|Table of Contents|

Tectonic Activity in the Southern Alashan Block and the Latest Boundary of Outward Expansion on the Northeastern Tibetan Plateau, China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2021年第02期
Page:
224-236
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Tectonic Activity in the Southern Alashan Block and the Latest Boundary of Outward Expansion on the Northeastern Tibetan Plateau, China
Author(s):
ZHENG Wen-jun1234 ZHANG Bo-xuan1234 YUAN Dao-yang5 CHEN Gan1234 ZHANG Yi-peng1234 YU Jing-xing4 ZHANG Dong-li1234 BI Hai-yun4 LIU Bing-xu1234 YANG Jing-jun1234
(1. School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275, Guangdong, China; 2. Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, Sun Yat-sen University, Guangzhou 510275, Guangdong, China; 3. Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai), Zhuhai 519082, Guangdong, China; 4. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China; 5. School of Earth Sciences, Lanzhou University, Lanzhou 730000, Gansu, China)
Keywords:
tectonic activity geometry kinematics tectonic transformation outward expansion the latest boundary of plateau the southern Alashan block the northeastern Tibetan Plateau
PACS:
P546
DOI:
10.19814/j.jese.2021.01039
Abstract:
Recently, the most controversial and attractive issue in studying the tectonic deformation of the northeastern Tibetan Plateau is the way of northeastward expansion of Tibetan Plateau and the location of the latest active boundary of the northeastern Tibetan Plateau. Based on the investigation and quantitative research of active tectonics in the southern Alashan block and its adjacent regions, the geometry and kinematics of active faults located at the southern Alashan block were summarized. It is pointed out that Alashan block, which has been considered as a stable block, is actually composed of a set of active faults with different sizes and motion characteristics in the Late Cenozoic. These faults are either newly formed during the outward extension of the plateau or the results of reactivation of preexisting faults. The control of these faults on regional geomorphology leads to the geomorphological and tectonic boundary of the southern Alashan block. Combining the research results of Cenozoic deformation, tectonic geomorphology, low-temperature thermalchronology, geodesy and modern seismicity, it is proposed that the northeastern Tibetan Plateau has been expanding outward in a sequential way since the Late Cenozoic and forms two crucial boundaries. One is dominantly controlled by the North Qilian Shan fault since Late Miocene(10 Ma). The another is the latest active boundary which mainly consists of thrust faults located at the southern Alashan block paralleling to North Qilian Shan fault since Pliocene(3-2 Ma). In the present tectonic and geomorphic framework, the southern Alashan block has become the latest component of the northeastern Tibetan Plateau.

References:

[1] BURCHFIEL B,DENG Q D,MOLNAR P,et al.Intracrustal Detachment Within Zones of Continental Deformation[J].Geology,1989,17(8):748-752.
[2] DARBY B J,RITTS B D,YUE Y J,et al.Did the Altyn Tagh Fault Extend Beyond the Tibetan Plateau?[J].Earth and Planetary Science Letters,2005,240(2):425-435.
[3] TAPPONNIER P,XU Z Q,ROGER F,et al.Oblique Stepwise Rise and Growth of the Tibet Plateau[J].Science,2001,294:1671-1677.
[4] VINCENT S J,ALLEN M B.Evolution of the Minle and Chaoshui Basins,China:Implications for Mesozoic Strike-slip Basin Formation in Central Asia[J].GSA Bulletin,1999,111(5):725-742.
[5] LIMB M A,HANSON A D,GRAHAM S A,et al.Left-lateral Sense Offset of Upper Proterozoic to Paleozoic Features Across the Gobi Onon,Tost,and Zuunbayan Faults in Southern Mongolia and Implications for Other Central Asian Faults[J].Earth and Planetary Science Letters,1999,173(3):183-194.
[6] YIN A,RUMELHART P E,BUTLER R,et al.Tectonic History of the Altyn Tagh Fault System in Northern Tibet Inferred from Cenozoic Sedimentation[J].GSA Bulletin,2002,114(10):1257-1295.
