Tectonics,23:TC1020.
Fang X M,Zhang W L,Meng Q Q,et al.2007.High-resolution magnetostratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau,Qinghai Province,China and its implication on tectonic uplift of the NE Tibetan Plateau[J].Earth and Planetary Science Letters,258(1-2):293-306.
Gehrels G E,Yin A,Wang X F.2003.Detrital-zircon geochronology of the northeastern Tibetan Plateau[J].Geological Society of America Bulletin,115(7):881-896.
Gilder S,Chen Y,Sen S.2001.Oligo-Miocene magnetostratigraphy and rock magnetism of the Xishuigou section,Subei(Gansu Province,western China)and implications for shallow inclinations in central Asia[J].Journal of Geophysical Research:Solid Earth,106(B12):30505-30521.
He J K,Vernant P,Chéry J,et al.2013.Nailing down the slip rate of the Altyn Tagh Fault[J].Geophysical Research Letters,40(20):5382-5386.
Ji J L,Zhang K X,Clift P D,et al.2017.High-resolution magnetostratigraphic study of the Paleogene-Neogene strata in the northern Qaidam Basin:Implications for the growth of the northeastern Tibetan Plateau[J].Gondwana Research,46:141-155.
Jolivet M,Brunel M,Seward D,et al.2001.Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan Plateau:Fission-track constraints[J].Tectonophysics,343(1-2):111-134.
Li B S,Yan M D,Zhang W L,et al.2017.New paleomagnetic constraints on Middle Miocene strike-slip faulting along the middle Altyn Tagh Fault[J].Journal of Geophysical Research:Solid Earth,122(6):4106-4122.
Li B S,Yan M D,Zhang W L,et al.2018.Paleomagnetic rotation constraints on the deformation of the northern Qaidam marginal thrust belt and implications for strike-slip faulting along the Altyn Tagh Fault[J].Journal of Geophysical Research:Solid Earth,123(9):7207-7224.
Li Z Y,Ding L,Song P P,et al.2015.Paleomagnetic constraints on the paleolatitude of the Lhasa block during the Early Cretaceous:Implications for the onset of India-Asia collision and latitudinal shortening estimates across Tibet and stable Asia[J].Gondwana Research,41:352-382.
Lu H J,Fu B H,Shi P L,et al.2016.Constraints on the uplift mechanism of northern Tibet[J].Earth and Planetary Science Letters,453:108-118.
Lu H J,Wang E,Shi X H,et al.2012.Cenozoic tectonic evolution of the Elashan range and its surroundings,northern Tibetan Plateau as constrained by paleomagnetism and apatite fission track analyses[J].Tectonophysics,580:150-161.
Lu H J,Xiong S F.2009.Magnetostratigraphy of the Dahonggou section,northern Qaidam Basin and its bearing on Cenozoic tectonic evolution of the Qilian Shan and Altyn Tagh Fault[J].Earth and Planetary Science Letters,288(3-4):539-550.
Mao L G,Xiao A C,Wu L,et al.2014.Cenozoic tectonic and sedimentary evolution of southern Qaidam Basin,NETibetan Plateau and its implication for the rejuvenation of eastern Kunlun Mountains[J].Science in China:Earth Sciences,57(11):2726-2739.
Mao L G,Xiao A C,Zhang H W,et al.2016.Structural deformation pattern within the NW Qaidam Basin in the Cenozoic era and its tectonic implications[J].Tectonophysics,687:78-93.
Meyer B,Tapponnier P,Bourjot L,et al.1998.Crustal thickening in Gansu-Qinghai,lithospheric mantle subduction,and oblique,strike-slip controlled growth of the Tibet plateau[J].Geophysical Journal International,135(1):1-47.
Peltzer G,Tapponnier P.1988.Formation and evolution of strike-slip faults,rifts,and basins during the India-Asia Collision:An experimental approach[J].Journal of Geophysical Research:Solid Earth,93(B12):15085-15117.
Ritts B D,Biffi U.2000.Magnitude of post-Middle Jurassic(Bajocian)displacement on the central Altyn Tagh fault system,northwest China[J].Geological Society of America Bulletin,112(1):61-74.
