平衡剖面反映的柴西新生代变形对青藏高原隆升的响应
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摘要
柴达木盆地为一中新生代盆地,位于青藏高原北缘,盆内中新生代地层发育很好地记录了印度-欧亚板块自约55 Ma以来碰撞传到高原北缘的地质事件.在最新的高精度磁性地层绝对年代控制下,通过盆内西部五条北东-南西向地震大剖面,用平衡剖面方法恢复了新生代以来盆地因两大板块碰撞而引起的地壳收敛缩短量.结果显示:在宏观上柴西地区存在两个相对快速收缩期:早始新世-渐新世和晚中新世或上新世-现今(E_(1+2)末-N_1,43.80～22.00 Ma和N_2~2或N_2~3-现今,8.20或2.65～0 Ma)和两个相对较弱收缩期:中生代末-早始新世和渐新世-晚中新世(Mz-E_(1+2)初期,65.00～43.80 Ma和N_1末-N_2~2,22.00～2.65 Ma)以及两个主要的断裂活动期次,早期路乐河组末-下干柴沟组上段时期(E_(1+2)-E_3~2)和晚期上油砂山组至今(N_2~2-Q).在微观上,盆地内部受自身断裂活动的控制,发育了独特的形态.表明在印欧板块碰撞高原隆升的早期,柴西地区就开始变形响应,随后盆地在整个新生代发展过程中,都处于板块碰撞高原隆升的大环境影响下而发生整体的变形缩短,同时自身的断裂活动控制了盆地的微观形态.
Qaidam Basin in the northern margin of the Tibetan Plateau is a large mesozoic-cenozoic basin and bears huge thick continuous cenozoic strata,recording well the geological events of collision of India with Eurasia since 55 Ma.Based on latest progress in precise dating of stratigraphy,a technique of balanced section was applied to five NE-SW seismic geological profiles in the western Qaidam Basin to reconstruct the crust shortening history from collision and to understand the nature of the basin.Two main rapid deformation periods were determined:the early eocene-oligocene and the late miocene or the pliocene to today(the end of E_(1+2)-N_1,43.80～22.00 Ma and N_2~2 or N_2~3 to now,8.20 or 2.65～0 Ma) and two main slow shorting periods:the end of mesozoic to the early eocene and the oligocene to the late miocene(the early Mz—E_(1+2), 65.00～43.80 Ma and the end of N_1-N_2~2,22.00～2.65 Ma).At the same time,there were two main the fault activity periods in the western Qaidam Basin.The one movement period was the end of the Lulehe formation to Xiaganchaigou formation(E_(1+2)-E_3~2) and the other was since the Xiayoushashan formation(N_2~2-Q).The Qaidam Basin's evolution was controlled by the faults action in the cenozoic and it shaped the particular modality.The results showed that the western Qaidam Basin began to deform weakly nearly synchronous to the early collision and the Tibetan Plateau uplift,and continued to the present.Qaidam Basin formed the particular shape that is controlled on the fault movement in the interior.
Qaidam Basin in the northern margin of the Tibetan Plateau is a large mesozoic-cenozoic basin and bears huge thick continuous cenozoic strata,recording well the geological events of collision of India with Eurasia since 55 Ma.Based on latest progress in precise dating of stratigraphy,a technique of balanced section was applied to five NE-SW seismic geological profiles in the western Qaidam Basin to reconstruct the crust shortening history from collision and to understand the nature of the basin.Two main rapid deformation periods were determined:the early eocene-oligocene and the late miocene or the pliocene to today(the end of E_(1+2)-N_1,43.80～22.00 Ma and N_2~2 or N_2~3 to now,8.20 or 2.65～0 Ma) and two main slow shorting periods:the end of mesozoic to the early eocene and the oligocene to the late miocene(the early Mz—E_(1+2), 65.00～43.80 Ma and the end of N_1-N_2~2,22.00～2.65 Ma).At the same time,there were two main the fault activity periods in the western Qaidam Basin.The one movement period was the end of the Lulehe formation to Xiaganchaigou formation(E_(1+2)-E_3~2) and the other was since the Xiayoushashan formation(N_2~2-Q).The Qaidam Basin's evolution was controlled by the faults action in the cenozoic and it shaped the particular modality.The results showed that the western Qaidam Basin began to deform weakly nearly synchronous to the early collision and the Tibetan Plateau uplift,and continued to the present.Qaidam Basin formed the particular shape that is controlled on the fault movement in the interior.