[7] ZHANG P Z,MOLNAR P,XU X W.Late Quaternary and Present-day Rates of Slip Along the Altyn Tagh Fault,Northern Margin of the Tibetan Plateau[J].Tectonics,2007,26(5):TC5010.
[8] ZHENG W J,ZHANG P Z,HE W G,et al.Transformation of Displacement Between Strike-slip and Crustal Shortening in the Northern Margin of the Tibetan Plateau:Evidence from Decadal GPS Measurements and Late Quaternary Slip Rates on Faults[J].Tectonophysics,2013,584:267-280.
[9] ZHENG W J,ZHANG P Z,GE W P,et al.Late Quaternary Slip Rate of the South Heli Shan Fault(Northern Hexi Corridor,NW China)and Its Implications for Northeastward Growth of the Tibetan Pla-teau[J].Tectonics,2013,32(2):271-293.
[10] YU J X,ZHENG W J,KIRBY E,et al.Kinematics of Late Quaternary Slip Along the Yabrai Fault:Implications for Cenozoic Tectonics Across the Gobi Alashan Block,China[J].Lithosphere,2016,8(3):199-218.
[11] YU J X,ZHENG W J,ZHANG P Z,et al.Late Quaternary Strike-slip Along the Taohuala Shan-Ayouqi Fault Zone and Its Tectonic Implications in the Hexi Corridor and the Southern Gobi Alashan,China[J].Tectonophysics,2017,721:28-44.
[12] DEWEY J F,BURKE K C A.Tibetan,Variscan,and Precambrian Basement Reactivation:Products of Continental Collision[J].The Journal of Geology,1973,81(6):683-692.
[13] ENGLAND P,HOUSEMAN G.Finite Strain Calculations of Continental Deformation:2.Comparison with the India-Asia Collision Zone[J].Journal of Geophysical Research:Solid Earth,1986,91(B3):3664-3676.
[14] MÉTIVIER F,GAUDEMER Y,TAPPONNIER P,et al.Northeastward Growth of the Tibet Plateau Deduced from Balanced Reconstruction of Two Depositional Areas:The Qaidam and Hexi Corridor Basins,China[J].Tectonics,1998,17(6):823-842.
[15] MEYER B,TAPPONNIER P,BOURJOT L,et al.Crustal Thickening in Gansu-Qinghai,Lithospheric Mantle Subduction,and Oblique,Strike-slip Controlled Growth of the Tibet Plateau [J].Geophysical Journal International,1998,135(1):1-47.
[16] CLARK M K,FARLEY K A,ZHENG D W,et al.Early Cenozoic Faulting of the Northern Tibetan Plateau Margin from Apatite(U-Th)/He Ages[J].Earth and Planetary Science Letters,2010,296(1/2):78-88.
[17] DUVALL A R,CLARK M K,PLUIJM B A,et al.Direct Dating of Eocene Reverse Faulting in Northeastern Tibet Using Ar-dating of Fault Clays and Low-temperature Thermochronometry[J].Earth and Planetary Science Letters,2011,304(3/4):520-526.
[18] DUPONT-NIVET G,HORTON B K,BUTLER R F,et al.Paleogene Clockwise Tectonic Rotation of the Xining-Lanzhou Region,Northeastern Tibetan Plateau[J].Journal of Geophysical Research:Solid Earth,2004,109(B4):B002620.
[19] MOLNAR P,STOCK J M.Slowing of India's Convergence with Eurasia Since 20 Ma and Its Implications for Tibetan Mantle Dynamics[J].Tectonics,2009,28(3):TC0271.
[20] WANG W T,ZHANG P Z,KIRBY E,et al.A Revised Chronology for Tertiary Sedimentation in the Sikouzi Basin:Implications for the Tectonic Evolution of the Northeastern Corner of the Tibetan Plateau[J].Tectonophysics,2011,505(1/2/3/4):100-114.