Robinson D M,Dupont-Nivet G,Gehrels G E,et al.2003.The Tula uplift,northwestern China:Evidence for regional tectonism of the northern Tibetan Plateau during late Mesozoic-early Cenozoic time[J].Geological Society of America Bulletin,115(1):35-47.
Shen F,Royden L H,Burchfiel B C.2001.Large-scale crustal deformation of the Tibetan Plateau[J].Journal of Geophysical Research:Solid Earth,106(B4):6793-6816.
Sobel E R,Arnaud N,Jolivet M,et al.2001.Jurassic to Cenozoic exhumation history of the Altyn Tagh range,northwest China,constrained by40Ar/39Ar and apatite fission track thermochronology[J].Geological Society of America Memoir,194:247-267.
Song B W,Zhang K X,Chen R M,et al.2013.The sedimentary record in northern Qaidam Basin and its response to the uplift of the south Qilian Mountain at around 30Ma[J].Acta Geologica Sinica,87(2):528-539.
Song C H,Hu S H,Han W X,et al.2014.Middle Miocene to earliest Pliocene sedimentological and geochemical records of climate change in the western Qaidam Basin on the NE Tibetan Plateau[J].Palaeogeography,Palaeoclimatology,Palaeoecology,395:67-76.
Sun Z M,Jiang W,Li H B,et al.2010.New paleomagnetic results of Paleocene volcanic rocks from the Lhasa block:Tectonic implications for the collision of India and Asia[J].Tectonophysics,490(3-4):257-266.
Sun Z M,Yang Z Y,Pei J L,et al.2005.Magnetostratigraphy of Paleogene sediments from northern Qaidam Basin,China:Implications for tectonic uplift and block rotation in northern Tibetan Plateau[J].Earth and Planetary Science Letters,237(3-4):635-646.
Vandamme D.1994.A new method to determine paleosecular variation[J].Physics of the Earth and Planetary Interiors,85(1-2):131-142.
Wang E.1997.Displacement and timing along the northern strand of the Altyn Tagh fault zone,Northern Tibet[J].Earth and Planetary Science Letters,150(1-2):55-64.
Wang E,Burchfiel B C.2004.Late Cenozoic right-lateral movement along the Wenquan Fault and associated deformation:Implications for the kinematic history of the Qaidam Basin,northeastern Tibetan Plateau[J].International Geology Review,46(10):861-879.
Wang E,Zhou J X,Wang S F,et al.2008.Vertical-axis bending of the Altyn Tagh belt along the Altyn Tagh Fault:Evidence from late Cenozoic deformation within and around the Xorkol Basin[G].Geological Society of America Special Paper,444:25-44.
Wang F,Lo C H,Li Q,et al.2004.Onset timing of significant unroofing around Qaidam Basin,northern Tibet,China:Constraints from40Ar/39Ar and FT thermochronology on granitoids[J].Journal of Asian Earth Sciences,24(1):59-69.
Wang W T,Zhang P Z,Pang J Z,et al.2016.The Cenozoic growth of the Qilian Shan in the northeastern Tibetan Plateau:A sedimentary archive from the Jiuxi Basin[J].Journal of Geophysical Research:Solid Earth,121(4):2235-2257.
Wang W T,Zheng W J,Zhang P Z,et al.2017.Expansion of the Tibetan Plateau during the Neogene[J].Nature Communications,8:15887.
Wang X M,Wang B Y,Qiu Z X,et al.2003.Danghe area(western Gansu,China)biostratigraphy and implications for depositional history and tectonics of northern Tibetan Plateau[J].Earth and Planetary Science Letters,208(3):253-269.
Wang Y D,Zheng J J,Zhang W L,et al.2012.Cenozoic uplift of the Tibetan Plateau:Evidence from the tectonicsedimentary evolution of the western Qaidam Basin[J].Geoscience Frontiers,3(2):175-187.
Wu L,Kravchinsky V A,Potter D K.2017.Apparent polar wander paths of the major Chinese blocks since the Late Paleozoic:Toward restoring the amalgamation history of east Eurasia[J].Earth-Science Reviews,171:492-519.
