青藏高原东北缘六盘山—马东山地区晚新生代构造变形综合研究
|
摘要
青藏高原东北缘地区是晚新生代以来高原隆升并向北持续扩展的最新变形前缘地带,形成了特有的“盆-山”地貌格局和环境演化,大规模陆内逆冲-褶皱造山系的强烈隆升,相关盆地东西向串珠排列,环境的变化也反映在沉积物的变化上,从东部的六盘山,沿着祁连、河西走廊、昆仑一直到中国西部的天山,第三系的红层沉积是高原北部特有现象。因此,青藏高原东北缘因其所处的构造位置而成为解决青藏高原隆升和周边造山带造山过程的关键地区。
青藏高原东北缘位于海原断裂带东段的六盘山-马东山地区属于中新生代典型挤压逆冲造山带,相关盆山构造变形历史具有连续变形和周期性脉动的特征,中新世以来该造山带前缘寺口子盆地和后缘隆德盆地为典型前陆盆地,造山作用过程和盆地沉积演化具有盆山耦合特征,盆地中地层层序齐全,沉积了巨厚的陆相沉积物,保存着大量的高原隆升远程效应、陆内碰撞造山过程以及构造变形的大量信息,通过这些记录使得我们可以揭示、反演出构造变形历史,探索构造变形空间迁移和不同构造之间的转换平衡关系,重塑青藏高原东北缘变形和隆升历史,详细探讨该区在整个青藏高原在向北扩展过程中造山带和盆地之间动力学过程。通过对六盘山-马东山地区造山带和相关盆地区域地质背景、沉积学特征、磁性地层、生物地层、沉积相和构造层序及构造变形序列和样式的综合分析,系统探讨了研究区盆山演化的动力学过程,主要获得的以下认识:
六盘山-马东山逆冲褶皱造山带的前缘和后缘分布着不同类型的盆地,寺口子盆地沉积特征表明它是该造山带前缘的一个典型前陆盆地,而六盘山后缘隆德盆地在第三纪时期是一个逆冲挤压走滑性质盆地,二者尽管在成因上有所不同,但是其沉积特征具有非常类似的特征,属于同一造山带上的不同产物。
寺口子剖面地层出露齐全,因此本文将寺口子剖面作为研究的重点,并系统采集了古地磁样品,对其进行了详细的磁性地层分析,寺口子剖面沉积主要属于中新世以来的新生代沉积,地质时代由老至新进行重新划分和标定,由老至新依次为寺口子组划归为早中新世沉积(N_1~1),其顶界年龄与清水营组底界约有1.53Ma沉积间断,底界年龄大约为18.02Ma;清水营组划归为中中新世沉积(N_1~2),地质时代在10.97-14.9Ma之间;红柳沟组属于晚中新世沉积(N_1~3),时代间隔为5.28-10.97Ma;马家庄组为早上新世沉积(N_2~1),沉积时代为3.60-5.25Ma之间;干河沟组为晚上新世沉积(N_2~2),地质时代为1.77-3.60Ma之间;老庄组相当于更新世沉积(Q_1),沉积时代大约在0.2-1.77Ma之间。上述划分与早期划分差别较大,在六盘山-马东山地区早期可能并不存在始新世和渐新世沉积,可能原因是早期高原隆升并向北扩展效应导致该区遭受逆冲挤压造山作用使山体抬升出现沉积间断而导致始新世和渐新世沉积地层缺失。
隆德盆地是六盘山-马东山褶皱逆冲造山带后缘典型盆地,其沉积特征和岩石地层与前缘盆地寺口子盆地具有十分类似的特征,隆德剖面中寺口子组大致相当于早中新世沉积(N_1~1),清水营组的沉积时代大致相当于中中新世(N_1~2),红柳沟组相当于晚中新世(N_1~3)的沉积,顶界年龄不会晚于8Ma。根据区域地层对比,本文海原地区的清水营组、红柳沟组和干河沟组在年代学确定和分析上与寺口子盆地和隆德盆地是完全不同的概念,其时代主要限制在渐新世-中新世之间,其间缺失了晚中新世-更新世之间的地层,直到第四纪时期才开始继续接受沉积,结合贺家口子磁性地层结果,由南西向北东较老地层保存逐渐完整,
The northeastern margin of the Tibetan plateau is the frontier of the northeastward expanding Tibetan plateau since the late Cenozoic. This region is characterized by a structural pattern of“basin and range”which was formed during the uplifting and outward expanding process of the Tibetan plateau in the late Cenozoic era. Mountains controlled by fold and thrust belts uplift strongly, and separate the widespread Cenozoic basin into many smaller basins with thick Cenozoic deposits. The Cenozoic stratum of the northeastern Tibetan Plateau is spectacular, distributed from the Liupanshan, via the Hexi corridor, Qilianshan and Qaidam, to the Tianshan. Since the Oligocene all these areas are characterized by thick, nearly continually deposited layers. The Cenozoic layers not only record the environment change, but preserve detailed information about the Cenozoic tectonic deformation also. Therefore, the northeastern Tibetan Plateau is an ideal region for the resolution of problems, such as the uplifting history of the Tibetan Plateau.
The Liupanshan-Madongshan, which is located on the eastern segment of the Haiyuan fault zone is a typical Mesozoic and Cenozoic compressive thrust mountain belt. The correlative sedimentary and orogenic evolvement have the character of continous deformation and periodic pulsatory mountain-building in the basin-and-range coupling system,To the north, the Sikouzi basin is a typical foreland basin and the trailing-edge Longde bansin is a representative basin with thrusting and strike-slipping since the Miocene. The development of these basins is coupled with the uplifting of the surrounding mountains. The basins are filled with thick terrigenous deposits which record detailed information about the uplifting of the Tibetan plateau, intracontinental collision and relevant Cenozoic deformation. Deciphering of these records will help illuminate the history of Cenozoic deformation, migration of deformation, relationships among different structures, and the histories of deformation and uplifting of the whole northeastern margin of the Tibetan plateau.
Based on integrated analyses of the regional geologic setting, depositional characteristics, paleomagneto-stratigraphy, bio-stratigraphy, sedimentary facies, tectonic sequences, and sequences and styles of the Cenozoic deformation, many interesting results are obtained, and the evolution process of the mountains and basins of the studied region are discussed. Main results of this thesis are summarized below:
Different types of basins developed in the front of and behind the Liupanshan-Mandongshan fold and thrust mountain belt. The Sikouzi basin in front of the mountain is a typical foreland basin, while the Longde basin, which lies at the back of the Liupanshan, is a compressive, strike-slip related basin.
The Sikouzi section is emphasized in this study. Along this section systematic paleo-magnetic samples are collected and analyzed. The results show that most of the layers were deposited since the Miocene. According to the paleomagnetic ages, formations on this section are divided and calibrated, and six formations are recognized. The lowest Sikouzi formation is the early Miocene(N_1~1)with the bottom age of 18.02 Ma, and there is a 1.53Ma disruption of the deposition
青藏高原东北缘位于海原断裂带东段的六盘山-马东山地区属于中新生代典型挤压逆冲造山带,相关盆山构造变形历史具有连续变形和周期性脉动的特征,中新世以来该造山带前缘寺口子盆地和后缘隆德盆地为典型前陆盆地,造山作用过程和盆地沉积演化具有盆山耦合特征,盆地中地层层序齐全,沉积了巨厚的陆相沉积物,保存着大量的高原隆升远程效应、陆内碰撞造山过程以及构造变形的大量信息,通过这些记录使得我们可以揭示、反演出构造变形历史,探索构造变形空间迁移和不同构造之间的转换平衡关系,重塑青藏高原东北缘变形和隆升历史,详细探讨该区在整个青藏高原在向北扩展过程中造山带和盆地之间动力学过程。通过对六盘山-马东山地区造山带和相关盆地区域地质背景、沉积学特征、磁性地层、生物地层、沉积相和构造层序及构造变形序列和样式的综合分析,系统探讨了研究区盆山演化的动力学过程,主要获得的以下认识:
六盘山-马东山逆冲褶皱造山带的前缘和后缘分布着不同类型的盆地,寺口子盆地沉积特征表明它是该造山带前缘的一个典型前陆盆地,而六盘山后缘隆德盆地在第三纪时期是一个逆冲挤压走滑性质盆地,二者尽管在成因上有所不同,但是其沉积特征具有非常类似的特征,属于同一造山带上的不同产物。
寺口子剖面地层出露齐全,因此本文将寺口子剖面作为研究的重点,并系统采集了古地磁样品,对其进行了详细的磁性地层分析,寺口子剖面沉积主要属于中新世以来的新生代沉积,地质时代由老至新进行重新划分和标定,由老至新依次为寺口子组划归为早中新世沉积(N_1~1),其顶界年龄与清水营组底界约有1.53Ma沉积间断,底界年龄大约为18.02Ma;清水营组划归为中中新世沉积(N_1~2),地质时代在10.97-14.9Ma之间;红柳沟组属于晚中新世沉积(N_1~3),时代间隔为5.28-10.97Ma;马家庄组为早上新世沉积(N_2~1),沉积时代为3.60-5.25Ma之间;干河沟组为晚上新世沉积(N_2~2),地质时代为1.77-3.60Ma之间;老庄组相当于更新世沉积(Q_1),沉积时代大约在0.2-1.77Ma之间。上述划分与早期划分差别较大,在六盘山-马东山地区早期可能并不存在始新世和渐新世沉积,可能原因是早期高原隆升并向北扩展效应导致该区遭受逆冲挤压造山作用使山体抬升出现沉积间断而导致始新世和渐新世沉积地层缺失。
隆德盆地是六盘山-马东山褶皱逆冲造山带后缘典型盆地,其沉积特征和岩石地层与前缘盆地寺口子盆地具有十分类似的特征,隆德剖面中寺口子组大致相当于早中新世沉积(N_1~1),清水营组的沉积时代大致相当于中中新世(N_1~2),红柳沟组相当于晚中新世(N_1~3)的沉积,顶界年龄不会晚于8Ma。根据区域地层对比,本文海原地区的清水营组、红柳沟组和干河沟组在年代学确定和分析上与寺口子盆地和隆德盆地是完全不同的概念,其时代主要限制在渐新世-中新世之间,其间缺失了晚中新世-更新世之间的地层,直到第四纪时期才开始继续接受沉积,结合贺家口子磁性地层结果,由南西向北东较老地层保存逐渐完整,
The northeastern margin of the Tibetan plateau is the frontier of the northeastward expanding Tibetan plateau since the late Cenozoic. This region is characterized by a structural pattern of“basin and range”which was formed during the uplifting and outward expanding process of the Tibetan plateau in the late Cenozoic era. Mountains controlled by fold and thrust belts uplift strongly, and separate the widespread Cenozoic basin into many smaller basins with thick Cenozoic deposits. The Cenozoic stratum of the northeastern Tibetan Plateau is spectacular, distributed from the Liupanshan, via the Hexi corridor, Qilianshan and Qaidam, to the Tianshan. Since the Oligocene all these areas are characterized by thick, nearly continually deposited layers. The Cenozoic layers not only record the environment change, but preserve detailed information about the Cenozoic tectonic deformation also. Therefore, the northeastern Tibetan Plateau is an ideal region for the resolution of problems, such as the uplifting history of the Tibetan Plateau.
The Liupanshan-Madongshan, which is located on the eastern segment of the Haiyuan fault zone is a typical Mesozoic and Cenozoic compressive thrust mountain belt. The correlative sedimentary and orogenic evolvement have the character of continous deformation and periodic pulsatory mountain-building in the basin-and-range coupling system,To the north, the Sikouzi basin is a typical foreland basin and the trailing-edge Longde bansin is a representative basin with thrusting and strike-slipping since the Miocene. The development of these basins is coupled with the uplifting of the surrounding mountains. The basins are filled with thick terrigenous deposits which record detailed information about the uplifting of the Tibetan plateau, intracontinental collision and relevant Cenozoic deformation. Deciphering of these records will help illuminate the history of Cenozoic deformation, migration of deformation, relationships among different structures, and the histories of deformation and uplifting of the whole northeastern margin of the Tibetan plateau.
Based on integrated analyses of the regional geologic setting, depositional characteristics, paleomagneto-stratigraphy, bio-stratigraphy, sedimentary facies, tectonic sequences, and sequences and styles of the Cenozoic deformation, many interesting results are obtained, and the evolution process of the mountains and basins of the studied region are discussed. Main results of this thesis are summarized below:
Different types of basins developed in the front of and behind the Liupanshan-Mandongshan fold and thrust mountain belt. The Sikouzi basin in front of the mountain is a typical foreland basin, while the Longde basin, which lies at the back of the Liupanshan, is a compressive, strike-slip related basin.
The Sikouzi section is emphasized in this study. Along this section systematic paleo-magnetic samples are collected and analyzed. The results show that most of the layers were deposited since the Miocene. According to the paleomagnetic ages, formations on this section are divided and calibrated, and six formations are recognized. The lowest Sikouzi formation is the early Miocene(N_1~1)with the bottom age of 18.02 Ma, and there is a 1.53Ma disruption of the deposition
引文
Abascal L.V. 2005. Combined thin-skinned and thick-skinned deformation in the central Andean foreland of northwestern Argentina. Journal of South American Earth Sciences, 19(1): 75-81
An Zhisheng, Kutzbach J. E., Prell W. L., et al. 2001. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibet plateau since late Miocene times. Nature, 411: 62-66
Arne D., Worley B., Wilson C., et al. 1997. Differential exhumation in response to episodic thrusting along the eastern margin of the Tibetan Plateau. Tectonophysics, 280: 239-256
Baker D.M., Robert J.L., Johnson G.D., et al. 1988. Development of the Himalayan frontal thrust zone: Salt Range, Pakistan. Geology, 16: 3-7
Beck R.A., Burbank D.W., Sercombe W.J., et al. 1995. Stratigraphic evidence for an early collision between northwest India and Asia. Nature, 373: 55-57
Bookhagen B., Thiede R.C. and Strecker M.R. 2005. Abnormal monsoon years and their control on erosion and sediment flux in the high, arid northwest Himalaya. Earth and Planetary Science Letters, 108:1-11
Bullen M.E. 2003. Late Cenozoic tectonic evolution of the Kyrgyz Range and adjoining Chu Basin: New age constraints from fission-track, U-Th/He, and magnetostratigraphy. The Paper of Master of Science, 1-55
Bullen M.E., Burbank D.W., and Garver J.I., et al. 2003. Building the northern Tien Shan: Integrated thermal, structural, and topographic constraints. J. Geol., 111: 149-165
Burbank D.W. 1992. Cause of recent Himalayan uplift deduced from deposited patterns in the Ganges basin. Nature, 357: 680-683
Burbank D.W., McLean J.K., Bullen M.E., et al. 1999. Partitioning of intermontane basins by thrust-related folding, Tien Shan, Kyrgyzstan. Basin Research , 11: 75-92
Burbank D.W., Richard A.B., Thomas M., et al. 1996. The Himalayan foreland basin. In: An Yin, Mark Harrison, ed. The Tectonic Evolution of Aisa, 149-188
Burchfiel B. C., Chen Z., Liu Y., et al.1997. Tectonics of the Longmen Shan and adjacent regions, central China, Intern. Geological Review, 37(8): 661~735.