引文
[1]SHACKLETON N J,BACHKMAN J,ZIMMEMAN H, et al.Oxygen isotope calibration of the onset of icerafting and history of glaciation in the north Atlantic region[J].Nature,1984,307:620-623.
[2]MILLER K G,FAIRBANKS R G,MOUNTAIN G S. Tertiary oxygen isotope synthesis,sea level history, and continental margin erosion[J].Paleoceanography, 1987,2(1):1-19.
[3]RAYMO M E,RUDDIMAN W F.Tectonic forcing of late cenozoic climate[J].Nature,1992,359: 117-122.
[4]LI Ji-jun.The environmental effects of the uplift of the Qinghai-Xizang Plateau[J].Quaternary Science Reviews,1991,10(6):478-483.
[5]李吉均,李炳元.青藏高原隆升与全球变化[M].兰州:兰州大学出版社,1995:181-207.
[6]MOLNAR P,CHEN W P.Depths and fault plane solutions of earthquakes under the Tibetan Plateau[J].Geophys Res,1983,88:1 180-1 196.
[7]李吉均,方小敏.青藏高原隆升与环境变化研究[J].科学通报,1998,43(15):1 569-1 574.
[8]READ K,SNOECKX H,JOSEPH L H.Late cenozoic eolian deposition in the north Pacific:Asian drying,Tibetan uplift,and cooling of the northern hemisphere[J].Paleoceanography,1998,13(3): 215-224.
[9]施雅风,汤懋苍,马玉贞.青藏高原二期隆升与亚洲季风孕育关系探讨[J].中国科学D辑:地球科学,1998,28(3):263-271.
[10]安芷生,符淙斌.全球变化科学的进展[J].地球科学进展,2001,16(5):671-680.
[11]KROON D,STEENS T N F,TROELSTRA S R.Onset of monsoonal related upwelling in the western Arabian Sea as revealed by planktonic foraminifers[C]// PRELL W L,NIITSUMA N.Proceedings of the Ocean Drilling Program,Scientific Results.Texas: Ocean Drilling Program,1991:257-264.
[12]徐先海,方小敏,付开道.甘肃临夏盆地8～6 MaBP的构造变化[J].兰州大学学报:自然科学版,2006, 42(6):1-5.
[13]王勇,潘保田,崔明.1.2～0.6 MaBP青藏高原的隆升与东亚地表各圈层的相互作用[J].兰州大学学报:自然科学版,2006,42(3):1-7.
[14]SOOFI M A,KING S D.Oblique convergence between India and Eurasia[J].Geophysical Research, 2002,107(5):ETG3-1-ETG3-8.
[15]JOHNSON M R W.Shortening budgets and the role of continental subduction during the India-Asia collision[J].Earth Science Reviews,2002,59: 101-123.
[16]YIN An,HARRISON T M.Geologic evolution of the Himalaya-Tibetan orogen[J].Annu Rev Earth Planet Sci,2000,28:211-280.
[17]YIN An.Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry,exhumation history, and foreland sedimentation[J].Earth Science Reviews, 2006,76(1-2):1-131.
[18]SHEN Zhen-gang,WANG Min,LI Yan-xing,et al. Crustal deformation along the Altyn Tang fanult system,western China,from GPS[J].Journal of Geophysical Research,2001,106:30 607-30 621.
[19]ZHANG Pei-zhen,SHEN Zheng-kang,WANG Min, et al.Continuous deformation of the Tibetan Plateau from global position system data[J].Geology, 2004,32(9):809-812.
[20]宋廷光.同沉积逆断层的发育特点及油气聚集条件[J].青海地质,1997(2):6-13.
[21]翟光明,徐凤银,李建青.重新认识柴达木盆地、力争油气勘探的新突破[J].石油学报,1997,18(2): 1-7.
[22]陈世悦,徐凤银,彭德华.柴达木盆地基底构造特征及其控油意义[J].新疆石油地质,2000,21(3): 1-7.
[23]尚尔杰.柴达木盆地北缘西段第三系构造基本样式及石油地质意义[J].现代地质,2001,15(4): 421-424.
[24]王信国,曹代勇,占文锋,等.柴达木盆地北缘中、新生代盆地性质及构造演化[J].现代地质,2006, 20(4):592-596.
[25]范连顺,王明儒.柴达木盆地茫崖坳陷含油气系统及勘探方向[J].石油实验地质,1999,21(1): 41-47.