[21] WANG W T,ZHANG P Z,PANG J Z,et al.The Cenozoic Growth of the Qilian Shan in the Northeastern Tibetan Plateau:A Sedimentary Archive from the Jiu-xi Basin[J].Journal of Geophysical Research:Solid Earth,2016,121(4):2235-2257.
[22] YUAN D Y,GE W P,CHEN Z W,et al.The Growth of Northeastern Tibet and Its Relevance to Large-scale Continental Geodynamics:A Review of Recent Studies[J].Tectonics,2013,32(5):1358-1370.
[23] ZHENG W J,ZHANG H P,ZHANG P Z,et al.Late Quaternary Slip Rates of the Thrust Faults in Western Hexi Corridor(Northern Qilian Shan,China)and Their Implications for Northeastward Growth of the Tibetan Plateau[J].Geosphere,2013,9(2):342-354.
[24] 郑文俊,袁道阳,张培震,等.青藏高原东北缘活动构造几何图像、运动转换与高原扩展[J].第四纪研究,2016,36(4):775-788.
ZHENG Wen-jun,YUAN Dao-yang,ZHANG Pei-zhen,et al.Tectonic Geometry and Kinematic Dissipation of the Active Faults in the Northeastern Tibetan Plateau and Their Implication for Understanding Northeastward Growth of the Plateau[J].Quaternary Sciences,2016,36(4):775-788.
[25] 郑文俊,张培震,袁道阳,等.中国大陆活动构造基本特征及其对区域动力过程的控制[J].地质力学学报,2019,25(5):699-721.
ZHENG Wen-jun,ZHANG Pei-zhen,YUAN Dao-yang,et al.Basic Characteristics of Active Tectonics and Associated Geodynamic Processes in Continental China[J].Journal of Geomechanics,2019,25(5):699-721.
[26] PALUMBO L,HETZEL R,TAO M X,et al.Topographic and Lithologic Control on Catchment-wide Denudation Rates Derived from Cosmogenic 10Be in Two Mountain Ranges at the Margin of NE Tibet[J].Geomorphology,2010,117(1/2):130-142.
[27] PALUMBO L,HETZEL R,TAO M X,et al.Deciphering the Rate of Mountain Growth During Topographic Presteady State:An Example from the NE Margin of the Tibetan Plateau[J].Tectonics,2009,28(4):TC0245.
[28] TAPPONNIER P,PELTZER G,DAIN A Y L,et al.Propagating Extrusion Tectonics in Asia:New Insights from Simple Experiments with Plasticine[J].Geology,1982,10(12):611-616.
[29] 陈文彬,徐锡伟.阿拉善地块南缘的左旋走滑断裂与阿尔金断裂带的东延[J].地震地质,2006,28(2):319-324.
CHEN Wen-bin,XU Xi-wei.Sinistral Strike-slip Faults Along the Southern Alashan Margin and Eastwards Extending of the Altun Fault[J].Seismology and Geology,2006,28(2):319-324.
[30] 邓起东,张培震,冉勇康,等.中国活动构造基本特征[J].中国科学:D辑,地球科学,2002,32(12):1020-1030.
DENG Qi-dong,ZHANG Pei-zhen,RAN Yong-kang,et al.Basic Characteristics of Active Tectonics of China[J].Science in China:Series D,Earth Sciences,2002,32(12):1020-1030.
[31] YUE Y J,LIOU J.Two-stage Evolution Model for the Altyn Tagh Fault,China[J].Geology,1999,27(3):227-230.
[32] YUE Y J,LIOU J,GRAHAM S.Tectonic Correlation of Beishan and Inner Mongolia Orogens and Its Implications for the Palinspastic Reconstruction of North China[J].GSA Memoirs,2001,194:101-116.
[33] WEBB L,JOHNSON C.Tertiary Strike-slip Faulting in Southeastern Mongolia and Implications for Asian Tectonics[J].Earth and Planetary Science Letters,2006,241(1/2):323-335.
[34] YIN A,DANG Y Q,ZHANG M,et al.Cenozoic Tectonic Evolution of the Qaidam Basin and Its Surrounding Regions(Part 3):Structural Geology,Sedimentation,and Regional Tectonic Reconstruction[J].GSA Bulletin,2008,120(7/8):847-876.