Burchfiel B.C., Deng Q., Molnar P., et al. 1989. Intracrustal detachment zones of continental deformation. Geology, 17: 448-452
Burchfiel B.C., Zhang P., Wang Y., et al. 1991. Geology of Haiyuan fault zone, Ningxia-Hui Autonomous Region, China, and its relation to the evolution of the northeastern margin of the Tibetan plateau, Tectonics, 10: 1091-1110
Calabro R.A., Corrado S., Di Bucci D., et al. 2003. Thin-skinned vs. thick-skinned tectonics in the Matese Massif, Central–Southern Apennines (Italy). Tectonophysics, 377(3-4): 269-297
Cande S. C. and kent D. V. 1995. Revised calibration of geomagnetic polaryity time scale for the late Creaceous and Cenozoic.J.G.R., 100: 6093-6095
Catuneanu O. 2004. Retroarc foreland systems––evolution through time. Journal of African Earth Sciences, 38(3): 225-242
Chen Jie, Burbank D.W., Scharer K.M., et al. 2002. Magnetochronology of the upper Cenozoic strata in the Southwestern Chinese Tian Shan: rates of Pleistocene folding and thrusting. Earth and Planetary Science Letters, 195: 113-130
Chen Jie, Lu Yanchou, Ding Guoyu.1998.Quaternary tectonic deformation in Jiuxi Basin, west Qilianshan Mountain, northwestern China. Journal of Earthquake Prediction Research, (7):510~522
Chen Yan, Wu Hanning, Courtillot V., et al. 2002. Large N–S convergence at the northern edge of the Tibetan plateau? New Early Cretaceous paleomagnetic data from Hexi Corridor, NW China. J. Earth and Planetary Science Letters, 201(2): 293-307
Coleman M, Hodges K. 1995. Evidence for Tibetan Plateau uplift before 14Myr ago from a new minimum age for east-west extension. Nature, 374:49-52
Currie B. 1997. Sequence stratigraphy of nonmarine Hurassic-Cretaceous rocks, central Cordilleran foreland basin system. GSA Bulletin, 109(9): 1206-1222
Dahlen F.A. 1990. Critical taper model of fold-and-thrust belts and accretionary wedges. Annual Review of Earth and Planetary Sciences, 18: 55-99
Darby B. J., Ritts B. D., Yue Yongjun, et al. 2005. Did the Altyn Tagh fault extend beyond the Tibetan Plateau? Earth and Planetary Science Letters, 240(2): 425-435
Decelles P.D., Gehrels G.E., Quade J., et al. 1998. Neogene foreland basin deposits, erosional unroofing, and the kinematic history of the Himalayan fold-thrust belt, western Nepal. Geol. Soc. Ame. Bulletin, 1:2-21
DeCelles P.G. and Giles P.A. 1996. Foreland basin systems. Basin Res., 8: 105-123
DeCells P.G. 1994. Late Cretaceous-Paleocene synorogenic sedimentation and kinematic history of the Sevier thrust belt, northeast Utah and southwest Wyoming. GSA Bulletin, 106: 32-56
DeCells P.G. and Currie B.S. 1996. Long-term sediment accumulation in the Middle Jurassic-Early Eocene Cordilleran retroarc foreland-basin system. Geology, 24(7):591-594
DeCells P.G.. and Gehrels G.E. 1998. Eocene-Early Miocene foreland basin development and the history of Himalayan thrusting western and central Nepal. Tectonics, 17(5): 741-765
DeCells P.G.. and Giles K.A. 1996. Foreland basin systems. Basin Research, 8: 105-123
DeCells P.G.., Mitra G. 1995. History of the Sevier orogenic wedge interns of critical taper models, northeast Utah and southwest Wyoming. Geological Society of America Bulletin, 107: 454-462
Dettman, D.L. Fang, X., Garzione, C.N., et al. 2003. Uplift-driven climate change at 12Ma: a long δ18O record from the NE margin of the Tibetan plateau. Earth Planet. Sci. Lett., 214:267-277
Dewey J. F. 1988. Extensional collapse of orogens. Tectonics, 7(6): 1123-1139
Dewey J. F. and Burke K.C. 1973. Tibetan, Variscan and Precambrian basement reactivation:Products of continental collision, Journal of Geology, 81:683-692
Dewey J. F., Holdsworth R. E., Strachan R.A. 1998. Transpression and transtension zones. In:Holdsworth,R.E., Strachan,R.A. and Deway, J. F. (eds) 1998. Continental teanspressional and transtensional tectonics. Geological Society, London, Special Publications, 135:15-33
Dewey J.F., Shackleton R.M.,常承法,等. 1990. 青藏高原的构造演化. 青藏高原地质演化, 北京: 科学出版社, 384-415
Dupont-Nivet G., Butler R.F., Yin A., et al. 2002. Paleomagnetism indicates no Neocene rotation of the Qaidam Basin in northern Tibet during Indo-Asian collision, Geology, 30(3): 263-266
Dupont-Nivet G., Horton B.K., Butler R.F., et al. 2004. Paleogene clockwise tectonicrotation of the Xining -Lanzhou region, Northeastern Tibetan Plateau, J. Geophys. Res., 109(B04401): 1-13
Eji Uba C., Heubeck C.and Hulka C. 2005. Facies analysis and basin architecture of the Neogene Subandean synorogenic wedge, southern Bolivia. Sedimentary Geology, 180(3-4): 91-123
England P. and Molnar P. 1990. Right-lateral shear and rotation as explanation for strike-slip fauting in eastern Tibet. Nature, 1990, 344(6262): 140-142
England P. and Molnar P. 1997. The field of crustal velocity in Asia calculated from Quaternary rates of slip on faults. Geophys. J. Int., 130: 551-582
England P. and Molnar. P. 1990. Surface uplift, uplift of rocks, and exhumation of rocks. Geology, 18: 1173-1177
England P.C. and G.A.Houseman. 1985. Role of lithospheric strength heterogeneities in the tectonics of Tibet and neighbouring regions. Nature, 315(6017): 297-301
England P.C. and G.A.Houseman. 1988. The mechnics of the Tibetan Plateau, Phil. Trans. R. Soc. Lond. A., 326: 301-320
Fang Xiaomin, Carmala G., Van der V.R., et al. 2003. Flexural subsidence by 29 Ma on the NE edge of Tibet from the magnetostratigraphy of Linxia Basin, China. Earth and Planetary Science Letters, 210: 545-560
Fang, X. M., Yan M.D., Van der Voo R., et al., 2005. Late Cenozoic deformation and uplift of the NE Tibetan Plateau: evidence from high-resolution magnetostratigraphy of the Guide Basin, Qinghai Province, China. Geol. Soc. Am. Bull., 117:1208-1225
Fisher R.A. 1953. Dispersion on a sphere. Proc R Soc London, Ser A, 217: 295-305
Flesch L.M., Haines A.J., Holt W.E. 2003. Dynamics of the India-Eurasia collision zone. J. Geophys. Res., 106: 16435-16460
Fu Bihong, Awata Y., Du Jianguo, et al. 2005. Late Quaternary systematic stream offsets caused by repeated large seismic events along the Kunlun fault, northern Tibet. Geomorphology, 71(3-4): 278-292
Gao Cunhai. 2004. Sedimentary facies changes and climatic-tectonic controls in a foreland basin, the Urumqi River, Tian Shan, Northwest China. Sedimentary Geology, 169(1-2): 29-46
Garzione C.N., Dettaman D.L., Quade J., et al. 2000. high times on the Tibetan plateau: paleoelevation of the Thakkhola garben, Nebal. Geology, 28(4): 339-342
Gaudemer Y., Tapponnier P., Meyer B., et al. 1995. Partitioning of crustal slip between linked, active faults in the eastern Qilian Shan, and evidence for a major seismic gap, The ‘Tianzhu gap’, on the western Haiyuan Fault, Gansu(China). Geophys. J. Int., 120: 599-645
Gautam P. and Rosler W. 1999. Depositional chronology and fabric of Siwalik group sediments in Central Nepal from magnetostratigraphy and magnetic anisotropy. Journal of Asian Earth Sciences, 17(5-6): 659-682
George A.D., Marshallsea S.J., Wyrwoll K.H., et al. 2001. Miocene cooling in the northern Qilian Shan, northeastern margin of the Tibetan Plateau, revealed by apatite fission-track and vitrinite-reflectance analysis. Geology, 29: 939-942
Ghiglione M.C. and Ramos V.A. 2005. Progression of deformation and sedimentation in the southernmost Andes. Tectonophysics, 405(1-4): 25-46
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. G. R., 106(B12): 30505-30521
Golonka J. 2004. Plate tectonic evolution of the southern margin of Eurasia in the Mesozoic and Cenozoic. Tectonophysics, 381(1-4): 235-273
Gonzalez-Bonorino G. and Kraemer G.P. 2001. Andean Cenozoic foreland basins: a review. Journal of South American Earth Sciences, 14(7): 651-654
Greb S.F., Eble C. F. and Chesnut D. R. 2002. Comparison of the Eastern and Western Kentucky coal fields (Pennsylvanian), USA—why are coal distribution patterns and sulfur contents so different in these coal fields? International Journal of Coal Geology, 50(1-4): 89-118
Halim N., Cogne J.P., Chen Y., et al. 1998. New cretaceous and Early Tertiary Paleomagnetic results from xining-lanzhou basin, Kunlun and Qiangtang Blocks, China: Implications on the Geodynamic evolution of Asia. J. G. R., 103(B9): 21025-21045
Harrison T. M., Lovera O. M., Grove M. 1997. New insights into the origin of two contrasting Himalayan granite belts. Geology, 25(10):899-902
Harrison T.M., Yin A., Grove M. et al. 2000. The Zedong Window: A record of superposed Tertiary convergence in southeastern Tibet, JGR, 105(B8):19211-19230
Harrison, T.M., Copeland P., Kidd W.S.F., et al. 1992. Raising Tibet. Science, 255: 1663-1670
Hendrix M.S., Dumitru T.A., Graham S. A. 1994. Late Oligocene-early Miocene uprooting in the Chinese Tian Shan : An early effect of the India-Asia collision. Geology, 22: 487-490
Holt W.E., Chamot-Rooke N., Le Pichon X., et al. 2000. Velocity field in Aisa inferred from Quaternary fault slip rates and Global Positioning System observations. J. Geophys. Res., 105: 19185-19209
Homewood P., Allen P.A., Williams G.D. 1986. Foreland basins: An introduction. In: Allen P.A., Homewood P. ed. Foreland basin. International Association of Sedimentologists Special Publication 8, 3-12
Horton B.K., Dupont-Nivet J., Zhou G..L., et al. 2004. Mesozoic-Cenozoic evolution of the Xining, Minhe and Dangchang basins, northeastern Tibetan Plateau: Magnetostratigraphic and biostratigraphic results. Journal of Geophysical Research, 109(B04402): 1-15
Houseman G. and England P. 1993. Crustal thickening versus lateral expulsion in the India-Asian continental collision. J. Geophys. Res., 98: 12233-12249
Huang B. C., Wang Y. C., Liu T., et al. 2004. Paleomagnetism of Miocene sediments from the Turfan Basin, Northwest China: no significant vertical-axis rotation during Neotectonic compression within the Tian Shan Range, Central Asia. Tectonophysics, 384(1-4): 1-21
Jackson J. 2003. Strength of the continental lithosphere: time to abandon the jelly sandwich? GSA Today, 12(9): 4-10
Jain V. and Sinha R. 2004. Fluvial dynamics of an anabranching river system in Himalayan foreland basin, Baghmati river, north Bihar plains, India. Geomorphology, 60(1-2): 147-170
Jiang M., Galve A., Hirn A., et al. 2006. Crustal thickening and variations in architecture from the Qaidam basin to the Qang Tang (North–Central Tibetan Plateau) from wide-angle reflection seismology. Tectonophysics, 412(3-4): 121-140
Johnson N.M., Opdyke N.J., Johnson G.D., et al. 1982. Magnetic polarity stratigraphy and ages of Siwalik Group rocks of the Potwar Plateau, Pakistan. Palaeogeography, Palaeoclimatology, Palaeoecology, 37:17-42
Jolivet J., Brunel M., Seward D., et al. 2001. Mesozoic and Cenzoic tectonics of the northern edge of the Tibetan plateau: fission-track constraints. Tectonophysics, 343: 111-134
Jolivet M., Brunel M., Seward D., et al. 2001. Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan plateau: fission-track constraints. Tectonophysics, 343(1-2): 111-134
Jordan T.A. and Watts A.B. 2005. Gravity anomalies, flexure and the elastic thickness structure of the India–Eurasia collisional system. Earth and Planetary Science Letters, 236(3-4): 732-750
Kimura H., Azmy K., Yamamuro M., et al. 2005. Integrated stratigraphy of the upper Neoproterozoic succession in Yunnan Province of South China: Re-evaluation of global correlation and carbon cycle. Precambrian Research, 138(1-2): 1-36
Kirby E., Whipple K.X., Tang W.,et al. 2003. Distribution of active rock uplift along the eastern margin of the Tibetan Plateau: Inferences from bedrock channel longitudinal profiles. J.Geophys.Res., 108(B4):2217, doi: 10.1029/2001JB000861
Kirschvink J.L. 1980. The least-squares line and plane and the analysis of paleomagnetic data. Geophys J R Astron Soc, 62: 699-718
Kletetschka G. and Wasilewski P.J. 2002. Grain size limit for SD hematite. Physics of The Earth and Planetary Interiors, 129(1-2): 173-179
Koroteev V.A., Necheukhin, V.M. and Sazonov, V.N. 1997. Geodynamic setting of the mineral deposits of the Urals. Tectonophysics. 276(1-4): 291-300
Krishna K. S., Bull J. M., Scrutton R.A. 2001. Evidence for multiphase folding of the central Indian Ocean lithosphere. Geology, 29(8):715-718
Kumaravel V., Sangode S.J., Siddaiah N.S., et al. 2005. Rock magnetic characterization of pedogenesis under high energy depositional conditions: A case study from the Mio–Pliocene Siwalik fluvial sequence near Dehra Dun, NW Himalaya, India. Sedimentary Geology, 177(3-4): 229-252
Kusky T.M. and Li Jianghai. 2003. Paleoproterozoic tectonic evolution of the North China Craton. Journal of Asian Earth Sciences, 22(4): 383-397
Lacassin R., Valli F., Arnaud N., et al. 2004. Large-scale geometry, offset and kinematic evolution of the Karakorum fault, Tibet. Earth and Planetary Science Letters, 219(3-4): 255-269
Larrasoana, J.C., Murelaga, X. and Garces, M. 2006. Magnetobiochronology of Lower Miocene (Ramblian) continental sediments from the Tudela Formation (western Ebro basin, Spain). Earth and Planetary Science Letters, 243(3-4):409-423
Lasserre C., Gaudemer Y., et al. 2002. Fast late Pleistocene slip rate on the Lenglongling segment of the Haiyuan fault,Qinghai,China. Journal of Geophysical Research, 107(B11):2276
Lasserre C., Morel P.H., Gaudemer Y. et al. 1999. Postglacial left slip rate and post occurrence of M>=8 earthquakes on the western Haiyuan fault, Gansu, China. Journal of Geophysical Research, 104(B8): 17633-17651
Leech M.L., Singh S., Jain A.K., et al. 2005. The onset of India–Asia continental collision: Early, steep subduction required by the timing of UHP metamorphism in the western Himalaya. Earth and Planetary Science Letters, 234(1-2): 83-97
Lehmkuhl F. and Haselein F. 2000. Quaternary paleoenvironmental change on the Tibetan Plateau and adjacent areas (Western China and Western Mongolia). Quaternary International, 65-66: 121-145
Li Youli, Yang Jingchun, Tan Lihua, et al. 1999. Impact of tectonics on alluvial landforms in the Hexi Corridor, Northwest China. Geomorphology, 28(3-4): 299-308