[26]汤良杰,金之钧,张明利,等.柴达木盆地北缘构造演化与油气成藏阶段[J].石油勘探与开发,2000, 27(2):36-39.
[27]XIA Wen-cheng,ZHANG Ning,YUAN Xiao-ping, et al.Cenozoic Qaidam Basin,China:a stronger tectonic inversed,extensional rifted basin[J].AAPG Bulletin,2001,85(4):715-736.
[28]王成善,朱利东,刘志飞.青藏高原北部盆地构造沉积演化与高原向北生长过程[J].地球科学进展, 2004,19(3):373-381.
[29]ZHU Li-dong,WANG Cheng-shan,ZHENG Hong-bo, et al.Tectonic and sedimentary evolution of basins in the northeast of Qinghai-Tibet Plateau and their implication for the northward growth of the Plateau[J].Palaeogeography Palaeoclimateology Palaeoecology,2006,241:49-60.
[30]王桂宏,谭彦虎,陈新领,等.新生代柴达木盆地构造演化与油气勘探领域[J].中国石油勘探, 2006(1):80-84.
[31]王步清.柴达木盆地新生代构造演化与沉积特征[J].新疆石油地质,2006,27(6):670-672.
[32]吴光大,葛肖虹,刘永江,等.柴达木盆地中、新生代构造演化及其对油气的控制[J].世界地质,2006, 25(4):411-417.
[33]杨藩,马志强,许同春,等.柴达木盆地第三纪磁性地层柱[J].石油学报,1992,13(2):97-101.
[34]刘泽纯,孙世英,杨藩,等.柴达木盆地三湖地区第四纪地层学和其年代学分析[J].中国科学B辑:化学,1990,20(11):1 202-1 212.
[35]刘泽纯,范连顺.柴达木盆地茫崖凹陷井下第三系的年代地层学与气候地层学研究[J].地层学杂志, 1996,20(2):104-113.
[36]孙知明,杨振宇,葛肖虹,等.柴达木盆地西北缘古近系磁性年代研究进展[J].地质通报,2004, 23(9/10):899-902.
[37]LIU Ze-chun,WANG Yong-jin,CHEN Yan-an,et al. Magnetostrigraphy and sedimentologically derived geochronology of the quaternary lacustrine deposits of a 3 000 m thick sequence in the central Qaidam Basin,western China[J].Palaeogeography Palaeoclimatology Palaeoecology,1998,140(1-4): 459-473.
[38]SUN Zhi-ming,YANG Zhen-yu,PEI Jun-ling,et al. Magnetostratigraphy of paleogenesediments from northern Qaidam Basin,China:implications for tectonic uplift and block rotation in northern Ti- betan Plateau[J].Earth Planet Sci Lett,2005, 237(3-4):635-646.
[39]张伟林.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:兰州大学资源环境学院, 2006.
[40]FANG Xiao-min,ZHANG Wei-lin,MENG Qing-quan, et al.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,2007,258(1-2):293-306.
[41]DAHLSTROM C D A.Balanced cross section[J]. Canadian Journal of Earth Sciences,1969,6(2): 743 - 759.
[42]ROYDEN L H,BURCHFIEL B C,KING R W,et al. Surface deformation and lower crustal flow in eastern Tibet[J].Science,1997,276:788-790.
[43]万天丰,朱鸿.中国大陆及邻区中生代-新生代大地构造与环境变迁[J].现代地质,2002,16(2): 107-120.
[44]周建勋.同沉积挤压盆地构造演化回复的平衡剖面方法及其应用[J].地球学报,2005,26(2): 151-156.
[45]何维刚.平衡剖面技术计算机模拟[D].成都:成都理工大学信息管理学院,2003.
[46]崔之久,高全洲,刘耕年,等.夷平面、古岩溶与青藏高原隆升[J].中国科学D辑:地球科学,1996, 26(4):378-386.
[47]WANG Cheng-shan,LIU Zhi-fei,YI Hai-sheng, et al.Tertiary crustal shortening and paneplanation in Hohxil region:implications for tectonic history of the northern Tibetan Plateau[J].Asian Earth Sciences, 2002,20:211-223.
[48]吴珍汉,吴中海,胡道功,等.青藏高原腹地中新世早期古大湖的特征及其构造意义[J].地质通报, 2006,25(7):782-791.