[35] YIN A,DANG Y Q,WANG L C,et al.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].GSA Bulletin,2008,120(7/8):813-846.
[36] YIN A,DANG Y Q,ZHANG M,et al.Cenozoic Tectonic Evolution of Qaidam Basin and Its Surrounding Regions(Part 2):Wedge Tectonics in Southern Qai-dam Basin and the Eastern Kunlun Range[J].GSA Special Paper,2007,433:369-390.
[37] HETZEL R,TAO M X,NIEDERMANN S,et al.Implications of the Fault Scaling Law for the Growth of Topography:Mountain Ranges in the Broken Foreland of North-East Tibet[J].Terra Nova,2004,116(3):157-162.
[38] BI H Y,ZHENG W J,GE W P,et al.Constraining the Distribution of Vertical Slip on the South Heli Shan Fault(Northeastern Tibet)from High-resolution Topographic Data[J].Journal of Geophysical Research:Solid Earth,2018,123(3):2484-2501.
[39] YANG J J,ZHENG W J,WANG Y,et al.Quantitative Geomorphological Constraints on the Landform Evolution of the Current Active Boundary of the Northeastern Tibetan Plateau[J].Geomorphology,2020,358:107-120.
[40] 方小敏,赵志军,李吉均,等.祁连山北缘老君庙背斜晚新生代磁性地层与高原北部隆升[J].中国科学:D辑,地球科学,2004,34(2):97-106.
FANG Xiao-min,ZHAO Zhi-jun,LI Ji-jun,et al.Magnetostratigraphy of the Late Cenozoic Laojunmiao Anticline in the Northern Qilian Mountains and Its Implications for the Northern Tibetan Plateau Uplift[J].Science in China:Series D,Earth Sciences,2004,34(2):97-106.
[41] RITTS B,YUE Y J,GRAHAM SA.Oligocene-Miocene Tectonics and Sedimentation Along the Altyn Tagh Fault,Northern Tibetan Plateau:Analysis of the Xorkol,Subei,and Aksay Basins[J].The Journal of Geology,2004,112(2):207-229.
[42] CLARK M,ROYDEN L,BURCHFIEL B,et al.Late Cenozoic Uplift of Southeastern Tibet[J].Geology,2003,33(6):525-528.
[43] KIRBY E,REINERS P,KROL M,et al.Late Cenozoic Evolution of the Eastern Margin of the Tibetan Plateau:Inferences from 40Ar/39Ar and(U-Th)/He Thermochronology[J].Tectonics,2002,21(1):TC001246.
[44] ZHENG D W,CLARK M,ZHANG P Z,et al.Erosion,Fault Initiation and Topographic Growth of the North Qilian Shan(Northern Tibetan Plateau)[J].Geosphere,2010,6(6):937-941.
[45] ZHENG D W,ZHANG P Z,WAN J L,et al.Rapid Exhumation at ~8 Ma on the Liupan Shan Thrust Fault from Apatite Fission-track Thermochronology:Implications for Growth of the Northeastern Tibetan Plateau Margin[J].Earth and Planetary Science Letters,2006,248(1/2):198-208.
[46] WANG W T,ZHENG D W,LI C Y,et al.Cenozoic Exhumation of the Qilian Shan in the Northeastern Tibetan Plateau:Evidence from Low-temperature Thermochronology[J].Tectonics,2020,39(4):TC005705.
[47] ZHENG D W,WANG W T,WAN J L,et al.Progressive Northward Growth of the Northern Qilian Shan-Hexi Corridor(Northeastern Tibet)During the Cenozoic[J].Lithosphere,2017,9(3):408-416.
[48] WANG Y Z,ZHENG D W,PANG J Z,et al.Using Slope-area and Apatite Fission Track Analysis to Decipher the Rock Uplift Pattern of the Yumu Shan:New Insights into the Growth of the NE Tibetan Plateau[J].Geomorphology,2018,308:18-128.