Lin Aimin, Yang Zhengyu, Sun Zhiming, et al. 2001. How and when did the Yellow River develop its square bend? Geology, 29(10): 951-954
Liu Shaofeng, Steel R.and Zhang Guowei. 2005. Mesozoic sedimentary basin development and tectonic implication, northern Yangtze Block, eastern China: record of continent–continent collision. Journal of Asian Earth Sciences, 25(1): 9-27
Liu Z.,C. Wang. 2001. Facies analysis and depositinal systems of Cenozoic sediments in the Hoh Xil basin, northern Tibet. Sedimentary Geology, 140:251-270
Liu Zhifei and Wang Chengshan. 2001. Facies analysis and depositional systems of Cenozoic sediments in the Hoh Xil basin, northern Tibet. Sedimentary Geology, 140(3-4): 251-270
Mankinen E. A. and Dalrymlie G. B. 1979. Revised geomagnetic polarity time scale for interval 0.5m.y.BP, J.G.R., 1979, 84: 615-626
Marques F. O.and Cobbold P. R. 2002. Topography as a major factor in the development of arcuate thrust belts: insights from sandbox experiments. Tectonophysics, 348(4): 247-268
McFadden P.L. 1990. A new fold test for paleomagnetic studies. Geophys J Int,103: 163-169
Meissner R., Rabbel W. and Kern H. 2006. Seismic lamination and anisotropy of the Lower Continental Crust. Tectonophysics, 416(1-4): 81-99
Metivier F., Gaudemer Y., Tapponnier P., et al. 1998. Northastward growth of the Tibet plateau deduced from balanced reconstruction of two deposional areas: The Qaidam and Hexi corridor basins, China. Tectonics, 17(6):823-842
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. Geophys. J. Int., 135: 1-47
Molanar P., Burchfiel B.C., Lian K., et al. 1987. Geomorphic evidence for active faulting in the Altyn Tagh and northern Tibet and qualitative estimates of its contribution to the convergence of India and Eurasia. Geology, 15:245-253
Molar P., Tapponnier P. 1975. Cenozoic tectonics of Asia: Effects of a continental collision. Science, 189: 419-426
Molnar P. 1986. The Geologic History and structure of the Himalaya. American Scientist, 74: 144-154
Molnar P. 1988. Continental tectonics in the aftermath of plate tectonics. Nature, 335(6186): 131-137
Molnar P. 2004. Late Cenozoic increase in accumulation rates of terrestrial sediment: How might climate change have affected erosion rates? Ann. Rev. Earth Planet. Sci., 32: 67-89
Molnar P. and England P. 1990. Late Cenozoic uplift of mountain ranges and global climate change: chicken or egg? Nature, 346: 29-33
Molnar P.,England P.,Martinod J.1993. Mantle dynamics,uplift of the Tibet plateau, and the Indian monsoon. Rev. Geophys, 31: 357-396
Molnar, P., 2005. Mio-Pliocene Growth of the Tibetan Plateau and Evolution of East Asian Climate. Palaeontologia Electronica, 8(1): 1-23
Morrill C., Overpeck J. T., Cole J. E., et al. 2006. Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet. Quaternary Research, Volume 65(2): 232-243
Mukhopadhyay D.K.and Mishra P. 2005. A balanced cross section across the Himalayan frontal fold-thrust belt, Subathu area, Himachal Pradesh, India: thrust sequence, structural evolution and shortening. Journal of Asian Earth Sciences, 25(5):735-746
Mukul M. 2000. The geometry and kinematics of the Main Boundary Thrust and related neotectonics in the Darjiling Himalayan fold-and-thrust belt, West Bengal, India. Journal of Structural Geology, 22(9): 1261-1283
Myrow P. M., Hughes N. C., Paulsen T. S., et al. 2003. Integrated tectonostratigraphic analysis of the Himalaya and implications for its tectonic reconstruction. Earth and Planetary Science Letters, 212(3-4): 433-441
Najman Y. 2006. The detrital record of orogenesis: A review of approaches and techniques used in the Himalayan sedimentary basins. Earth-Science Reviews, 74(1-2): 1-72
Pares, J.M., Van der Voo, R., Downs, R.W., et al. 2003. Northeastward growth and uplift of the Tibetan Plateau: Magnetostratigraphic insights from the Guide Basin. J. Geophys. Res., 108:1-11
Peltzer G. and P. Tapponnier, 1989. Armijo R. Magnitude of late Quaternary left-lateral displacements along the northern edge of Tibet. Science, 246:1285-1289
Peltzer G. and Tapponnier P. 1988. Formation and evolution of strike-slip faults, rifts,and basins during the India-Asia collision: an experimental approach, Journal of Geophysical research, 93(B12): 15085-15117
Piedilato S. and Prosser G. 2005. Thrust sequences and evolution of the external sector of a fold and thrust belt: An example from the Southern Apennines (Italy). Journal of Geodynamics, 39(4): 386-402
Qiang X. K., Li Z. X., Powell C. McA., et al. 2001. Magnetostratigraphic record of the Late Miocene onset of the East Asian monsoon, and Pliocene uplift of northern Tibet. Earth and Planetary Science Letters, 187(1-2): 83-93
Quade J., Cerling T. E., Bowman J.R. 1989. Development of Aasian monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan. Nature, 342(9): 163-166
Raza S. M., Cheema I. U., Downs W. R., et al. 2002. Miocene stratigraphy and mammal fauna from the Sulaiman
Range, Southwestern Himalayas, Pakistan. Palaeogeography, Palaeoclimatology, Palaeoecology, 186(3-4): 185-197
Royden L.H., Burchfiel B.C., King R.C., et al. 1997. Surface deformation and lower crustal flow in eastern Tibet. Science, 276: 788-790
Sanyal P., Bhattacharya S. K., Kumar R., et al. 2004. Mio–Pliocene monsoonal record from Himalayan foreland basin (Indian Siwalik) and its relation to vegetational change. Palaeogeography, Palaeoclimatology, Palaeoecology, 205(1-2): 23-41
Scharer K. M., Burbank D. W., Chen J., et al. 2004. Detachment folding in the Southwestern Tian Shan–Tarim foreland, China: shortening estimates and rates. Journal of Structural Geology, 26(11): 2119-2137
Sciesciani V. Calamita F. Tavarnelli E., et al. 2001. Foreland-dipping normal faults in the inner edges of syn-orogenic basin: a case from the Central Apennines, Italy. Tectonophysics, 330: 211-224
Shi Yafeng. 2002. Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia. Quaternary International, 97-98: 79-91
Singh B. P. 2003. Evidence of growth fault and forebulge in the Late Paleocene (57.9–54.7 Ma), western Himalayan foreland basin, India. Earth and Planetary Science Letters, 216(4): 717-724
Sissingh W. 2001. Tectonostratigraphy of the West Alpine Foreland: correlation of Tertiary sedimentary sequences, changes in eustatic sea-level and stress regimes. Tectonophysics, 333(3-4): 361-400
Sobel E. R., and Dumitru T.A. 1997. Exhumation of the margins of the western Tarim Basin during the Himalayan orogeny. J. Geophys. Res., 102: 5043-5064
Sobel E.R., Hilley G.E., and Strecker M.R. et al. 2003. Formation of internally drained contractional basins by aridity-limited bedrock incision. Journal of Geophysical Research, 108(B7): 2344, doi:10.1029/2002JB001883
Sobel E.R., Trevor A.D. 1997. Thrusting and exhumation around the margins of the weatern Tarim basin during the India-Asia collision. Journal of Geophysical Research, 102(B3): 5043-5063
Speranza F., Adamoli L., Maniscalco R., et al. 2003. Genesis and evolution of a curved mountain front: paleomagnetic and geological evidence from the Gran Sasso range (central Apennines, Italy). Tectonophysics, 362(1-4): 183-197
Sun Jimin, Zhu Rixiang and An Zhisheng. 2005. Tectonic uplift in the northern Tibetan Plateau since 13.7 Ma ago inferred from molasse deposits along the Altyn Tagh Fault. Earth and Planetary Science Letters, 235(3-4): 641-653
Sun Zhiming, Yang Zhenyu, Pei Junling, et al. 2005. Magnetostratigraphy of Paleogene sediments from northern Qaidam Basin, China: Implications for tectonic uplift and block rotation in northern Tibetan plateau. Earth and Planetary Science Letters, 237(3-4): 635-646
Sun Zhiming, Yang Zhenyu, Pei Junling, et al. 2006. New Early Cretaceous paleomagnetic data from volcanic and red beds of the eastern Qaidam Block and its implications for tectonics of Central Asia. Earth and Planetary Science Letters, 243(1-2):268-281
Suppe J., Chou T. and Stephen C. 1992. Rate of folding and faulting determined from growth strata. In: McClay K. R. Ed. Thrust Tectonics, New York: Chapman and Hall, 105-122.
Tapponnier P. and Molnar P. 1976. Slip-line field theoory and large-scale continental tectonics. Nature, 264(5584):319-324
Tapponnier P., B. Meyer, J.P. Avouac et al. 1993. Active thrusting and folding in the Qi Lian Shan, and decoupling between upper crust and mantle in northeastern Tibet.Earth and Planetary science Letters, 97:382-403
Tapponnier P., Ryerson F.J., Woerd J.V., et al. 2001a. Long-term slip rates and characteristic slip: keys to active fault behavior and earthquake hazard. Earth and Planetary Sciences, 333: 483-494
Tapponnier P., Xu Zhiqin, Francoise R., et al. 2001b. Oblique stepwise rise and growth of the Tibet Plateau. Science, 294: 1671-1677
Vincent S.J. and Allen M.B. 1999. Evolution of the Minle and Chao shui Basins,China:Implications for Mesozoic strike-slip basin formation in Central Asia. GSA Bulletin, 111(5): 725-742
Wang E. 1997. Displacement and timing along the northern strand of the Altyn Tagh fault zone, Northern Tibet. Earth and Planetary Science Letters, 150:55-64
Wang R. L., Scarpitta S. C., Zhang S. C., et al. 2002. Later Pleistocene/Holocene climate conditions of Qinghai–Xizhang Plateau (Tibet) based on carbon and oxygen stable isotopes of Zabuye Lake sediments. Earth and Planetary Science Letters, 203(1): 461-477
Williams H., Turner S., Kelley S., et al. 2001. Age and composition of dikes in Southern Tibet: New constraints on the timing of east-west extension and its relationship to postcollisional volcanism. Geology, 29(4):339-342
Willis B. J. and Behrensmeyer A. K. 1995. Fluvial systems in the Siwalik Miocene and Wyoming Paleogene. Palaeogeography, Palaeoclimatology, Palaeoecology, 115(1-4): 13-35
Wu Yongqiu, Cui Zhijiu, Liu Gengnian, et al. 2001. Quaternary geomorphological evolution of the Kunlun Pass area and uplift of the Qinghai-Xizang (Tibet) Plateau. Geomorphology, 36(3-4): 203-216
Yamada K., Fukusawa, Fang H., Pan X.M., et al. 1999. High-resolution multi-proxy records of Asian monsoon activities from terrestrial sediments over the last 75,000 years. Chin. Sci. Bull., 44 (Suppl. 1): 223-229
Yan Maodu, VanderVoo R., Fang Xiao-min, et al. 2006. Paleomagnetic evidence for a mid-Miocene clockwise rotation of about 25° of the Guide Basin area in NE Tibet. Earth and Planetary Science Letters, 241(1-2): 234-247
Yin A. and Harrison. M.T. 2000. Geologic Evolution of the Himalayan-Tibetan Orogen. Annu. Rev. Earth Planet. Sci. , 2000, 28: 211-28
Yin A., Nie S., Harrison T. M., et al. 1998. Lateozoic tectonic evolution of the southern Chinese Tinshan. Tectonic,17:1-27
Yin An, Rumelhart P.E., Butler R., et al. 2002. Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation. GSA Bulletin, 114(10): 1257-1295
Yin An. 2006. Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation. Earth-Science Reviews, In Press
Yue Yongjun, Graham S. A., Ritts B. D., et al. 2005. Detrital zircon provenance evidence for large-scale extrusion along the Altyn Tagh fault. Tectonophysics, 406(3-4): 165-178
Zachos, J. C., Pagani M., Sloan L., et al. 2001. Trends, rhythms, and aberrations in global climate 65 Ma to Present, Science, 292: 686-693
Zhang P.Z, Shen Z.K., Burgman R., et al. 2004. Continuous deformation of the Tibetan Plateau constrained from Global Positioning measurements. Geology, 32(9): 809-812
Zhang P.Z., Burchfiel B.C., Molnar P., et al. 1990. Late Cenozoic tectonic evolution of southern Ningxia, northeastern margin of Tibetan Plateau. Bull. Geol. Soc. Am., 102: 1484-1498
Zhang P.Z., Burchfiel B.C., Molnar P., et al. 1991a. Rate, amount, and style of late Cenozoic deformation of southern Ningxia, northeastern margin of Tibetan Plateau. Tectonics, 10: 1111-1129
Zhang P.Z., Molnar P. and Downs W. et al. 2001. Increased sedimentation rates and grainsizes 2-4 Myr ago due to the influence of climate changes on erosion rates. Nature, 410: 891-897
Zhang P.Z., Burchfiel B.C., Molnar P., et al. 1991b. Later Cenozoic tectonic evolution of the Ningxia Hui Autonomous Region, China. GSA Bulletin, 102:1484-1498
Zhang Y., Vergely P. and Mercier J. 1995. Active faulting in and along the Qinling Range (China) inferred from spot imagery analysis and extrusion tectonics of south China. Tectonophysics, 243: 69-95
Zhang Yueqiao, Ma Yinsheng, Yang Nong, et al. 2003. Cenozoic extensional stress evolution in North China. Journal of Geodynamics, 36(5): 591-613
Zhang Zhenke, Wang Sumin, Yang Xiangdong, et al. 2004. Evidence of a geological event and environmental change in the catchment area of the Yellow River at 0.15 Ma. Quaternary International, 117(1): 35-40
Zhou Jianxun, Xu Fengyin, Wang Tiecheng, et al. 2006. Cenozoic deformation history of the Qaidam Basin, NW China: Results from cross-section restoration and implications for Qinghai–Tibet Plateau tectonics. Earth and Planetary Science Letters, 243(1-2): 195-210
曹国强, 陈世悦, 徐凤银, 等. 2005. 柴达木盆地西部中-新生代沉积构造演化. 中国地质,32(1): 33-40
柴炽章,焦德成,张维歧.1997.天景山断裂带晚第四纪水平活动强度的分时、分段研究.中国地震,13(1):35-42
常承法, 郑锡澜. 1973. 中国西藏南部珠穆朗玛地区地质构造特征及其青藏高原东西向诸山系形成的探讨. 中国科学(D), 2: 190-201
陈发景,汪新文,张光亚等. 1996. 中国中、新生代前陆盆地的构造特征和地球动力学. 地球科学,21(4):366-372
陈发景和汪新文. 1997. 中国中、新生代含油气盆地成因类型、构造体系及地球动力学模式. 现代地质,11(4):409-424
陈建华和田景春. 2000. 层序地层学的产生、现状与展望. 复式油气田, 2: 9-12
陈杰, 卢演俦, 丁国瑜. 1996. 祁连山西段及酒西盆地区第四纪构造运动的阶段划分. 第四纪研究, 3:265-271
陈杰, 卢演俦, 丁国瑜. 2001. 塔里木西缘晚新生代造山过程的记录——磨拉石建造及生长地层和生长不整合. 第四纪研究, 21(6): 528-539
陈杰, 卢演俦. 2001. 中国西部前陆盆地生长不整合、生长地层与构造变形. 卢演俦, 高维明, 等主编, 新构造与环境. 北京: 地震出版社, 407-421
陈杰, 尹金辉, 曲国胜, 等. 2000. 塔里木盆地西缘西域组的底界、时代、成因与变形过程的初步研究. 地震地质, 22(增刊): 104-116
陈杰,卢演俦. 2001. 中国西部前陆盆地生长不整合、生长地层与构造变形.卢演俦,高维明等主编:新构造与环境,北京:地震出版社,407-421
陈诗越, 王苏民, 沈吉. 2003. 青藏高原中部错鄂湖晚新生代以来的沉积环境演变及其构造隆升意义. 湖泊科学, 15(1): 21-27
陈书平, 汤良杰, 张一伟. 2001. 前陆、前陆盆地和前陆盆地系统. 世界地质, 20(4): 332-338
陈宣华, Yin An, Gehrels G. E., 等. 2004. 青藏高原北缘阿尔金东段中生代南北向伸展作用. 地质力学学报, 10(3): 193-212
陈正乐, 万景林, 王小风, 等. 2002. 阿尔金断裂带 8Ma 的快速走滑及其地质意义. 地球学报, 23(4): 295-300
陈正乐, 王小凤, 冯夏红, 等. 2003. 青藏高原北缘山脉隆升时间的同位素证据. 吉林大学学报(地球科学版), 33(3): 270-275
崔效锋, 谢富仁, 赵建涛. 2005. 中国及邻区震源机制解的分区特征. 地震地质, 27(2): 298-307
崔之久, 伍永秋, 刘耕年, 等. 1997. 昆仑-黄河运动的发现及其性质. 科学通报, 42(18): 1986-1989.