Wu L,Xiao A,Wang L,et al.2011.Late Jurassic-early Cretaceous northern Qaidam Basin,NW China:Implications for the earliest Cretaceous intracontinental tectonism[J].Cretaceous Research,32:552-564.
Wu L,Xiao A C,Wang L Q,et al.2012a.EW-trending uplifts along the southern side of the central segment of the Altyn Tagh Fault,NW China:Insight into the rising mechanism of the Altyn Mountain during the Cenozoic[J].Science in China:Earth Sciences,55(6):926-939.
Wu L,Xiao A,Yang S F,et al.2012b.Two-stage evolution of the Altyn Tagh Fault during the Cenozoic:New insight from provenance analysis of a geological section in NW Qaidam Basin,NW China[J].Terra Nova,24(5):387-395.
Yan M D,Fang X M,Van Der Voo R,et al.2013.Neogene rotations in the Jiuquan Basin,Hexi Corridor,China[J].Geological Society,London,Special Publications,373:173-189.
Yan M D,Van Der Voo R,Fang X M,et al.2006.Paleomagnetic evidence for a mid-Miocene clockwise rotation of about 25°of the Guide Basin area in NE Tibet[J].Earth and Planetary Science Letters,241(1-2):234-247.
Yi Z Y,Huang B C,Chen J S,et al.2011.Paleomagnetism of early Paleogene marine sediments in southern Tibet,China:Implications to onset of the India-Asia collision and size of Greater India[J].Earth and Planetary Science Letters,309(1):153-165.
Yin A,Dang Y Q,Wang L C,et al.2008a.Cenozoic tectonic evolution of Qaidam Basin and its surrounding regions(Part 1):The southern Qilian Shan-Nan Shan thrust belt and northern Qaidam Basin[J].Geological Society of America Bulletin,120(7-8):813-846.
Yin A,Dang Y Q,Zhang M,et al.2007.Cenozoic tectonic evolution of Qaidam Basin and its surrounding regions(part2):Wedge tectonics in southern Qaidam Basin and the eastern Kunlun Range[J].In:Sears J W,Harms T A,Evenchick C A,eds.Whence the Mountains?Inquiries into the Evolution of Orogenic Systems:A Volume in Honor of Raymond A Price.Geological Society of America Special Papers,433:369-390.
Yin A,Dang Y Q,Zhang M,et al.2008b.Cenozoic tectonic evolution of the Qaidam Basin and its surrounding regions(Part 3):Structural geology,sedimentation,and regional tectonic reconstruction[J].Geological Society of America Bulletin,120(7-8):847-876.
Yin A,Harrison T M.2000.Geologic evolution of the Himalayan-Tibetan Orogen[J].Annual Review of Earth and Planetary Sciences,28(1):211-280.
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(10):1257-1295.
Yu X J,Fu S T,Guan S W,et al.2014.Paleomagnetism of Eocene and Miocene sediments from the Qaidam Basin:Implication for no integral rotation since the Eocene and a rigid Qaidam block[J].Geochemistry Geophysics Geosystems,15(6):2109-2127.
Yue Y J,Graham S A,Ritts B D,et al.2005.Detrital zircon provenance evidence for large-scale extrusion along the Altyn Tagh Fault[J].Tectonophysics,406(3-4):165-178.
Yue Y J,Liou J G.1999.Two-stage evolution model for the Altyn Tagh Fault,China[J].Geology,27(3):227-230.
Yue Y J,Ritts B D,Graham S A,et al.2003.Slowing extrusion tectonics:Lowered estimate of post-early Miocene slip rate for the Altyn Tagh Fault[J].Earth and Planetary Science Letters,217(1-2):111-122.
Zhuang G S,Hourigan J K,Ritts B D,et al.2011.Cenozoic multiple-phase tectonic evolution of the northern Tibetan Plateau:Constraints from sedimentary records from Qaidam Basin,Hexi Corridor,and Subei Basin northwest China[J].American Journal of Science,311(2):116-152.
© 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 |