[49] 袁道阳,张培震,刘百篪,等.青藏高原东北缘晚第四纪活动构造的几何图像与构造转换[J].地质学报,2004,78(2):270-278.
YUAN Dao-yang,ZHANG Pei-zhen,LIU Bai-chi,et al.Geometrical Imagery and Tectonic Transformation of Late Quaternary Active Tectonics in Northeastern Margin of Qinghai-Xizang Plateau[J].Acta Geologica Sinica,2004,78(2):270-278.
[50] REPLUMAZ A,TAPPONNIER P.Reconstruction of the Deformed Collision Zone Between India and Asia by Backward Motion of Lithospheric Blocks[J].Journal of Geophysical Research:Solid Earth,2003,108(B6):B000661.
[51] HETZEL R.Active Faulting,Mountain Growth,and Erosion at the Margins of the Tibetan Plateau Constrained by In-situ-produced Cosmogenic Nuclides[J].Tectonophysics,2013,582:1-24.
[52] 张培震,邓起东,张竹琪,等.中国大陆的活动断裂、地震灾害及其动力过程[J].中国科学:地球科学,2013,43(10):1607-1620.
ZHANG Pei-zhen,DENG Qi-dong,ZHANG Zhu-qi,et al.Active Faults,Earthquake Hazards and Associated Geodynamic Processes in Continental China[J].Science China:Earth Sciences,2013,43(10):1607-1620.
[53] 张培震,张会平,郑文俊,等.东亚大陆新生代构造演化[J].地震地质,2014,36(3):574-585.
ZHANG Pei-zhen,ZHANG Hui-ping,ZHENG Wen-jun,et al.Cenozoic Tectonic Evolution of Continental Eastern Asia[J].Seismology and Geology,2014,36(3):574-585.
[54] LIU X W,YUAN D Y,SU Q.Late Pleistocene Slip Rate of the Northern Qilian Shan Frontal Thrust,Western Hexi Corridor,China[J].Terra Nova,2017,29(4):238-244.
[55] LIU X W,YUAN D Y,SU Q.Late Pleistocene Slip Rate on a Blind Thrust in the Western Qilian Shan,NW China[J].Geomorphology,2019,345:106841.
[56] YANG H B,YANG X P,ZHAN Y,et al.Quaternary Activity of the Beihewan Fault in the Southeastern Beishan Wrench Belt,Western China:Implications for Crustal Stability and Intraplate Earthquake Hazards North of Tibet[J].Journal of Geophysical Research:Solid Earth,2019,124(12):13286-13309.
[57] YANG H B,YANG X P,ZHANG H P,et al.Active Fold Deformation and Crustal Shortening Rates of the Qilian Shan Foreland Thrust Belt,NE Tibet,Since the Late Pleistocene[J].Tectonophysics,2018,742:84-100.
[58] 张培震,郑德文,尹功明,等.有关青藏高原东北缘晚新生代扩展与隆升的讨论[J].第四纪研究,2006,26(1):5-13.
ZHANG Pei-zhen,ZHENG De-wen,YIN Gong-ming,et al.Discussion on Late Cenozoic Growth and Rise of Northeastern Margin of the Tibetan Plateau[J].Quaternary Sciences,2006,26(1):5-13.
[59] 葛伟鹏,王 敏,沈正康,等.柴达木—祁连山地块内部震间上地壳块体运动特征与变形模式研究[J].地球物理学报,2013,56(9):2994-3010.
GE Wei-peng,WANG Min,SHEN Zheng-kang,et al.Intersiesmic Kinematics and Deformation Patterns on the Upper Crust of Qaidam-Qilianshan Block[J].Chinese Journal of Geophysics,2013,56(9):2994-3010.
[60] MOLNAR P.Mio-Pliocene Growth of the Tibetan Plateau and Evolution of East Asian Climate[J].Palaeontologia Electronica,2005,8(1):1A.
[61] 郑文俊,张培震,袁道阳,等.甘肃高台合黎山南缘发现地震地表破裂带[J].地震地质,2009,31(2):247-255.