崔之久, 伍永秋, 刘耕年, 等. 1998. 关于“昆仑-黄河运动”. 中国科学(D), 28(1): 53-59
戴霜, 方小敏, 宋春晖, 等. 2005. 印度-欧亚板块碰撞在高原北部的早期响应. 科学通报,50(7): 673-683
邓宏文, 王红亮, 阎伟鹏, 等. 2004. 河流相层序地层构成模式探讨. 沉积学报, 22(3): 373-379
邓宏文, 王洪亮, 翟爱国, 等. 1999. 中国陆源碎屑盆地层序地层与储层展布. 石油与天然气地质, 20(2): 108-114
邓晋福, 苏尚过, 赵海玲, 等. 2003. 华北地区燕山期岩石圈减薄的深部过程. 地学前缘(中国地质大学,北京), 10(3): 41-50
邓平, 舒良树, 谭正中, 等. 2003 华南中、新生代盆地地球动力学背景. 华南铀矿地质, 20(1): 1-17
邓起东, 张培震, 冉勇康, 等. 2003. 中国活动构造基本特征. 中国科学(D 辑), 32(12): 1020-1030
邓涛, 王晓鸣, 倪喜军, 等. 2004. 临夏盆地的新生代地层及其哺乳动物化石证据. 古脊椎动物学报, 42(1): 45-66
邓涛. 2004. 临夏盆地晚新生代哺乳动物群演替与青藏高原隆升背景. 第四纪研究, 24(4): 413-420
邓万明. 2003. 青藏及邻区新生代火山活动及构造演化. 地震地质, 25(增刊): 51-61
丁林, 钟大赉, 刘福田, 等. 2000. 造山带岩石层多向层架构造及其对新生代岩浆活动制约——以三江及邻区为例. 中国科学(D), 30(增刊): 1-8。
丁林,钟大赉,潘裕生等. 1995. 东西马拉雅构造结上新世以来快速抬升的裂变径迹证据. 科学通报,40(16):1479-1500。
董国榜, 陈云, 吴锡浩, 等. 1999. 中国更新世环境巨变的孢粉植物群记录. 地质力学学报, 5(4): 11-21
董冶平, 雷芳, 申秀荣,等. 2003. 西秦岭北缘断裂带的深部构造特征及其与地震活动的关系.内陆地震, 10(3): 224-234
杜远生, 张哲, 周道华, 等. 2002. 北祁连—河西走廊志留纪和泥盆纪古地理及其对同造山过程的沉积响应. 古地理学报, 4(4): 1-8
杜远生, 朱杰, 韩欣, 等. 2004. 从弧后盆地到前陆盆地——北祁连造山带奥陶纪-泥盆纪的沉积盆地与构造演化. 地质通报, 23(9-10): 911-917
段志明, 李勇, 李亚林, 等. 2005. 青藏高原北部温泉活动沉积盆地的沉积特征及其地质意义. 沉积与特提斯地质, 25(1-2): 181-188
范马洁, 宋春晖. 2003. 青藏高原东北缘临夏盆地王家山地区沉积环境分析与构造隆升. 兰州大学学报, 39(3): 84-89
方爱民, 阎臻, 刘小汉, 等. 2005. 藏南柳区砾岩中古植物化石组合及其特征. 古生物学报, 44(3): 435-445
方世虎, 郭召杰, 张志诚, 等. 2004. 天山北缘前陆冲断带形成时间的地层学证据. 新疆地质, 22(1): 24-28
方小敏, 李吉均, 马玉贞, 等. 1998. 青藏高原(以临夏盆地为主)天然剖面记录. 施雅风、李吉均和李炳元主编,青藏高原晚新生代隆升与环境变化. 广州: 广东科技出版社, 19-48
方小敏, 赵志军, 李吉均, 等. 2004. 祁连山北缘酒西盆地晚新生代磁性地层与高原隆升. 中国科学(D 辑), 34(2): 97-106
方小敏,李吉均,朱俊杰, 等. 1995. 临夏盆地中心王家山剖面磁性地层与构造事件. 见:见青藏高原形成演化、环境变迁与生态系统研究学术论文年刊(1994),北京: 科学出版社
方小敏,李吉均,朱俊杰, 等. 1997. 甘肃临夏盆地新生代地层绝对年龄测定与划分. 科学通报, 42(14):1457-1471
方小敏,宋春晖,高军平, 等. 2003. 青藏高原东北边缘晚新生代哺乳动物化石的磁性地层学. 科学通报, 47(23): 1824-1828
方小敏和李吉均. 1998. 3.4 百万年来青藏高原隆升的阶段性与环境演变. 施雅风、李吉均和李炳元主编, 青藏高原晚新生代隆升与环境变化. 广州: 广东科技出版社. 394-414
冯益民. 1997. 祁连造山带研究概况, 历史, 现状及展望. 地球科学进展, 12(4): 307-314
冯有良, 周海民, 李思田, 等. 2004. 陆相断陷盆地层序类型与构造特征. 地质论评, 50(1): 43-49
符超峰, 方小敏, 宋友桂, 等. 2005. 盆山沉积耦合原理在定量恢复造山带隆升剥蚀过程中的应用. 海洋地质与第四纪地质,25(1): 105-112
甘肃省地质矿产局. 1989. 甘肃省区域地质志. 北京: 地质出版社
高长林, 叶德燎, 钱一雄. 2000. 前陆盆地的类型及油气远景. 石油实验地质, 22(2): 99-104
高红山, 潘保田, 邬光剑, 等. 2004. 祁连山东段剥蚀面与青藏高原隆升. 冰川冻土, 26(5): 540-544
高星, 王卫民, 姚振兴. 2005. 中国及邻近地区地壳结构. 地球物理学报, 48(3): 591-601
葛肖虹, 刘俊来. 1999. 北祁连造山带的形成与背景. 地学前缘, 6(4): 223-230
顾家裕, 张兴阳. 2005. 中国西部陆内前陆盆地沉积特征与层序格架. 沉积学报,23(2): 187-193
国家地震局地质研究所, 宁夏回族自治区地震局. 1990. 海原活动断裂带. 北京: 地震出版社, 1-286
韩建恩, 余佳, 孟庆伟, 等. 2005. 西藏阿里地区札达盆地第四纪砾石统计及其意义. 地质通报, 24(7): 630-636
何登发,李德生,吕修祥. 1996. 中国西北地区含油气盆地构造类型. 石油学报,17( 4):8-18
何光玉, 卢华复, 杨树锋, 等. 2004. 库车中新生代盆地沉降特征. 浙江大学学报(理学版), 21(1): 110-113
侯明才, 陈洪德, 田景春. 2003. 层序充填动力学——层序地层研究的新方向. 地层学杂志, 27(4): 358-364
侯明才, 伊海生, 刘与安, 等. 2002. 测老庙盆地层序地层格架与其幕式构造演化. 地球学报, 23(1): 63-66
胡见义,赵文智,钱凯等. 1996. 中国西北地区石油天然气地质基本特征. 石油学报,17(3):1-11
胡玲, 何登发, 胡道功. 2005. 准噶尔盆地南缘霍尔果斯-玛纳斯-吐谷鲁断裂晚新生代构造变形的 ESR 测年证据. 地球学报, 26(2): 121-126
黄宝春, Yo-Ichiro O, 杨振宇, 等. 2000. 河西走廊和阿拉善东缘地区中寒武世古地磁研究的初步结果. 地球物理学报, 43(3): 393-401
黄华芳,彭作林,卢伟, 等. 1993. 酒西盆地、酒东盆地第三系磁性地层的划分与对比. 甘肃地质学报, 2(1): 6-16
黄继钧. 2000. 羌塘盆地性质及构造演化. 地质力学学报, 6(1): 58-66
黄立功, 钟建华, 郭泽清, 等. 2004. 阿尔金造山带中、新生代的演化. 地球学报, 25(3): 287-294
吉让寿, 刘光祥, 潘文蕾, 等. 2003. 试论前陆-伸展盆地. 石油实验地质, 25(增刊): 539-542
吉让寿,钱一雄,范小林等. 2000. 中国西北地区中生代盆地与油气. 西安:西安地图出版社,239
贾承造, 何登发, 陆洁民. 2004. 中国喜马拉雅运动的期次及其动力学背景. 石油与天然气地质, 25(2): 121-169
蒋晓玮, 王江海, 张会化. 2003. 西秦岭断裂走滑与盆地的耦合——西秦岭—松甘块体新生代向东走滑挤出的证据. 地学前缘(中国地质大学,北京), 10(3): 207-208
靳久强. 1997. 中国中西部前陆盆地的油气勘探. 石油勘探与开发,24(5):11-14
康来迅. 1990. 西秦岭北缘断裂带晚更新世晚期以来断裂运动的基本特征及运动机理. 中国地震, 6(3): 53-61
赖绍聪, 秦江锋, 李永飞. 2005. 青藏北羌塘新第三纪玄武岩单斜辉石地球化学. 西北大学学报(自然科学版),35(5): 611-615
雷振宇,何登发,张朝军. 2001. 中国中西部类前陆盆地与典型前陆盆地类比及其油气勘探前景. 地球学报,22(2): 169-174
李才, 翟明国, 程立人, 等. 2005. 青藏高原羌塘地区几个关键地质问题的思考. 地质通报, 24(4): 295-301
李春昱,刘仰文,朱宝清,等. 1978. 秦岭及祁连山构造发展史. 西北地质科技情报,4: 1-12
李大荣. 2004. 陆相层序地层学研究新进展. 江汉石油学报, 14(2): 13-17
李德威. 2003. 青藏高原隆升机制新模式. 地球科学——中国地质大学学报, 28(6): 593-600
李奋其, 王成善, 朱利东, 等. 2002. 区域挤压体制下盆-山耦合关系探讨——以河西走廊和北祁连山为例. 沉积与特提斯地质, 22(4): 17-25
李吉均, 方小敏, 马海洲, 等. 1996. 晚新生代黄河上游地貌演化与青藏高原隆起. 中国科学(D), 26(4): 316-322
李吉均, 方小敏, 潘保田, 等. 2001. 新生代晚期青藏高原强烈隆起及其对周边环境的影响. 第四纪研究, 21(5): 381-391
李吉均, 方小敏, 朱俊杰, 等. 1995. 临夏盆地新生代地层古地磁年代与模式序列. 见: 青藏项目专家委员会编, 青藏高原形成演化、环境变迁与生态系统研究学术论文年刊(1994). 北京: 科学出版社, 41-54
李吉均, 施雅风, 方小敏, 等. 1998. 青藏高原晚新生代隆生与环境变化. 广东科技出版社
李吉均, 文世宣, 张青松, 等. 1979. 青藏高原隆起的时代、幅度和形式的探讨. 中国科学, 6: 608-616
李吉均. 1999. 青藏高原的地貌演化与亚洲季风. 海洋地质与第四纪地质, 19(1): 1-11
李吉均和方小敏. 1998. 青藏高原隆起与环境变化研究. 科学通报, 43(15): 1569-1574
李继亮, 肖文交, 闫臻. 2003. 盆山耦合与沉积作用. 沉积学报, 21(1): 52-60
李江海, 牛向龙, 陈征, 等. 2004. 太行山区深层次推覆构造的发现及其地质意义. 自然科学进展, 14(10): 1118-1127
李前裕, 郑洪波, 钟广法, 等. 2005. 南海晚渐新世滑塌沉积指示的地质构造事件. 地球科学——中国地质大学学报, 30(1): 19-24
李儒峰, 马永生, 汤良杰, 等. 2004. 云南楚雄盆地波动特征及构造沉积演化. 地球科学-中国地质大学学报, 29(3): 309-316
李双泉. 2005. 潮水盆地与酒西盆地中新生代构造对比. 天然气地球科学, 16(4): 464-468
李双应, 岳书仓, 王道轩, 等. 2002. 大别造山带北缘中生代地层格架厘定. 地层学杂志, 26(3): 178-186
李喜臣, 王永, 丁孝忠. 2005. 西昆仑山前晚新生代磨拉石时代及意义. 地质力学学报,11(2): 181-186
李向东和王克卓. 2000. 塔里木盆地西南及邻区特提斯格局和构造意义. 新疆地质, 18(2): 113-120
李孝泽, 董光荣, 陈惠中, 等. 2001. 从青藏高原南北两个磨拉石削面的对比看青藏高原的隆升过程. 中国沙漠, 21(4): 354-360
李勇, 曹叔尤, 周荣军, 等. 2005. 晚新生代岷江下蚀速率及其对青藏高原东缘山脉隆升机制和形成时限的定量约束. 地质学报, 79(1): 28-37
李勇, 侯中健, 司光影, 等. 2002. 青藏高原东缘新生代构造层序与构造事件. 中国地质, 29(1): 30-36
李勇, 王成善, 伊海生, 等. 2001. 青藏高原中侏罗世 —早白垩世羌塘复合型前陆盆地充填模式. 地层学杂志, 19(1): 20-27
李勇, 王成善, 伊海生. 2002. 中生代羌塘前陆盆地充填序列及演化过程. 地层学杂志, 26(1): 62-67
李勇, 王成善, 曾允孚, 等. 2000. 造山作用与沉积响应. 矿物岩石, 20(2): 49-56
李勇和孙爱珍. 2000. 龙门山造山带构造地层学研究. 地层学杂志, 24(3): 202-206
李云通, 孙秀玉, 王大宁, 等. 1984. 中国地层(13)——中国的第三系. 北京: 地质出版社, 1-362.