[49]吴珍汉,赵逊,叶培盛,等.根据湖相沉积碳氧同位素估算青藏高原古海拔高度[J].地质学报,2007, 81(9):1 277-1 288.
[50]ZHOU Jian-xun,XU Feng-yin,WANG Tie-cheng, et al.Cenozoic deformation history of the Qaidam Basin,NW China:results from cross-section restoration and implications for Qinghai-Tibet Plateau tectonics[J].Earth and Planetary Science Letters,2006,243(1-2):195-210.
[51]YIN An,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):1 257-1295.
[52]FANG Xiao-min,CARMALA G,ROB V D V,et al. Flexural subsidence by 29 Ma on the NE edge of Tibet from the magnetostratigraphy of Linxia Basin,China[J].Earth and Planetary Science Letters, 2003,210(3-4):545-560.
[53]WANG Xiao-ming,WANG Ban-yue,QIU Zhanxiang, et al.Danghe area(western Gansu,China) biostratigraphy and implications for depositional history of northern Tibetan Plateau[J].Earth Planet Sci Lett,2003,208(3-4):253-269.
[54]戴霜,方小敏,宋春晖,等.青藏高原北部的早期隆升[J].科学通报,2005,50(7):673-683.
[55]SCHARER U.The effect of initial ~(230)Th disequilibrium on young U-Pb ages:the Makalu case, Himalaya[J].Earth Planet Sci Lett,1984,67: 191-204.
[56]钟大赉,丁林.青藏高原的隆起过程及其机制探讨[J].中国科学D辑:地球科学,1996,26(4): 289-295.
[57]张进江,丁林.青藏高原东西向伸展及其地质意义[J].地质科学,2003,38(2):179-189.
[58]COLEMAN M,HODGES K.Evidence for Tibetan uplift before 14 Myr ago from a new minimum age for east-west extension[J].Nature,1995,374:49-52.
[59]TUENER A,ARNAUD N,LIU Li,et al.Postcollision, shoshonitic volcanism on the Tibetan Plateau:implications for convective thinning of the lithosphere and the source of ocean island basalts[J]. Journal of Petrology,1996,37(1):45-71.
[60]BLISNIUK P M,HACKER B R,GLODNY J,et al. Normal faulting in central Tibet since at least 13.5 Myr ago[J].Nature,2001,412:628-632.
[61]方小敏,赵志军,李吉均,等.祁连山北缘酒西盆地晚新生代磁性地层与高原隆升[J].中国科学D辑:地球科学,2004,32(2):97-106.
[62]FANG Xiao-min,YAN Mao-du,Voo R V D,et al. Late cenozoic deformation and uplift of the NE Tibetan Plateau:evidence from high-resolution magnetostratigraphy of the Guide Basin,Qinghai Province,China[J].Geol Soc Am Bull,2005,117: 1 208-1 225.
[63]ZHANG Jin-jiang,ZHONG Da-lai,SANG Hai-qing, et al.Structural and geochronological evidence for multiple episodes of tertiary deformation along the Ailaoshan-Red River shear zone,southeastern Asia, since the paleocene[J].ACTA Geologica Sinica, 2006,80:79-96.
[64]METIVIER F,GAUDEMER Y,TAPPONNIER P,et al. Northeasterward growth of the Tibetan Plateau deduced from balanced reconstruc-tion of two depositional areas:the Qaidam and Hexi Corridor Basins, China[J].Tectonics,1998,17(6):823-842.
[65]赵志军,方小敏,李吉均,等.酒泉砾石层的古地磁年代与青藏高原隆升[J].科学通报,2001,46(14): 1208-1212.
[66]李吉均,方小敏,马海洲,等.晚新生代黄河上游地貌演化与青藏高原隆起[J].中国科学D辑:地球科学,1996,26(4):316-322.
[67]赵志军,史正涛,方小敏.祁连山北缘早-中更新世新构造运动的地层记录[J].兰州大学学报:自然科学版,2001,37(6):92-98.
[68]崔之久,伍永秋,刘耕年,等.关于“昆仑-黄河运动”[J].中国科学D辑:地球科学,1998,28(1): 53-59.
[69]MOLNAR P,ENGLAND P,MARTINOD J.Mantle dynamics,uplift of the Tibetan Plateau and the Indian monsoon[J].Reviews of Geophysics,1993, 31(4):357-396.
[70]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].Geophys J Int,1998,135:1-47.