ZHENG Wen-jun,ZHANG Pei-zhen,YUAN Dao-yang,et al.Discovery of Surface Rupture Zone on the South of Helishan in Gaotai,Gansu Province[J].Seismology and Geology,2009,31(2):247-255.
[62] 张 宁,郑文俊,刘兴旺,等.河西走廊西端黑山断裂运动学特征及其在构造转换中的意义[J].地球科学与环境学报,2016,38(2):245-257.
ZHANG Ning,ZHENG Wen-jun,LIU Xing-wang,et al.Kinematics Characteristics of Heishan Fault in the Western Hexi Corridor and Its Implications for Regional Tectonic Transformation[J].Journal of Earth Sciences and Environment,2016,38(2):245-257.
[63] 张 波,何文贵,庞 炜,等.青藏块体北部金塔南山断裂晚第四纪走滑活动的地质地貌特征[J].地震地质,2016,38(1):1-21.
ZHANG Bo,HE Wei-gui,PANG Wei,et al.Geologi-cal and Geomorphic Expressions of Late Quaternary Strike-slip Activity on Jinta Nanshan Fault in Northern Edge of Qing-Zang Block[J].Seismology and Geology,2016,38(1):1-21.
[64] 雷启云,张培震,郑文俊,等.青藏高原东北缘三关口—牛首山断裂的右旋走滑与弧形构造带扩展[J].中国科学:地球科学,2016,59(5):1025-1040.
LEI Qi-yun,ZHANG Pei-zhen,ZHENG Wen-jun,et al.Dextral Strike-slip of Sanguankou-Niushoushan Fault Zone and Extension of Arc Tectonic Belt in the Northeastern Margin of the Tibet Plateau[J].Science China:Earth Sciences,2016,59(5):1025-1040.
[65] LIU J R,REN Z K,ZHENG W J,et al.Late Quaternary Slip Rate of the Aksay Segment and Its Rapidly Decreasing Gradient Along the Altyn Tagh Fault[J].Geosphere,2020,16(6):1538-1557.
[66] LIU R,LI A,ZHANG S M,et al.A NW-striking Dextral Strike-slip Fault at the Eastern End of the Altyn Tagh Fault and Its Tectonic Implications for Northeastward Growth of the Tibetan Plateau[J].Journal of Asian Earth Sciences,2020,188:104069.
[67] 陈 涛,刘玉刚,闵 伟,等.塔尔湾断裂活动时代厘定及地貌陡坎成因分析[J].地震地质,2012,34(3):401-414.
CHEN Tao,LIU Yu-gang,MIN Wei,et al.The Activity Age of Tarwan Fault and Genesis of the Topographic Scarp[J].Seismology and Geology,2012,34(3):401-414.
[68] 俞晶星,郑文俊,雷启云,等.阿拉善地块南部雅布赖山前断裂的运动学特征及意义初探[J].地震地质,2013,35(4):731-744.
YU Jing-xing,ZHENG Wen-jun,LEI Qi-yun,et al.Neotectonics and Kinemetics Along the Yabrai Range-front Fault in the South Alashan Block and Its Implications for Regional Tectonics[J].Seismology and Geology,2013,35(4):731-744.
[69] 郑文俊,张竹琪,张培震,等.1954年山丹71/4级地震的孕震构造和发震机制探讨[J].地球物理学报,2013,56(3):916-928.
ZHENG Wen-ju,ZHANG Zhu-qi,ZHANG Pei-zhen,et al.Seismogenic Structure and Mechanism of the 1954 M71/4 Shandan Earthquake,Gansu Province,Western China[J].Chinese Journal of Geophysics,2013,56(3):916-928.
[70] 李佳昱,郑文俊,王伟涛,等.青藏高原东北部龙首山晚新生代剥露历史:来自磷灰石(U-Th)/He的证据[J].地震地质,2020,42(2):472-491.