梁忠和邓涛. 2005. 甘肃临夏盆地晚中新世大唇犀化石的年龄结构与生活环境. 古脊椎动物学报, 43(3): 219-230
刘朝露, 贾承造, 夏斌, 等. 2005. 塔东地区盆山耦合与油气成藏模式研究. 天然气地球科学,16(5): 552-558
刘池洋, 赵红格, 王锋, 等. 2005. 鄂尔多斯盆地西缘(部)中生代构造属性. 地质学报, 79(6): 737-745
刘池洋, 赵红格, 杨兴科, 等. 2002. 前陆盆地及其确定和研究. 石油与天然气地质, 23(4): 307-313
刘德民和李德威. 2002. 造山带与沉积盆地的耦合——以青藏高原周边造山带与盆地为例. 西北地质, 35(1): 15-21
刘耕武. 1996. 青藏高原东部地区晚新生代孢粉组合特征及其古地理意义. 微体古生物学报, 13(4): 363-372
刘和甫, 李晓青, 刘立群, 等. 2004. 走滑构造体系盆山耦合与区带分析. 现代地质, 18(2): 139-150
刘和甫, 汪泽成, 熊保贤, 等. 2000. 中国中西部中、新生代前陆盆地与挤压造山带耦合分析. 地学前缘(中国地质大学学报,北京), 7(3): 55-72
刘和甫. 1995. 前陆盆地类型及褶皱-冲断层样式. 地学前缘(中国地质大学, 北京), 2(3-4): 59-68
刘和甫. 2000. 盆山耦合类型. 地学前缘,7(4 ):469
刘和甫. 2001. 盆地—山岭耦合体系与地球动力学机制. 地球科学——中国地质大学学报, 26(6): 582-596
刘少峰, 李思田, 庄新国, 等. 1996. 鄂尔多斯西南缘前陆盆地沉降和沉降过程模拟. 地质学报, 70(1): 12-22
刘树根, 罗志立, 赵锡奎, 等. 2005. 试论中国西部陆内俯冲型前陆盆地的基本特征. 石油与天然气地质, 26(1): 37-48
刘志飞, 王成善, 金玮, 等. 2004. 可可西里盆地早渐新世雅西措群爬升沙纹层理及其沉积环境意义. 沉积学报, 22(4): 560-565
刘志宏, 卢华复, 李西建, 等. 2000. 库车再生前陆盆地的构造演化. 地质科学, 35(4): 482-492
柳益群, 李文厚, 冯乔. 1997. 鄂尔多斯盆地东部上三叠统含油砂岩的古地温及成岩阶段. 地质学报, 71(1): 65-74
吕连清,方小敏,鹿化煜,等. 2004. 青藏高原黄土末次冰期千年尺度冬季风变化的粒度记录. 科学通报, 49:1091-1098
罗开平和范小林. 2004. 河西走廊及邻区中新生代成盆背景与盆地原型. 石油实验地质, 26(5): 432-436
罗志立, 李景明, 李小军, 等. 2004. 中国前陆盆地特征及含油气远景分析. 石油地质, 2: 1-11
马华东和扬子江. 2003. 塔里木盆地西南新生代盆地演化特征. 新疆地质, 21(1): 92-95
马钦忠, 李吉均. 2003. 晚新生代青藏高原北缘构造变形和剥蚀变化及其与山脉隆升关系. 海洋地质与第四纪地质, 23(1): 27-34
马寅生, 施炜, 张岳桥, 等. 2005. 东昆仑活动断裂带玛曲段活动特征及其东延. 地质通报, 24(1): 30-35
马玉贞, 李吉均, 方小敏. 1998. 临夏地区 30.6-5.0Ma 红层孢粉植物群与气候演化记录. 科学通报, 43(3): 301-304
毛明陆, 刘池洋. 1995. 河西走廊东部晚古生代前陆盆地演化特征. 甘肃地质学报, 4(2): 55-61
聂军胜, 宋春晖, 方小敏, 等. 2002. 贵德盆地黄河出现的古地磁年代及其意义. 海洋地质与第四纪地质, 23(2): 59-64
宁夏回族自治区地质局. 1990. 宁夏回族自治区地质志. 北京: 地质出版社, 47-85
宁夏回族自治区地质矿产局. 1996. 宁夏回族自治区岩石地层(全国地层多重划分和对比 64). 北京: 中国地质大学出版社, 1-32
潘安定. 1998. 临夏东山顶剖面的第四纪孢粉记录及其古环境研究. 海洋地质与第四纪地质, 18(1): 89-96
潘安定. 2000. 青藏高原东北边缘第四纪孢粉记录的环境意义(英文). 微体古生物学报, 17(2): 178-185
潘保田, 高红山, 李炳元, 等. 2004. 青藏高原层状地貌与高原隆升. 第四纪研究, 24(1): 50-58
潘裕生, 汪一鹏, 常承法. 1980. 喜马拉雅板块活动证据兼论青藏高原形成模式. 地震地质, 2(2): 1-9
潘裕生. 1999. 青藏高原的形成与隆升. 地学前缘(中国地质大学,北京), 6(3): 153-163
裴先治, 吴汉泉, 左国朝. 1999. 北祁连早古生代俯冲杂岩带的变形特征与构造演化. 西安工程学院学报, 21(1): 9-17
钱方. 1999. 青藏高原晚新生代磁性地层研究. 地质力学学报, 5(4): 22-34
钱祥麟. 2004. 新生代板内造山作用研究——认识中国区域地质构造基本特征的关键. 地学前缘(中国地质大学,北京), 11(3): 221-225
邱瑞照, 邓晋福, 周肃, 等. 2005. 青藏高原西部蛇绿岩类型:岩石学与地球化学证据. 地学前缘(中国地质大学,北京,北京大学), 12(2): 277-291
邱占祥, 王伴月, 邓涛. 2004. 甘肃临夏盆地牙沟的哺乳动物化石及有关地层问题. 古脊椎动物学报, 42(4): 276-296
任收麦, 葛肖虹, 刘永江, 等. 2004. 晚白垩世以来沿阿尔金断裂带的阶段性走滑隆升. 地质通报, 23(9-10): 926-932
任战利, 肖晖, 刘丽, 等. 2005. 沁水盆地新生代抬升冷却事件的确定. 石油与天然气地质, 26(1): 109-113
申旭辉, 田勤俭, 丁国瑜, 等. 2001. 宁夏贺家口子地区晚新生代地层序列及其构造意义. 中国地震, 17(2): 156-166
沈正康, 王敏, 甘卫军, 等. 2003. 中国大陆现今构造应变率场及其动力学成因研究. 地学前缘(中国地质大学,北京), 10(增刊): 307-313
施雅风, 李吉均, 李炳元, 等. 1999. 晚新生代青藏高原的隆升与东亚环境变化. 地理学报, 54(1): 10-21
施雅风和刘东生. 1964. 希夏邦马峰地区科学考察报告.科学通报,10: 928-938
舒良树, 郭召杰, 朱文斌, 等. 2004. 天山地区碰撞后构造与盆山演化. 高校地质学报,10(3): 393-404
宋春晖, 方小敏, 高军平, 等. 2001a. 青藏高原东北部贵德盆地新生代沉积演化与构造隆升. 沉积学报, 19(4): 493-500
宋春晖, 方小敏, 李吉均, 等. 2001b. 青藏高原北缘酒西盆地 13Ma 以来沉积演化与构造隆升. 中国科学(D辑), 31(增刊): 155-162
宋春晖, 高东林, 方小敏, 等. 2005. 青藏高原昆仑山垭口盆地晚新生代高精度磁性地层及其意义. 科学通报, 50(19): 2145-2154
宋述光, 张立飞, Niu Y., 等. 2004. 青藏高原北缘早古生代板块构造演化和大陆深俯冲. 地质通报, 23(9-10): 918-925
宋友桂, 方小敏, 李吉均, 等. 2000. 六盘山东麓朝那剖面红粘土年代及其构造意义. 第四纪研究, 20(5): 457-463
宋友桂,方小敏,李吉均,等. 2001. 晚新生代六盘山隆升过程初探. 中国科学(D 辑), 31(增刊): 142-148
孙洪艳, 李志祥, 田明中. 2003. 第四纪测年研究新进展. 地质力学学报, 9(4): 371-378
孙连浦, 马永生, 郭彤楼, 等. 2005. 十万大山盆地中生代沉积充填特征及其演化. 世界地质, 24(1): 30-35
孙素英. 1982. 宁夏同心地区渐新世孢粉组合. 中国地质科学院地质研究所所刊, 4: 127-138
孙知民, 杨振宇, 葛肖虹, 等. 2004. 柴达木盆地西北缘古近系磁性年代研究进展. 地质通报, 23(9-10): 899-902
谭利华, 杨景春, 段烽军. 1998.河西走廊新生代构造运动的阶段划分. 北京大学学报(自然科学版), 34(4): 523-532
唐领余和汪世兰. 1988. 青海共和盆地共和组抱粉植物群. 古生物学报, 27(5): 583- 606
汪泽成, 刘和甫, 熊宝贤, 等. 2001. 从前陆盆地充填地层分析盆山耦合关系. 地球科学——中国地质大学学报, 26(1): 33-39
王伴月, 邱占祥, 王晓鸣, 等. 2003. 甘肃省党河地区的新生代地层和青藏高原隆升. 古脊椎动物学报, 41(1): 66-75
王伴月, 阎志强, 陆俊彦, 等. 1994. 宁夏海原两个中期哺乳动物群的发现. 古脊椎动物学报, 32(4): 285-296
王成善, 刘志飞, 王国芝, 等. 2000. 新生代青藏高原三维古地形再造. 成都理工学院学报, 27(1): 1-7
王成善, 朱利东, 刘志飞. 2004. 青藏高原北部盆地构造沉积演化与高原向北生长过程. 地球科学进展, 19(3): 373-381
王成善和丁学林. 1998. 青藏高原隆升研究新进展综述. 地球科学进展, 13(6): 526-532
王崇孝, 马国福, 周在华. 2005. 酒泉盆地中、新生代构造演化及沉积充填特征. 石油勘探与开发, 32(1):33-42
王二七, 孟庆任, 陈智, 等. 2001. 龙门山断裂带印支期左旋走滑运动及其大地构造成因. 地学前缘(中国地质大学,北京), 8(2): 376-384
王二七. 2004. 山盆耦合的一种重要形式:造山带及其侧陆盆地. 科学通报, 49(4): 370-374
王峰, 王驹, 范洪海, 等. 2005. 甘肃北山旧井地区晚第四纪活动断裂分布及其构造意义. 地质论评, 51(3): 250-258
王红亮, 邓宏文, 孙德军, 等. 2000. 准噶尔盆地南缘层序地层特征与有利含气区带预测. 石油实验地质, 22(4): 336-340
王萍和王增光. 1997. 阿拉善活动块体的划分和归宿. 地震, 17(1): 103-112
王清晨, 李忠. 2003. 盆山耦合与沉积盆地成因. 沉积学报, 21(1): 24-30
王双绪, 张希, 张四新, 等. 2005. 青藏高原东北缘现今构造变动与地震活动特征. 地球学报, 26(3): 209-216
王训练. 1999. 露头层序地层学研究的几个基本理论问题. 中国科学(D 辑), 29(1): 22-30
王永, 李德贵, 王彦斌, 等. 2000. 西天山两侧前陆盆地晚新生代沉积特征及构造意义. 新疆地质, 18(3): 254-251
吴孔友, 查明, 王绪龙, 等. 2005. 准噶尔盆地构造演化与动力学背景再认识. 地球学报, 26(3): 217-222
吴因业, 宋岩, 贾承造, 等. 2005. 柴北缘地区层序格架下的沉积特征. 地学前缘(中国地质大学(北京),北京大学),12(3): 105-112
吴玉书. 2001. 甘肃灵台雷家河地区中新世晚期-上新世早期孢粉植物群. 植物学报, 43(7): 750-756
伍杨洋和冯军. 2003. 前陆盆地研究进展. 新疆石油地质, 24(1): 87-91
夏邦栋, 张开均, 孔庆友, 等. 1999. 青藏高原内部三条磨拉石带的确定及其构造意义. 地学前缘, 6(3): 173-177
夏林圻, 夏祖春, 徐学义. 1995. 北祁连山构造-火山岩浆演化动力学. 西北地质科学, 16(1): 1-28
向芳, 王成善, 朱利东. 2002. 青藏高原南缘新生代磨拉石的沉积特征. 成都理工学院学报, 29(5): 515-519
向树元, 喻建新, 王国灿, 等. 2005. 东昆仑阿拉克湖盆地1.85～1.58MaBP间植被演替及高原隆升启示. 海洋地质与第四纪地质, 25(5): 47-53
肖爱芳, 黎敦朋, 张汉军, 等. 2003. 新疆库木库里盆地渐新-上新统孢粉组合特征与古气候演变. 陕西地质, 21(1): 36-44
肖序常, 王军, 苏犁, 等. 2003. 再论西昆仑库地蛇绿岩及其构造意义. 地质通报, 22(10): 745-750
谢富仁, 舒塞兵, 窦素芹, 等. 2000. 海原、六盘山断裂带至银川断陷第四纪构造应力场分析. 地震地质, 22(2): 139-146
徐建明, 杨振京, 郑宏瑞, 等. 2003. 塔里木盆地第四纪磁性地层学研究. 地层学杂志, 27(4): 276-281
徐强, 廖仕孟, 朱永刚, 等. 2000. 川西龙门山前陆盆地中砂砾质楔形体的定量统计. 沉积与特提斯地质, 20(4): 31-37
徐仁, 陶君容, 孙湘君, 等. 1973. 希夏邦马峰高山栎化石层的发现及其植物学和地质学上的意义. 植物学报, 15(1): 103-119
许效松, 徐强. 1996. 盆山转换和当代盆地分析中的新问题. 岩相古地理,16(2): 24-33
许志琴, 杨经绥, 姜枚, 等. 1999. 大陆俯冲及青藏高原周缘造山带的崛起. 地学前缘, 6(3): 139-152
许志琴, 曾令森, 杨经绥, 等. 2004. 走滑断裂、“挤压性盆—山构造”与油气资源关系的探讨. 地球科学——中国地质大学学报, 29(6): 631-643
许志琴, 张建新, 许慧芬, 等. 1997. 中国主要大陆山链韧性剪切带及动力学. 北京:地质出版社, 28-211
许忠淮和石耀霖. 2003. 岩石圈结构与大陆动力学. 地震学报, 25(5): 512-527
薛祥煦, 李虎侯, 李永项, 等. 2004. 秦岭中更新世以来抬升的新资料及认识. 第四纪研究, 24(1): 82-87
闫小熊和周立发. 2001. 前陆盆地层序地层学研究现状及进展. 沉积与特提斯地质, 21(3): 60-64
闫臻, 方爱民, 潘裕生, 等. 2005. 西藏达金砾岩沉积环境、有孔虫时代及其大地构造意义. 自然科学进展, 15(5): 565-571
杨东, 方小敏, 宋友桂, 等. 2002. 六盘山西侧山麓剥蚀面的发育与新构造隆升. 沉积学报, 20(2): 282-287
杨明慧和刘池洋. 2000. 中国中西部类前陆盆地特征及含油气性. 石油与天然气地质,21(1): 46-49
杨振京, 刘志明, 张俊牌, 等. 2001. 银川盆地中更新世以来的孢粉记录及古气候研究. 海洋地质与第四纪地质, 21(3): 43-49
殷鸿福和童金南. 1995. 层序地层界面与年代地层界线的关系. 科学通报, 40(6): 539-541
尹安. 2001. 喜马拉雅-青藏高原造山带地质演化——显生宙亚洲大陆生长. 地球学报, 22(3): 193-230
余辉龙, 邓宏文, 胡勇. 2002. 从古地磁资料看柴达木盆地古构造环境. 石油勘探与开发, 29(6): 41-44
袁宝印和王振海. 1995. 青藏高原隆起与黄河地文期. 第四纪研究, 4: 353-359
袁道阳, 张培震, 刘百篪, 等. 2004. 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. 地质学报, 78(2): 271-278
岳乐平, Heller F., 邱占祥, 等. 2000. 兰州盆地第三系磁性地层年代与古环境记录. 科学通报, 45(18): 1998-2003
岳乐平, 李智佩, 朱桦, 等. 2002. 全球气候变化、青藏高原隆升与中国北方荒漠化. 地球学报, 23(增刊): 45-50
曾宜君, 杨学俊, 李云泉, 等. 2004. 川西前陆盆地南部中新生代砾岩的构造意义. 四川地质学报, 24(4): 198-201
曾允孚, 覃建雄. 1999. 沉积学发展现状与前瞻. 成都理工学院学报,26(1): 1-7
詹艳, 赵国泽, 王继军, 等. 2005. 青藏高原东北缘海原弧形构造区地壳电性结构探测研究. 地震学报, 27(4): 431-440
张柏桥, 胡望水, 舒志国, 等. 2004. 六盘山盆地与酒西盆地中新生代构造对比. 江汉石油学报, 26(1): 11-14
张波, 张进江, 杨武玲, 等. 2005. 我国中西部前陆盆地归属及其含油气性评述. 高校地质学报, 11(1): 126-136
张光亚和薛良清. 2002. 中国中西部前陆盆地油气分布与勘探方向. 石油勘探与开发,29(1): 1-5
张广良, 张培震, 陈杰. 2006,逆冲-褶皱造山过程中生长地层和生长不整合的识别及意义. 地震地质, 2
张国伟, 郭安林, 刘福田, 等. 1996. 秦岭造山带三维结构及其动力学分析. 中国科学(D), 26(增刊): 1-6
张国伟, 张本仁, 袁学诚, 等. 2001. 秦岭造山带与大陆动力学. 北京: 科学出版社, 421-727
张国伟,张宗清,董云鹏. 1995. 秦岭造山带主要构造岩石地层单元的构造性质及其大地构造意义. 岩石学报, 11(2): 102-114
张建新, 许志琴, 徐慧芬, 等. 1998. 北祁连加里东期俯冲-增生楔结构及动力学. 地质科学, 33(3): 290-299
张进, 马宗晋, 任文军, 等. 2004a. 鄂尔多斯西缘逆冲褶皱带构造特征及其南北差异的形成机制. 地质学报, 78(5): 600-611
张进, 马宗晋, 任文军, 等. 2004b. 宁夏中南部古生代弧型构造. 大地构造与成矿学, 28(1): 29-37
张进, 马宗晋, 任文军. 2005. 宁夏中南部新生界沉积特征及其与青藏高原演化的关系. 地质学报, 79(6): 757-773
张珂, 刘开瑜, 吴加敏, 等. 2004. 宁夏中卫盆地的沉积特征及其所反映的新构造运动. 沉积学报, 22(3): 465-473
张明利, 金之钧, 汤良杰, 等. 2002. 前陆盆地研究的回顾与展望. 地质论评, 48(2): 214-220
张培震, 邓起东, 杨晓平, 等. 1996. 天山的晚新生代构造变形及其地球动力学问题. 中国地震,12(2): 127-140
张培震, 沈正康, 王敏, 等. 2004. 青藏高原及周边现今构造变形的运动学. 地震地质, 26(3): 365-368
张培震, 王敏, 甘卫军, 等. 2003. GPS 观测的活动断裂滑动速率及其对现今大陆动力作用的制约. 地学前缘,10(3): 81-92
张培震, 王琪, 马宗晋. 2002. 中国大陆现今构造运动大的 GPS 速度场与活动地块. 地学前缘, 9(2): 430-441
张旗, 郭原生, 王岳明, 等. 1997. 祁连山地区镁铁-超镁铁岩的多样性. 地球科学进展, 12(5): 324-330
张旗, 王焰, 钱青. 2000. 北祁连早古生代洋盆是裂陷槽还是大洋盆?——与葛肖虹讨论. 地质科学, 35(1): 121-158
张青松,李炳元,景可. 1981. 青藏地区上新世古地理与高原隆起.见.青藏高原隆起的时代、幅度和形式问题. 北京:科学出版社,26-35
张清志, 陈智梁, 刘宇平, 等. 2005. 青藏高原及其东南前陆地壳运动的 GPS 监测. 地球物理学进展, 20(2): 524-527
张希明. 2001. 塔里木盆地中新生代沉积演化特征. 新疆地质, 19(4): 246-250
张行. 2001. 甘肃临夏盆地中新世地层及哺乳动物化石. 兰州大学学报(自然科学版), 37(2): 123-130
张一勇. 1995. 中国早第三纪孢粉植物群纲要. 古生物学报, 34(2): 212-227
张永志, 王卫东, 祝意青, 等. 2004. 青藏高原东北侧断层活动引起的地壳三维变形与重力场变化研究. 地
球学报, 25(5): 583-586
张岳桥, 陈正乐, 杨农. 2001. 阿尔金断裂晚新生代左旋走滑位错的地质新证据. 现代地质, 15(1): 8-12
张岳桥, 杨农, 陈文, 等. 2003. 中国东西部地貌边界带晚新生代构造变形历史与青藏高原东缘隆升过程初
步研究. 地学前缘(中国地质大学,北京), 10(4): 599-612
张招崇, 毛景文, 杨健民, 等. 1998. 北祁连山西段中元古代蛇绿岩的发现及其意义. 矿物岩石地球化学通报, 17(2): 114-118
张振法, 李超英, 牛颖智. 1997. 阿拉善-敦煌陆块的性质/范围及其构造作用和意义. 内蒙古地质, 81(2): 1-14
张振法. 1997. “北山晚华力西地槽褶皱带”(西阿拉善)的性质/归属及有关问题探讨. 内蒙古地质, 84(1): 24-40
张正涛和张永志. 2005. GPS 观测研究青藏东北缘的水平变形特征. 测绘和空间地理信息, 28(3): 6-8
赵培坤和纪有亮. 2005. 鄂尔多斯西缘前陆盆地上古生界沉积相特征研究. 新疆地质, 23(2): 152-158
赵生贵. 1996. 祁连造山带特征及其构造演化. 甘肃地质学报, 5(1): 16-29
赵志军, 方小敏, 李吉均, 等. 2001. 酒泉砾石层的古地磁年代与青藏高原隆升. 科学通报, 46(14): 1208-1212
郑德文, 张培震, 万景林, 等. 2005. 六盘山盆地热历史的裂变径迹证据. 地球物理学报, 48(1): 157-164
郑德文, 张培震, 万景林,等. 2003. 青藏高原东北边缘晚新生代构造变形的时序—临夏盆地碎屑颗粒磷灰石裂变径迹记录. 中国科学(D 辑), 33(增刊): 190-198
郑洪波, Botcher K. and Powell C. 2002a. 新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升—I 地层学与岩石学证据. 沉积学报, 20(2): 274-281
郑洪波, Botcher K. and Powell C. 2003. 新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升-Ⅱ沉积相与沉积盆地演化. 沉积学报, 21(1): 46-51
郑洪波, 陈惠中, 靳鹤龄, 等. 2002b. 上新世—早更新世青藏高原北缘隆升的磁性地层学证据. 海洋地质与第四纪地质, 22(2): 57-62
郑洪波, 黄湘通, 刘锐, 等. 2005. 晚中新世以来亚洲季风阶段性演化的海陆记录. 矿物岩石地球化学通报, 24(2): 103-109
郑洪波. 2002. 从新疆叶城剖面砂岩和砾岩组分看西昆仑山的剥蚀历史. 地质力学学报, 8(4): 297-305
郑民, 孟自芳, 李相博, 等. 2005. 陆内前陆盆地的复合动力演化研究——以库车陆内前陆盆地为例. 新疆石油天然气, 1(1): 12-16
中国岩石圈动力学概论编委会. 1991. 中国岩石圈动力学概论. 北京: 地震出版社, 144-155
钟大赉和丁林. 1996. 青藏高原隆起过程及其机制探讨. 中国科学(D 辑), 26(4): 289-295
钟巍, 李吉均, 方小敏. 2001. 临夏盆地晚新生代沉积特征与青藏高原隆升. 新疆大学学报(理工版), 18(4): 401-407
周鼎武, 董云鹏, 华洪, 等. 1996. “磨拉石建造”和“不整合”在地层对比中的意义. 地质论评, 42(5): 416-423
周江羽, 王江海, 尹安, 等. 2002. 青藏东北缘早第三纪盆地充填的沉积型式及构造背景—以囊谦和下拉秀盆地为例. 沉积学报, 20(1): 85-91
朱大岗, 孟宪刚, 邵兆刚, 等. 2004. 西藏阿里札达盆地上新世—早更新世沉积相及其构造演化特征. 地质力学学报, 10(3): 245-252
朱弟成, 潘桂棠, 莫宣学, 等. 2004. 印度大陆和欧亚大陆的碰撞时代. 地球科学进展, 19(4): 564-571
朱利东, 王成善, 伊海生, 等. 2004. 青藏高原盆地系统演化与高原形成时间. 成都理工大学学报:自然科学版,31(3): 249-255
朱筱敏, 康安, 康强. 2005. 柴达木盆地第四纪底界时代及识别标志. 西安石油大学学报(自然科学版),20(5): 1-5
朱筱敏, 康安, 王贵文. 2003. 陆相坳陷型和断陷型湖盆层序地层样式探讨. 沉积学报, 21(2): 283-287
朱筱敏, 王贵文, 李滨阳, 等. 2002. 开鲁盆地陆西凹陷下白垩统层序地层学和油气评价. 沉积学报, 20(4): 532-567
左国朝, 吴茂炳, 毛景文, 等. 1999. 北祁连西段早古生代构造演化史. 甘肃地质学报, 8(1): 6-13
左国朝和吴汉泉. 1997. 北祁连中段早古生代双向俯冲碰撞造山模式剖析. 地球科学进展, 12(4): 315-332
An Zhisheng, Kutzbach J. E., Prell W. L., et al. 2001. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibet plateau since late Miocene times. Nature, 411: 62-66
Arne D., Worley B., Wilson C., et al. 1997. Differential exhumation in response to episodic thrusting along the eastern margin of the Tibetan Plateau. Tectonophysics, 280: 239-256
Baker D.M., Robert J.L., Johnson G.D., et al. 1988. Development of the Himalayan frontal thrust zone: Salt Range, Pakistan. Geology, 16: 3-7
Beck R.A., Burbank D.W., Sercombe W.J., et al. 1995. Stratigraphic evidence for an early collision between northwest India and Asia. Nature, 373: 55-57
Bookhagen B., Thiede R.C. and Strecker M.R. 2005. Abnormal monsoon years and their control on erosion and sediment flux in the high, arid northwest Himalaya. Earth and Planetary Science Letters, 108:1-11