[71]TAPPONNIER P,XU Zhi-qing,ROGE F,et al. Oblique stepwise rise and growth of the Tibet Plateau[J].Science,2001,294:1 671-1677.
[2]MILLER K G,FAIRBANKS R G,MOUNTAIN G S. Tertiary oxygen isotope synthesis,sea level history, and continental margin erosion[J].Paleoceanography, 1987,2(1):1-19.
[3]RAYMO M E,RUDDIMAN W F.Tectonic forcing of late cenozoic climate[J].Nature,1992,359: 117-122.
[4]LI Ji-jun.The environmental effects of the uplift of the Qinghai-Xizang Plateau[J].Quaternary Science Reviews,1991,10(6):478-483.
[5]李吉均,李炳元.青藏高原隆升与全球变化[M].兰州:兰州大学出版社,1995:181-207.
[6]MOLNAR P,CHEN W P.Depths and fault plane solutions of earthquakes under the Tibetan Plateau[J].Geophys Res,1983,88:1 180-1 196.
[7]李吉均,方小敏.青藏高原隆升与环境变化研究[J].科学通报,1998,43(15):1 569-1 574.
[8]READ K,SNOECKX H,JOSEPH L H.Late cenozoic eolian deposition in the north Pacific:Asian drying,Tibetan uplift,and cooling of the northern hemisphere[J].Paleoceanography,1998,13(3): 215-224.
[9]施雅风,汤懋苍,马玉贞.青藏高原二期隆升与亚洲季风孕育关系探讨[J].中国科学D辑:地球科学,1998,28(3):263-271.
[10]安芷生,符淙斌.全球变化科学的进展[J].地球科学进展,2001,16(5):671-680.
[11]KROON D,STEENS T N F,TROELSTRA S R.Onset of monsoonal related upwelling in the western Arabian Sea as revealed by planktonic foraminifers[C]// PRELL W L,NIITSUMA N.Proceedings of the Ocean Drilling Program,Scientific Results.Texas: Ocean Drilling Program,1991:257-264.
[12]徐先海,方小敏,付开道.甘肃临夏盆地8～6 MaBP的构造变化[J].兰州大学学报:自然科学版,2006, 42(6):1-5.
[13]王勇,潘保田,崔明.1.2～0.6 MaBP青藏高原的隆升与东亚地表各圈层的相互作用[J].兰州大学学报:自然科学版,2006,42(3):1-7.
[14]SOOFI M A,KING S D.Oblique convergence between India and Eurasia[J].Geophysical Research, 2002,107(5):ETG3-1-ETG3-8.
[15]JOHNSON M R W.Shortening budgets and the role of continental subduction during the India-Asia collision[J].Earth Science Reviews,2002,59: 101-123.
[16]YIN An,HARRISON T M.Geologic evolution of the Himalaya-Tibetan orogen[J].Annu Rev Earth Planet Sci,2000,28:211-280.
[17]YIN An.Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry,exhumation history, and foreland sedimentation[J].Earth Science Reviews, 2006,76(1-2):1-131.
[18]SHEN Zhen-gang,WANG Min,LI Yan-xing,et al. Crustal deformation along the Altyn Tang fanult system,western China,from GPS[J].Journal of Geophysical Research,2001,106:30 607-30 621.
[19]ZHANG Pei-zhen,SHEN Zheng-kang,WANG Min, et al.Continuous deformation of the Tibetan Plateau from global position system data[J].Geology, 2004,32(9):809-812.
[20]宋廷光.同沉积逆断层的发育特点及油气聚集条件[J].青海地质,1997(2):6-13.
[21]翟光明,徐凤银,李建青.重新认识柴达木盆地、力争油气勘探的新突破[J].石油学报,1997,18(2): 1-7.
[22]陈世悦,徐凤银,彭德华.柴达木盆地基底构造特征及其控油意义[J].新疆石油地质,2000,21(3): 1-7.
[23]尚尔杰.柴达木盆地北缘西段第三系构造基本样式及石油地质意义[J].现代地质,2001,15(4): 421-424.
[24]王信国,曹代勇,占文锋,等.柴达木盆地北缘中、新生代盆地性质及构造演化[J].现代地质,2006, 20(4):592-596.
[25]范连顺,王明儒.柴达木盆地茫崖坳陷含油气系统及勘探方向[J].石油实验地质,1999,21(1): 41-47.
[26]汤良杰,金之钧,张明利,等.柴达木盆地北缘构造演化与油气成藏阶段[J].石油勘探与开发,2000, 27(2):36-39.