LI Jia-yu,ZHENG Wen-jun,WANG Wei-tao,et al.The Northward Growth of the Northeastern Tibetan Plateau in Late Cenozoic:Implications from Apatite(U-Th)/He Ages of Longshou Shan[J].Seismology and Geology,2020,42(2):472-491.
[71] 俞晶星.雅布赖山前断裂晚第四纪滑动速率与古地震[D].北京:中国地震局地质研究所,2013.
YU Jing-xing.Late Quaternary Slip Rates and Paleoearthquakes Along the Yabrai Range-front Fault in the Southern Gobi-Alashan Block[D].Beijing:Institute of Geology,China Earthquake Administration,2013.
[72] 俞晶星.阿拉善地块南部构造活动及其对周边地块相互作用的响应[D].北京:中国地震局地质研究所,2016.
YU Jing-xing.Active Tectonics in the Southern Gobi-Alashan Block and Its Response to the Interactions of the Adjacent Crustal Blocks[D].Beijing:Institute of Geology,China Earthquake Administration,2016.
[73] 陈 虹,胡健民,公王斌,等.青藏高原东北缘牛首山—罗山断裂带新生代构造变形与演化[J].地学前缘,2013,20(4):18-35.
CHEN Hong,HU Jian-ming,GONG Wang-bin,et al.Cenozoic Deformation and Evolution of the Niushou Shan-Luo Shan Fault Zone in the Northeast Margin of the Tibet Plateau[J].Earth Science Frontiers,2013,20(4):18-35.
[74] YU J X,PANG J Z,WANG Y Z,et al.Mid-Miocene Uplift of the Northern Qilian Shan as a Result of the Northward Growth of the Northern Tibetan Plateau[J].Geosphere,2019,15(2):423-432.
[75] LI B,CHEN X H,ZUZA A V,et al.Cenozoic Cooling History of the North Qilian Shan,Northern Tibetan Plateau,and the Initiation of the Haiyuan Fault:Constraints from Apatite- and Zircon-fission Track Thermochronology[J].Tectonophysics,2019,751:109-124.
[76] PANG J Z,YU J X,ZHENG D W,et al.Neogene Expansion of the Qilian Shan,North Tibet:Implications for the Dynamic Evolution of the Tibetan Plateau[J].Tectonics,2019,38(3):1018-1032.
[77] WANG W T,ZHENG W J,ZHANG P Z,et al.Expansion of the Tibetan Plateau During the Neogene[J].Nature Communications,2017,8:15887.
[78] GEORGE A,MARSHALLSEA S,WYRWOLL K,et al.Miocene Cooling in the Northern Qilian Shan,Northeastern Margin of the Tibetan Plateau,Revealed by Apatite Fission-track and Vitrinite-reflectance Analysis[J].Geology,2001,29(10):939-942.
[79] BOVET P,RITTS B,GEHRELS G,et al.Evidence of Miocene Crustal Shortening in the North Qilian Shan from Cenozoic Stratigraphy of the Western Hexi Corridor,Gansu Province,China[J].American Journal of Science,2009,309(4):290-329.
[80] WANG W T,KIRBY E,ZHANG P Z,et al.Tertiary Basin Evolution Along the Northeastern Margin of the Tibetan Plateau:Evidence for Basin Formation During Oligocene Transtension[J].GSA Bulletin,2013,125(3/4):377-400.
[81] ZHENG G,WANG H,WRIGHT T J,et al.Crustal Deformation in the India-Eurasia Collision Zone from 25 Years of GPS Measurements:Crustal Deformation in Asia from GPS[J].Journal of Geophysical Research:Solid Earth,2017,122(13):9290-9312.
[82] 王伟涛,张培震,郑德文,等.青藏高原东北缘海原断裂带晚新生代构造变形[J].地学前缘,2014,21(4):266-274.
WANG Wei-tao,ZHANG Pei-zhen,ZHENG De-wen,et al.Late Cenozoic Tectonic Deformation of the Haiyuan Fault Zone in the Northeastern Margin of the Tibetan Plateau[J].Earth Science Frontiers,2014,21(4):266-274.

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Last Update: 2021-04-15