Bullen M.E. 2003. Late Cenozoic tectonic evolution of the Kyrgyz Range and adjoining Chu Basin: New age constraints from fission-track, U-Th/He, and magnetostratigraphy. The Paper of Master of Science, 1-55
Bullen M.E., Burbank D.W., and Garver J.I., et al. 2003. Building the northern Tien Shan: Integrated thermal, structural, and topographic constraints. J. Geol., 111: 149-165
Burbank D.W. 1992. Cause of recent Himalayan uplift deduced from deposited patterns in the Ganges basin. Nature, 357: 680-683
Burbank D.W., McLean J.K., Bullen M.E., et al. 1999. Partitioning of intermontane basins by thrust-related folding, Tien Shan, Kyrgyzstan. Basin Research , 11: 75-92
Burbank D.W., Richard A.B., Thomas M., et al. 1996. The Himalayan foreland basin. In: An Yin, Mark Harrison, ed. The Tectonic Evolution of Aisa, 149-188
Burchfiel B. C., Chen Z., Liu Y., et al.1997. Tectonics of the Longmen Shan and adjacent regions, central China, Intern. Geological Review, 37(8): 661~735.
Burchfiel B.C., Deng Q., Molnar P., et al. 1989. Intracrustal detachment zones of continental deformation. Geology, 17: 448-452
Burchfiel B.C., Zhang P., Wang Y., et al. 1991. Geology of Haiyuan fault zone, Ningxia-Hui Autonomous Region, China, and its relation to the evolution of the northeastern margin of the Tibetan plateau, Tectonics, 10: 1091-1110
Calabro R.A., Corrado S., Di Bucci D., et al. 2003. Thin-skinned vs. thick-skinned tectonics in the Matese Massif, Central–Southern Apennines (Italy). Tectonophysics, 377(3-4): 269-297
Cande S. C. and kent D. V. 1995. Revised calibration of geomagnetic polaryity time scale for the late Creaceous and Cenozoic.J.G.R., 100: 6093-6095
Catuneanu O. 2004. Retroarc foreland systems––evolution through time. Journal of African Earth Sciences, 38(3): 225-242
Chen Jie, Burbank D.W., Scharer K.M., et al. 2002. Magnetochronology of the upper Cenozoic strata in the Southwestern Chinese Tian Shan: rates of Pleistocene folding and thrusting. Earth and Planetary Science Letters, 195: 113-130
Chen Jie, Lu Yanchou, Ding Guoyu.1998.Quaternary tectonic deformation in Jiuxi Basin, west Qilianshan Mountain, northwestern China. Journal of Earthquake Prediction Research, (7):510~522
Chen Yan, Wu Hanning, Courtillot V., et al. 2002. Large N–S convergence at the northern edge of the Tibetan plateau? New Early Cretaceous paleomagnetic data from Hexi Corridor, NW China. J. Earth and Planetary Science Letters, 201(2): 293-307
Coleman M, Hodges K. 1995. Evidence for Tibetan Plateau uplift before 14Myr ago from a new minimum age for east-west extension. Nature, 374:49-52
Currie B. 1997. Sequence stratigraphy of nonmarine Hurassic-Cretaceous rocks, central Cordilleran foreland basin system. GSA Bulletin, 109(9): 1206-1222
Dahlen F.A. 1990. Critical taper model of fold-and-thrust belts and accretionary wedges. Annual Review of Earth and Planetary Sciences, 18: 55-99
Darby B. J., Ritts B. D., Yue Yongjun, et al. 2005. Did the Altyn Tagh fault extend beyond the Tibetan Plateau? Earth and Planetary Science Letters, 240(2): 425-435
Decelles P.D., Gehrels G.E., Quade J., et al. 1998. Neogene foreland basin deposits, erosional unroofing, and the kinematic history of the Himalayan fold-thrust belt, western Nepal. Geol. Soc. Ame. Bulletin, 1:2-21
DeCelles P.G. and Giles P.A. 1996. Foreland basin systems. Basin Res., 8: 105-123
DeCells P.G. 1994. Late Cretaceous-Paleocene synorogenic sedimentation and kinematic history of the Sevier thrust belt, northeast Utah and southwest Wyoming. GSA Bulletin, 106: 32-56
DeCells P.G. and Currie B.S. 1996. Long-term sediment accumulation in the Middle Jurassic-Early Eocene Cordilleran retroarc foreland-basin system. Geology, 24(7):591-594
DeCells P.G.. and Gehrels G.E. 1998. Eocene-Early Miocene foreland basin development and the history of Himalayan thrusting western and central Nepal. Tectonics, 17(5): 741-765
DeCells P.G.. and Giles K.A. 1996. Foreland basin systems. Basin Research, 8: 105-123
DeCells P.G.., Mitra G. 1995. History of the Sevier orogenic wedge interns of critical taper models, northeast Utah and southwest Wyoming. Geological Society of America Bulletin, 107: 454-462
Dettman, D.L. Fang, X., Garzione, C.N., et al. 2003. Uplift-driven climate change at 12Ma: a long δ18O record from the NE margin of the Tibetan plateau. Earth Planet. Sci. Lett., 214:267-277
Dewey J. F. 1988. Extensional collapse of orogens. Tectonics, 7(6): 1123-1139
Dewey J. F. and Burke K.C. 1973. Tibetan, Variscan and Precambrian basement reactivation:Products of continental collision, Journal of Geology, 81:683-692
Dewey J. F., Holdsworth R. E., Strachan R.A. 1998. Transpression and transtension zones. In:Holdsworth,R.E., Strachan,R.A. and Deway, J. F. (eds) 1998. Continental teanspressional and transtensional tectonics. Geological Society, London, Special Publications, 135:15-33
Dewey J.F., Shackleton R.M.,常承法,等. 1990. 青藏高原的构造演化. 青藏高原地质演化, 北京: 科学出版社, 384-415
Dupont-Nivet G., Butler R.F., Yin A., et al. 2002. Paleomagnetism indicates no Neocene rotation of the Qaidam Basin in northern Tibet during Indo-Asian collision, Geology, 30(3): 263-266
Dupont-Nivet G., Horton B.K., Butler R.F., et al. 2004. Paleogene clockwise tectonicrotation of the Xining -Lanzhou region, Northeastern Tibetan Plateau, J. Geophys. Res., 109(B04401): 1-13
Eji Uba C., Heubeck C.and Hulka C. 2005. Facies analysis and basin architecture of the Neogene Subandean synorogenic wedge, southern Bolivia. Sedimentary Geology, 180(3-4): 91-123
England P. and Molnar P. 1990. Right-lateral shear and rotation as explanation for strike-slip fauting in eastern Tibet. Nature, 1990, 344(6262): 140-142
England P. and Molnar P. 1997. The field of crustal velocity in Asia calculated from Quaternary rates of slip on faults. Geophys. J. Int., 130: 551-582
England P. and Molnar. P. 1990. Surface uplift, uplift of rocks, and exhumation of rocks. Geology, 18: 1173-1177
England P.C. and G.A.Houseman. 1985. Role of lithospheric strength heterogeneities in the tectonics of Tibet and neighbouring regions. Nature, 315(6017): 297-301
England P.C. and G.A.Houseman. 1988. The mechnics of the Tibetan Plateau, Phil. Trans. R. Soc. Lond. A., 326: 301-320
Fang Xiaomin, Carmala G., Van der V.R., et al. 2003. Flexural subsidence by 29 Ma on the NE edge of Tibet from the magnetostratigraphy of Linxia Basin, China. Earth and Planetary Science Letters, 210: 545-560
Fang, X. M., Yan M.D., Van der Voo R., et al., 2005. Late Cenozoic deformation and uplift of the NE Tibetan Plateau: evidence from high-resolution magnetostratigraphy of the Guide Basin, Qinghai Province, China. Geol. Soc. Am. Bull., 117:1208-1225
Fisher R.A. 1953. Dispersion on a sphere. Proc R Soc London, Ser A, 217: 295-305
Flesch L.M., Haines A.J., Holt W.E. 2003. Dynamics of the India-Eurasia collision zone. J. Geophys. Res., 106: 16435-16460
Fu Bihong, Awata Y., Du Jianguo, et al. 2005. Late Quaternary systematic stream offsets caused by repeated large seismic events along the Kunlun fault, northern Tibet. Geomorphology, 71(3-4): 278-292
Gao Cunhai. 2004. Sedimentary facies changes and climatic-tectonic controls in a foreland basin, the Urumqi River, Tian Shan, Northwest China. Sedimentary Geology, 169(1-2): 29-46
Garzione C.N., Dettaman D.L., Quade J., et al. 2000. high times on the Tibetan plateau: paleoelevation of the Thakkhola garben, Nebal. Geology, 28(4): 339-342
Gaudemer Y., Tapponnier P., Meyer B., et al. 1995. Partitioning of crustal slip between linked, active faults in the eastern Qilian Shan, and evidence for a major seismic gap, The ‘Tianzhu gap’, on the western Haiyuan Fault, Gansu(China). Geophys. J. Int., 120: 599-645
Gautam P. and Rosler W. 1999. Depositional chronology and fabric of Siwalik group sediments in Central Nepal from magnetostratigraphy and magnetic anisotropy. Journal of Asian Earth Sciences, 17(5-6): 659-682
George A.D., Marshallsea S.J., Wyrwoll K.H., et al. 2001. Miocene cooling in the northern Qilian Shan, northeastern margin of the Tibetan Plateau, revealed by apatite fission-track and vitrinite-reflectance analysis. Geology, 29: 939-942
Ghiglione M.C. and Ramos V.A. 2005. Progression of deformation and sedimentation in the southernmost Andes. Tectonophysics, 405(1-4): 25-46
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. G. R., 106(B12): 30505-30521
Golonka J. 2004. Plate tectonic evolution of the southern margin of Eurasia in the Mesozoic and Cenozoic. Tectonophysics, 381(1-4): 235-273
Gonzalez-Bonorino G. and Kraemer G.P. 2001. Andean Cenozoic foreland basins: a review. Journal of South American Earth Sciences, 14(7): 651-654
Greb S.F., Eble C. F. and Chesnut D. R. 2002. Comparison of the Eastern and Western Kentucky coal fields (Pennsylvanian), USA—why are coal distribution patterns and sulfur contents so different in these coal fields? International Journal of Coal Geology, 50(1-4): 89-118
Halim N., Cogne J.P., Chen Y., et al. 1998. New cretaceous and Early Tertiary Paleomagnetic results from xining-lanzhou basin, Kunlun and Qiangtang Blocks, China: Implications on the Geodynamic evolution of Asia. J. G. R., 103(B9): 21025-21045
Harrison T. M., Lovera O. M., Grove M. 1997. New insights into the origin of two contrasting Himalayan granite belts. Geology, 25(10):899-902
Harrison T.M., Yin A., Grove M. et al. 2000. The Zedong Window: A record of superposed Tertiary convergence in southeastern Tibet, JGR, 105(B8):19211-19230
Harrison, T.M., Copeland P., Kidd W.S.F., et al. 1992. Raising Tibet. Science, 255: 1663-1670
Hendrix M.S., Dumitru T.A., Graham S. A. 1994. Late Oligocene-early Miocene uprooting in the Chinese Tian Shan : An early effect of the India-Asia collision. Geology, 22: 487-490
Holt W.E., Chamot-Rooke N., Le Pichon X., et al. 2000. Velocity field in Aisa inferred from Quaternary fault slip rates and Global Positioning System observations. J. Geophys. Res., 105: 19185-19209
Homewood P., Allen P.A., Williams G.D. 1986. Foreland basins: An introduction. In: Allen P.A., Homewood P. ed. Foreland basin. International Association of Sedimentologists Special Publication 8, 3-12
Horton B.K., Dupont-Nivet J., Zhou G..L., et al. 2004. Mesozoic-Cenozoic evolution of the Xining, Minhe and Dangchang basins, northeastern Tibetan Plateau: Magnetostratigraphic and biostratigraphic results. Journal of Geophysical Research, 109(B04402): 1-15
Houseman G. and England P. 1993. Crustal thickening versus lateral expulsion in the India-Asian continental collision. J. Geophys. Res., 98: 12233-12249
Huang B. C., Wang Y. C., Liu T., et al. 2004. Paleomagnetism of Miocene sediments from the Turfan Basin, Northwest China: no significant vertical-axis rotation during Neotectonic compression within the Tian Shan Range, Central Asia. Tectonophysics, 384(1-4): 1-21
Jackson J. 2003. Strength of the continental lithosphere: time to abandon the jelly sandwich? GSA Today, 12(9): 4-10
Jain V. and Sinha R. 2004. Fluvial dynamics of an anabranching river system in Himalayan foreland basin, Baghmati river, north Bihar plains, India. Geomorphology, 60(1-2): 147-170
Jiang M., Galve A., Hirn A., et al. 2006. Crustal thickening and variations in architecture from the Qaidam basin to the Qang Tang (North–Central Tibetan Plateau) from wide-angle reflection seismology. Tectonophysics, 412(3-4): 121-140
Johnson N.M., Opdyke N.J., Johnson G.D., et al. 1982. Magnetic polarity stratigraphy and ages of Siwalik Group rocks of the Potwar Plateau, Pakistan. Palaeogeography, Palaeoclimatology, Palaeoecology, 37:17-42