[27]XIA Wen-cheng,ZHANG Ning,YUAN Xiao-ping, et al.Cenozoic Qaidam Basin,China:a stronger tectonic inversed,extensional rifted basin[J].AAPG Bulletin,2001,85(4):715-736.
[28]王成善,朱利东,刘志飞.青藏高原北部盆地构造沉积演化与高原向北生长过程[J].地球科学进展, 2004,19(3):373-381.
[29]ZHU Li-dong,WANG Cheng-shan,ZHENG Hong-bo, et al.Tectonic and sedimentary evolution of basins in the northeast of Qinghai-Tibet Plateau and their implication for the northward growth of the Plateau[J].Palaeogeography Palaeoclimateology Palaeoecology,2006,241:49-60.
[30]王桂宏,谭彦虎,陈新领,等.新生代柴达木盆地构造演化与油气勘探领域[J].中国石油勘探, 2006(1):80-84.
[31]王步清.柴达木盆地新生代构造演化与沉积特征[J].新疆石油地质,2006,27(6):670-672.
[32]吴光大,葛肖虹,刘永江,等.柴达木盆地中、新生代构造演化及其对油气的控制[J].世界地质,2006, 25(4):411-417.
[33]杨藩,马志强,许同春,等.柴达木盆地第三纪磁性地层柱[J].石油学报,1992,13(2):97-101.
[34]刘泽纯,孙世英,杨藩,等.柴达木盆地三湖地区第四纪地层学和其年代学分析[J].中国科学B辑:化学,1990,20(11):1 202-1 212.
[35]刘泽纯,范连顺.柴达木盆地茫崖凹陷井下第三系的年代地层学与气候地层学研究[J].地层学杂志, 1996,20(2):104-113.
[36]孙知明,杨振宇,葛肖虹,等.柴达木盆地西北缘古近系磁性年代研究进展[J].地质通报,2004, 23(9/10):899-902.
[37]LIU Ze-chun,WANG Yong-jin,CHEN Yan-an,et al. Magnetostrigraphy and sedimentologically derived geochronology of the quaternary lacustrine deposits of a 3 000 m thick sequence in the central Qaidam Basin,western China[J].Palaeogeography Palaeoclimatology Palaeoecology,1998,140(1-4): 459-473.
[38]SUN Zhi-ming,YANG Zhen-yu,PEI Jun-ling,et al. Magnetostratigraphy of paleogenesediments from northern Qaidam Basin,China:implications for tectonic uplift and block rotation in northern Ti- betan Plateau[J].Earth Planet Sci Lett,2005, 237(3-4):635-646.
[39]张伟林.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:兰州大学资源环境学院, 2006.
[40]FANG Xiao-min,ZHANG Wei-lin,MENG Qing-quan, et al.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,2007,258(1-2):293-306.
[41]DAHLSTROM C D A.Balanced cross section[J]. Canadian Journal of Earth Sciences,1969,6(2): 743 - 759.
[42]ROYDEN L H,BURCHFIEL B C,KING R W,et al. Surface deformation and lower crustal flow in eastern Tibet[J].Science,1997,276:788-790.
[43]万天丰,朱鸿.中国大陆及邻区中生代-新生代大地构造与环境变迁[J].现代地质,2002,16(2): 107-120.
[44]周建勋.同沉积挤压盆地构造演化回复的平衡剖面方法及其应用[J].地球学报,2005,26(2): 151-156.
[45]何维刚.平衡剖面技术计算机模拟[D].成都:成都理工大学信息管理学院,2003.
[46]崔之久,高全洲,刘耕年,等.夷平面、古岩溶与青藏高原隆升[J].中国科学D辑:地球科学,1996, 26(4):378-386.
[47]WANG Cheng-shan,LIU Zhi-fei,YI Hai-sheng, et al.Tertiary crustal shortening and paneplanation in Hohxil region:implications for tectonic history of the northern Tibetan Plateau[J].Asian Earth Sciences, 2002,20:211-223.
[48]吴珍汉,吴中海,胡道功,等.青藏高原腹地中新世早期古大湖的特征及其构造意义[J].地质通报, 2006,25(7):782-791.
[49]吴珍汉,赵逊,叶培盛,等.根据湖相沉积碳氧同位素估算青藏高原古海拔高度[J].地质学报,2007, 81(9):1 277-1 288.