Jolivet J., Brunel M., Seward D., et al. 2001. Mesozoic and Cenzoic tectonics of the northern edge of the Tibetan plateau: fission-track constraints. Tectonophysics, 343: 111-134
Jolivet M., Brunel M., Seward D., et al. 2001. Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan plateau: fission-track constraints. Tectonophysics, 343(1-2): 111-134
Jordan T.A. and Watts A.B. 2005. Gravity anomalies, flexure and the elastic thickness structure of the India–Eurasia collisional system. Earth and Planetary Science Letters, 236(3-4): 732-750
Kimura H., Azmy K., Yamamuro M., et al. 2005. Integrated stratigraphy of the upper Neoproterozoic succession in Yunnan Province of South China: Re-evaluation of global correlation and carbon cycle. Precambrian Research, 138(1-2): 1-36
Kirby E., Whipple K.X., Tang W.,et al. 2003. Distribution of active rock uplift along the eastern margin of the Tibetan Plateau: Inferences from bedrock channel longitudinal profiles. J.Geophys.Res., 108(B4):2217, doi: 10.1029/2001JB000861
Kirschvink J.L. 1980. The least-squares line and plane and the analysis of paleomagnetic data. Geophys J R Astron Soc, 62: 699-718
Kletetschka G. and Wasilewski P.J. 2002. Grain size limit for SD hematite. Physics of The Earth and Planetary Interiors, 129(1-2): 173-179
Koroteev V.A., Necheukhin, V.M. and Sazonov, V.N. 1997. Geodynamic setting of the mineral deposits of the Urals. Tectonophysics. 276(1-4): 291-300
Krishna K. S., Bull J. M., Scrutton R.A. 2001. Evidence for multiphase folding of the central Indian Ocean lithosphere. Geology, 29(8):715-718
Kumaravel V., Sangode S.J., Siddaiah N.S., et al. 2005. Rock magnetic characterization of pedogenesis under high energy depositional conditions: A case study from the Mio–Pliocene Siwalik fluvial sequence near Dehra Dun, NW Himalaya, India. Sedimentary Geology, 177(3-4): 229-252
Kusky T.M. and Li Jianghai. 2003. Paleoproterozoic tectonic evolution of the North China Craton. Journal of Asian Earth Sciences, 22(4): 383-397
Lacassin R., Valli F., Arnaud N., et al. 2004. Large-scale geometry, offset and kinematic evolution of the Karakorum fault, Tibet. Earth and Planetary Science Letters, 219(3-4): 255-269
Larrasoana, J.C., Murelaga, X. and Garces, M. 2006. Magnetobiochronology of Lower Miocene (Ramblian) continental sediments from the Tudela Formation (western Ebro basin, Spain). Earth and Planetary Science Letters, 243(3-4):409-423
Lasserre C., Gaudemer Y., et al. 2002. Fast late Pleistocene slip rate on the Lenglongling segment of the Haiyuan fault,Qinghai,China. Journal of Geophysical Research, 107(B11):2276
Lasserre C., Morel P.H., Gaudemer Y. et al. 1999. Postglacial left slip rate and post occurrence of M>=8 earthquakes on the western Haiyuan fault, Gansu, China. Journal of Geophysical Research, 104(B8): 17633-17651
Leech M.L., Singh S., Jain A.K., et al. 2005. The onset of India–Asia continental collision: Early, steep subduction required by the timing of UHP metamorphism in the western Himalaya. Earth and Planetary Science Letters, 234(1-2): 83-97
Lehmkuhl F. and Haselein F. 2000. Quaternary paleoenvironmental change on the Tibetan Plateau and adjacent areas (Western China and Western Mongolia). Quaternary International, 65-66: 121-145
Li Youli, Yang Jingchun, Tan Lihua, et al. 1999. Impact of tectonics on alluvial landforms in the Hexi Corridor, Northwest China. Geomorphology, 28(3-4): 299-308
Lin Aimin, Yang Zhengyu, Sun Zhiming, et al. 2001. How and when did the Yellow River develop its square bend? Geology, 29(10): 951-954
Liu Shaofeng, Steel R.and Zhang Guowei. 2005. Mesozoic sedimentary basin development and tectonic implication, northern Yangtze Block, eastern China: record of continent–continent collision. Journal of Asian Earth Sciences, 25(1): 9-27
Liu Z.,C. Wang. 2001. Facies analysis and depositinal systems of Cenozoic sediments in the Hoh Xil basin, northern Tibet. Sedimentary Geology, 140:251-270
Liu Zhifei and Wang Chengshan. 2001. Facies analysis and depositional systems of Cenozoic sediments in the Hoh Xil basin, northern Tibet. Sedimentary Geology, 140(3-4): 251-270
Mankinen E. A. and Dalrymlie G. B. 1979. Revised geomagnetic polarity time scale for interval 0.5m.y.BP, J.G.R., 1979, 84: 615-626
Marques F. O.and Cobbold P. R. 2002. Topography as a major factor in the development of arcuate thrust belts: insights from sandbox experiments. Tectonophysics, 348(4): 247-268
McFadden P.L. 1990. A new fold test for paleomagnetic studies. Geophys J Int,103: 163-169
Meissner R., Rabbel W. and Kern H. 2006. Seismic lamination and anisotropy of the Lower Continental Crust. Tectonophysics, 416(1-4): 81-99
Metivier F., Gaudemer Y., Tapponnier P., et al. 1998. Northastward growth of the Tibet plateau deduced from balanced reconstruction of two deposional areas: The Qaidam and Hexi corridor basins, China. Tectonics, 17(6):823-842
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. Geophys. J. Int., 135: 1-47
Molanar P., Burchfiel B.C., Lian K., et al. 1987. Geomorphic evidence for active faulting in the Altyn Tagh and northern Tibet and qualitative estimates of its contribution to the convergence of India and Eurasia. Geology, 15:245-253
Molar P., Tapponnier P. 1975. Cenozoic tectonics of Asia: Effects of a continental collision. Science, 189: 419-426
Molnar P. 1986. The Geologic History and structure of the Himalaya. American Scientist, 74: 144-154
Molnar P. 1988. Continental tectonics in the aftermath of plate tectonics. Nature, 335(6186): 131-137
Molnar P. 2004. Late Cenozoic increase in accumulation rates of terrestrial sediment: How might climate change have affected erosion rates? Ann. Rev. Earth Planet. Sci., 32: 67-89
Molnar P. and England P. 1990. Late Cenozoic uplift of mountain ranges and global climate change: chicken or egg? Nature, 346: 29-33
Molnar P.,England P.,Martinod J.1993. Mantle dynamics,uplift of the Tibet plateau, and the Indian monsoon. Rev. Geophys, 31: 357-396
Molnar, P., 2005. Mio-Pliocene Growth of the Tibetan Plateau and Evolution of East Asian Climate. Palaeontologia Electronica, 8(1): 1-23
Morrill C., Overpeck J. T., Cole J. E., et al. 2006. Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet. Quaternary Research, Volume 65(2): 232-243
Mukhopadhyay D.K.and Mishra P. 2005. A balanced cross section across the Himalayan frontal fold-thrust belt, Subathu area, Himachal Pradesh, India: thrust sequence, structural evolution and shortening. Journal of Asian Earth Sciences, 25(5):735-746
Mukul M. 2000. The geometry and kinematics of the Main Boundary Thrust and related neotectonics in the Darjiling Himalayan fold-and-thrust belt, West Bengal, India. Journal of Structural Geology, 22(9): 1261-1283
Myrow P. M., Hughes N. C., Paulsen T. S., et al. 2003. Integrated tectonostratigraphic analysis of the Himalaya and implications for its tectonic reconstruction. Earth and Planetary Science Letters, 212(3-4): 433-441
Najman Y. 2006. The detrital record of orogenesis: A review of approaches and techniques used in the Himalayan sedimentary basins. Earth-Science Reviews, 74(1-2): 1-72
Pares, J.M., Van der Voo, R., Downs, R.W., et al. 2003. Northeastward growth and uplift of the Tibetan Plateau: Magnetostratigraphic insights from the Guide Basin. J. Geophys. Res., 108:1-11
Peltzer G. and P. Tapponnier, 1989. Armijo R. Magnitude of late Quaternary left-lateral displacements along the northern edge of Tibet. Science, 246:1285-1289
Peltzer G. and Tapponnier P. 1988. Formation and evolution of strike-slip faults, rifts,and basins during the India-Asia collision: an experimental approach, Journal of Geophysical research, 93(B12): 15085-15117
Piedilato S. and Prosser G. 2005. Thrust sequences and evolution of the external sector of a fold and thrust belt: An example from the Southern Apennines (Italy). Journal of Geodynamics, 39(4): 386-402
Qiang X. K., Li Z. X., Powell C. McA., et al. 2001. Magnetostratigraphic record of the Late Miocene onset of the East Asian monsoon, and Pliocene uplift of northern Tibet. Earth and Planetary Science Letters, 187(1-2): 83-93
Quade J., Cerling T. E., Bowman J.R. 1989. Development of Aasian monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan. Nature, 342(9): 163-166
Raza S. M., Cheema I. U., Downs W. R., et al. 2002. Miocene stratigraphy and mammal fauna from the Sulaiman
Range, Southwestern Himalayas, Pakistan. Palaeogeography, Palaeoclimatology, Palaeoecology, 186(3-4): 185-197
Royden L.H., Burchfiel B.C., King R.C., et al. 1997. Surface deformation and lower crustal flow in eastern Tibet. Science, 276: 788-790
Sanyal P., Bhattacharya S. K., Kumar R., et al. 2004. Mio–Pliocene monsoonal record from Himalayan foreland basin (Indian Siwalik) and its relation to vegetational change. Palaeogeography, Palaeoclimatology, Palaeoecology, 205(1-2): 23-41
Scharer K. M., Burbank D. W., Chen J., et al. 2004. Detachment folding in the Southwestern Tian Shan–Tarim foreland, China: shortening estimates and rates. Journal of Structural Geology, 26(11): 2119-2137
Sciesciani V. Calamita F. Tavarnelli E., et al. 2001. Foreland-dipping normal faults in the inner edges of syn-orogenic basin: a case from the Central Apennines, Italy. Tectonophysics, 330: 211-224
Shi Yafeng. 2002. Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia. Quaternary International, 97-98: 79-91
Singh B. P. 2003. Evidence of growth fault and forebulge in the Late Paleocene (57.9–54.7 Ma), western Himalayan foreland basin, India. Earth and Planetary Science Letters, 216(4): 717-724
Sissingh W. 2001. Tectonostratigraphy of the West Alpine Foreland: correlation of Tertiary sedimentary sequences, changes in eustatic sea-level and stress regimes. Tectonophysics, 333(3-4): 361-400
Sobel E. R., and Dumitru T.A. 1997. Exhumation of the margins of the western Tarim Basin during the Himalayan orogeny. J. Geophys. Res., 102: 5043-5064
Sobel E.R., Hilley G.E., and Strecker M.R. et al. 2003. Formation of internally drained contractional basins by aridity-limited bedrock incision. Journal of Geophysical Research, 108(B7): 2344, doi:10.1029/2002JB001883
Sobel E.R., Trevor A.D. 1997. Thrusting and exhumation around the margins of the weatern Tarim basin during the India-Asia collision. Journal of Geophysical Research, 102(B3): 5043-5063
Speranza F., Adamoli L., Maniscalco R., et al. 2003. Genesis and evolution of a curved mountain front: paleomagnetic and geological evidence from the Gran Sasso range (central Apennines, Italy). Tectonophysics, 362(1-4): 183-197
Sun Jimin, Zhu Rixiang and An Zhisheng. 2005. Tectonic uplift in the northern Tibetan Plateau since 13.7 Ma ago inferred from molasse deposits along the Altyn Tagh Fault. Earth and Planetary Science Letters, 235(3-4): 641-653
Sun Zhiming, Yang Zhenyu, Pei Junling, et al. 2005. Magnetostratigraphy of Paleogene sediments from northern Qaidam Basin, China: Implications for tectonic uplift and block rotation in northern Tibetan plateau. Earth and Planetary Science Letters, 237(3-4): 635-646
Sun Zhiming, Yang Zhenyu, Pei Junling, et al. 2006. New Early Cretaceous paleomagnetic data from volcanic and red beds of the eastern Qaidam Block and its implications for tectonics of Central Asia. Earth and Planetary Science Letters, 243(1-2):268-281
Suppe J., Chou T. and Stephen C. 1992. Rate of folding and faulting determined from growth strata. In: McClay K. R. Ed. Thrust Tectonics, New York: Chapman and Hall, 105-122.