[50]ZHOU Jian-xun,XU Feng-yin,WANG Tie-cheng, et al.Cenozoic deformation history of the Qaidam Basin,NW China:results from cross-section restoration and implications for Qinghai-Tibet Plateau tectonics[J].Earth and Planetary Science Letters,2006,243(1-2):195-210.
[51]YIN An,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):1 257-1295.
[52]FANG Xiao-min,CARMALA G,ROB V D V,et al. Flexural subsidence by 29 Ma on the NE edge of Tibet from the magnetostratigraphy of Linxia Basin,China[J].Earth and Planetary Science Letters, 2003,210(3-4):545-560.
[53]WANG Xiao-ming,WANG Ban-yue,QIU Zhanxiang, et al.Danghe area(western Gansu,China) biostratigraphy and implications for depositional history of northern Tibetan Plateau[J].Earth Planet Sci Lett,2003,208(3-4):253-269.
[54]戴霜,方小敏,宋春晖,等.青藏高原北部的早期隆升[J].科学通报,2005,50(7):673-683.
[55]SCHARER U.The effect of initial ~(230)Th disequilibrium on young U-Pb ages:the Makalu case, Himalaya[J].Earth Planet Sci Lett,1984,67: 191-204.
[56]钟大赉,丁林.青藏高原的隆起过程及其机制探讨[J].中国科学D辑:地球科学,1996,26(4): 289-295.
[57]张进江,丁林.青藏高原东西向伸展及其地质意义[J].地质科学,2003,38(2):179-189.
[58]COLEMAN M,HODGES K.Evidence for Tibetan uplift before 14 Myr ago from a new minimum age for east-west extension[J].Nature,1995,374:49-52.
[59]TUENER A,ARNAUD N,LIU Li,et al.Postcollision, shoshonitic volcanism on the Tibetan Plateau:implications for convective thinning of the lithosphere and the source of ocean island basalts[J]. Journal of Petrology,1996,37(1):45-71.
[60]BLISNIUK P M,HACKER B R,GLODNY J,et al. Normal faulting in central Tibet since at least 13.5 Myr ago[J].Nature,2001,412:628-632.
[61]方小敏,赵志军,李吉均,等.祁连山北缘酒西盆地晚新生代磁性地层与高原隆升[J].中国科学D辑:地球科学,2004,32(2):97-106.
[62]FANG Xiao-min,YAN Mao-du,Voo R V D,et al. Late cenozoic deformation and uplift of the NE Tibetan Plateau:evidence from high-resolution magnetostratigraphy of the Guide Basin,Qinghai Province,China[J].Geol Soc Am Bull,2005,117: 1 208-1 225.
[63]ZHANG Jin-jiang,ZHONG Da-lai,SANG Hai-qing, et al.Structural and geochronological evidence for multiple episodes of tertiary deformation along the Ailaoshan-Red River shear zone,southeastern Asia, since the paleocene[J].ACTA Geologica Sinica, 2006,80:79-96.
[64]METIVIER F,GAUDEMER Y,TAPPONNIER P,et al. Northeasterward growth of the Tibetan Plateau deduced from balanced reconstruc-tion of two depositional areas:the Qaidam and Hexi Corridor Basins, China[J].Tectonics,1998,17(6):823-842.
[65]赵志军,方小敏,李吉均,等.酒泉砾石层的古地磁年代与青藏高原隆升[J].科学通报,2001,46(14): 1208-1212.
[66]李吉均,方小敏,马海洲,等.晚新生代黄河上游地貌演化与青藏高原隆起[J].中国科学D辑:地球科学,1996,26(4):316-322.
[67]赵志军,史正涛,方小敏.祁连山北缘早-中更新世新构造运动的地层记录[J].兰州大学学报:自然科学版,2001,37(6):92-98.
[68]崔之久,伍永秋,刘耕年,等.关于“昆仑-黄河运动”[J].中国科学D辑:地球科学,1998,28(1): 53-59.
[69]MOLNAR P,ENGLAND P,MARTINOD J.Mantle dynamics,uplift of the Tibetan Plateau and the Indian monsoon[J].Reviews of Geophysics,1993, 31(4):357-396.
[70]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].Geophys J Int,1998,135:1-47.
[71]TAPPONNIER P,XU Zhi-qing,ROGE F,et al. Oblique stepwise rise and growth of the Tibet Plateau[J].Science,2001,294:1 671-1677.
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