Tapponnier P. and Molnar P. 1976. Slip-line field theoory and large-scale continental tectonics. Nature, 264(5584):319-324
Tapponnier P., B. Meyer, J.P. Avouac et al. 1993. Active thrusting and folding in the Qi Lian Shan, and decoupling between upper crust and mantle in northeastern Tibet.Earth and Planetary science Letters, 97:382-403
Tapponnier P., Ryerson F.J., Woerd J.V., et al. 2001a. Long-term slip rates and characteristic slip: keys to active fault behavior and earthquake hazard. Earth and Planetary Sciences, 333: 483-494
Tapponnier P., Xu Zhiqin, Francoise R., et al. 2001b. Oblique stepwise rise and growth of the Tibet Plateau. Science, 294: 1671-1677
Vincent S.J. and Allen M.B. 1999. Evolution of the Minle and Chao shui Basins,China:Implications for Mesozoic strike-slip basin formation in Central Asia. GSA Bulletin, 111(5): 725-742
Wang E. 1997. Displacement and timing along the northern strand of the Altyn Tagh fault zone, Northern Tibet. Earth and Planetary Science Letters, 150:55-64
Wang R. L., Scarpitta S. C., Zhang S. C., et al. 2002. Later Pleistocene/Holocene climate conditions of Qinghai–Xizhang Plateau (Tibet) based on carbon and oxygen stable isotopes of Zabuye Lake sediments. Earth and Planetary Science Letters, 203(1): 461-477
Williams H., Turner S., Kelley S., et al. 2001. Age and composition of dikes in Southern Tibet: New constraints on the timing of east-west extension and its relationship to postcollisional volcanism. Geology, 29(4):339-342
Willis B. J. and Behrensmeyer A. K. 1995. Fluvial systems in the Siwalik Miocene and Wyoming Paleogene. Palaeogeography, Palaeoclimatology, Palaeoecology, 115(1-4): 13-35
Wu Yongqiu, Cui Zhijiu, Liu Gengnian, et al. 2001. Quaternary geomorphological evolution of the Kunlun Pass area and uplift of the Qinghai-Xizang (Tibet) Plateau. Geomorphology, 36(3-4): 203-216
Yamada K., Fukusawa, Fang H., Pan X.M., et al. 1999. High-resolution multi-proxy records of Asian monsoon activities from terrestrial sediments over the last 75,000 years. Chin. Sci. Bull., 44 (Suppl. 1): 223-229
Yan Maodu, VanderVoo R., Fang Xiao-min, et al. 2006. Paleomagnetic evidence for a mid-Miocene clockwise rotation of about 25° of the Guide Basin area in NE Tibet. Earth and Planetary Science Letters, 241(1-2): 234-247
Yin A. and Harrison. M.T. 2000. Geologic Evolution of the Himalayan-Tibetan Orogen. Annu. Rev. Earth Planet. Sci. , 2000, 28: 211-28
Yin A., Nie S., Harrison T. M., et al. 1998. Lateozoic tectonic evolution of the southern Chinese Tinshan. Tectonic,17:1-27
Yin An, Rumelhart P.E., Butler R., et al. 2002. Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation. GSA Bulletin, 114(10): 1257-1295
Yin An. 2006. Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation. Earth-Science Reviews, In Press
Yue Yongjun, Graham S. A., Ritts B. D., et al. 2005. Detrital zircon provenance evidence for large-scale extrusion along the Altyn Tagh fault. Tectonophysics, 406(3-4): 165-178
Zachos, J. C., Pagani M., Sloan L., et al. 2001. Trends, rhythms, and aberrations in global climate 65 Ma to Present, Science, 292: 686-693
Zhang P.Z, Shen Z.K., Burgman R., et al. 2004. Continuous deformation of the Tibetan Plateau constrained from Global Positioning measurements. Geology, 32(9): 809-812
Zhang P.Z., Burchfiel B.C., Molnar P., et al. 1990. Late Cenozoic tectonic evolution of southern Ningxia, northeastern margin of Tibetan Plateau. Bull. Geol. Soc. Am., 102: 1484-1498
Zhang P.Z., Burchfiel B.C., Molnar P., et al. 1991a. Rate, amount, and style of late Cenozoic deformation of southern Ningxia, northeastern margin of Tibetan Plateau. Tectonics, 10: 1111-1129
Zhang P.Z., Molnar P. and Downs W. et al. 2001. Increased sedimentation rates and grainsizes 2-4 Myr ago due to the influence of climate changes on erosion rates. Nature, 410: 891-897
Zhang P.Z., Burchfiel B.C., Molnar P., et al. 1991b. Later Cenozoic tectonic evolution of the Ningxia Hui Autonomous Region, China. GSA Bulletin, 102:1484-1498
Zhang Y., Vergely P. and Mercier J. 1995. Active faulting in and along the Qinling Range (China) inferred from spot imagery analysis and extrusion tectonics of south China. Tectonophysics, 243: 69-95
Zhang Yueqiao, Ma Yinsheng, Yang Nong, et al. 2003. Cenozoic extensional stress evolution in North China. Journal of Geodynamics, 36(5): 591-613
Zhang Zhenke, Wang Sumin, Yang Xiangdong, et al. 2004. Evidence of a geological event and environmental change in the catchment area of the Yellow River at 0.15 Ma. Quaternary International, 117(1): 35-40
Zhou Jianxun, Xu Fengyin, Wang Tiecheng, et al. 2006. Cenozoic deformation history of the Qaidam Basin, NW China: Results from cross-section restoration and implications for Qinghai–Tibet Plateau tectonics. Earth and Planetary Science Letters, 243(1-2): 195-210
曹国强, 陈世悦, 徐凤银, 等. 2005. 柴达木盆地西部中-新生代沉积构造演化. 中国地质,32(1): 33-40
柴炽章,焦德成,张维歧.1997.天景山断裂带晚第四纪水平活动强度的分时、分段研究.中国地震,13(1):35-42
常承法, 郑锡澜. 1973. 中国西藏南部珠穆朗玛地区地质构造特征及其青藏高原东西向诸山系形成的探讨. 中国科学(D), 2: 190-201
陈发景,汪新文,张光亚等. 1996. 中国中、新生代前陆盆地的构造特征和地球动力学. 地球科学,21(4):366-372
陈发景和汪新文. 1997. 中国中、新生代含油气盆地成因类型、构造体系及地球动力学模式. 现代地质,11(4):409-424
陈建华和田景春. 2000. 层序地层学的产生、现状与展望. 复式油气田, 2: 9-12
陈杰, 卢演俦, 丁国瑜. 1996. 祁连山西段及酒西盆地区第四纪构造运动的阶段划分. 第四纪研究, 3:265-271
陈杰, 卢演俦, 丁国瑜. 2001. 塔里木西缘晚新生代造山过程的记录——磨拉石建造及生长地层和生长不整合. 第四纪研究, 21(6): 528-539
陈杰, 卢演俦. 2001. 中国西部前陆盆地生长不整合、生长地层与构造变形. 卢演俦, 高维明, 等主编, 新构造与环境. 北京: 地震出版社, 407-421
陈杰, 尹金辉, 曲国胜, 等. 2000. 塔里木盆地西缘西域组的底界、时代、成因与变形过程的初步研究. 地震地质, 22(增刊): 104-116
陈杰,卢演俦. 2001. 中国西部前陆盆地生长不整合、生长地层与构造变形.卢演俦,高维明等主编:新构造与环境,北京:地震出版社,407-421
陈诗越, 王苏民, 沈吉. 2003. 青藏高原中部错鄂湖晚新生代以来的沉积环境演变及其构造隆升意义. 湖泊科学, 15(1): 21-27
陈书平, 汤良杰, 张一伟. 2001. 前陆、前陆盆地和前陆盆地系统. 世界地质, 20(4): 332-338
陈宣华, Yin An, Gehrels G. E., 等. 2004. 青藏高原北缘阿尔金东段中生代南北向伸展作用. 地质力学学报, 10(3): 193-212
陈正乐, 万景林, 王小风, 等. 2002. 阿尔金断裂带 8Ma 的快速走滑及其地质意义. 地球学报, 23(4): 295-300
陈正乐, 王小凤, 冯夏红, 等. 2003. 青藏高原北缘山脉隆升时间的同位素证据. 吉林大学学报(地球科学版), 33(3): 270-275
崔效锋, 谢富仁, 赵建涛. 2005. 中国及邻区震源机制解的分区特征. 地震地质, 27(2): 298-307
崔之久, 伍永秋, 刘耕年, 等. 1997. 昆仑-黄河运动的发现及其性质. 科学通报, 42(18): 1986-1989.
崔之久, 伍永秋, 刘耕年, 等. 1998. 关于“昆仑-黄河运动”. 中国科学(D), 28(1): 53-59
戴霜, 方小敏, 宋春晖, 等. 2005. 印度-欧亚板块碰撞在高原北部的早期响应. 科学通报,50(7): 673-683
邓宏文, 王红亮, 阎伟鹏, 等. 2004. 河流相层序地层构成模式探讨. 沉积学报, 22(3): 373-379
邓宏文, 王洪亮, 翟爱国, 等. 1999. 中国陆源碎屑盆地层序地层与储层展布. 石油与天然气地质, 20(2): 108-114
邓晋福, 苏尚过, 赵海玲, 等. 2003. 华北地区燕山期岩石圈减薄的深部过程. 地学前缘(中国地质大学,北京), 10(3): 41-50
邓平, 舒良树, 谭正中, 等. 2003 华南中、新生代盆地地球动力学背景. 华南铀矿地质, 20(1): 1-17
邓起东, 张培震, 冉勇康, 等. 2003. 中国活动构造基本特征. 中国科学(D 辑), 32(12): 1020-1030
邓涛, 王晓鸣, 倪喜军, 等. 2004. 临夏盆地的新生代地层及其哺乳动物化石证据. 古脊椎动物学报, 42(1): 45-66
邓涛. 2004. 临夏盆地晚新生代哺乳动物群演替与青藏高原隆升背景. 第四纪研究, 24(4): 413-420
邓万明. 2003. 青藏及邻区新生代火山活动及构造演化. 地震地质, 25(增刊): 51-61
丁林, 钟大赉, 刘福田, 等. 2000. 造山带岩石层多向层架构造及其对新生代岩浆活动制约——以三江及邻区为例. 中国科学(D), 30(增刊): 1-8。
丁林,钟大赉,潘裕生等. 1995. 东西马拉雅构造结上新世以来快速抬升的裂变径迹证据. 科学通报,40(16):1479-1500。
董国榜, 陈云, 吴锡浩, 等. 1999. 中国更新世环境巨变的孢粉植物群记录. 地质力学学报, 5(4): 11-21
董冶平, 雷芳, 申秀荣,等. 2003. 西秦岭北缘断裂带的深部构造特征及其与地震活动的关系.内陆地震, 10(3): 224-234
杜远生, 张哲, 周道华, 等. 2002. 北祁连—河西走廊志留纪和泥盆纪古地理及其对同造山过程的沉积响应. 古地理学报, 4(4): 1-8
杜远生, 朱杰, 韩欣, 等. 2004. 从弧后盆地到前陆盆地——北祁连造山带奥陶纪-泥盆纪的沉积盆地与构造演化. 地质通报, 23(9-10): 911-917
段志明, 李勇, 李亚林, 等. 2005. 青藏高原北部温泉活动沉积盆地的沉积特征及其地质意义. 沉积与特提斯地质, 25(1-2): 181-188
范马洁, 宋春晖. 2003. 青藏高原东北缘临夏盆地王家山地区沉积环境分析与构造隆升. 兰州大学学报, 39(3): 84-89
方爱民, 阎臻, 刘小汉, 等. 2005. 藏南柳区砾岩中古植物化石组合及其特征. 古生物学报, 44(3): 435-445
方世虎, 郭召杰, 张志诚, 等. 2004. 天山北缘前陆冲断带形成时间的地层学证据. 新疆地质, 22(1): 24-28
方小敏, 李吉均, 马玉贞, 等. 1998. 青藏高原(以临夏盆地为主)天然剖面记录. 施雅风、李吉均和李炳元主编,青藏高原晚新生代隆升与环境变化. 广州: 广东科技出版社, 19-48
方小敏, 赵志军, 李吉均, 等. 2004. 祁连山北缘酒西盆地晚新生代磁性地层与高原隆升. 中国科学(D 辑), 34(2): 97-106
方小敏,李吉均,朱俊杰, 等. 1995. 临夏盆地中心王家山剖面磁性地层与构造事件. 见:见青藏高原形成演化、环境变迁与生态系统研究学术论文年刊(1994),北京: 科学出版社
方小敏,李吉均,朱俊杰, 等. 1997. 甘肃临夏盆地新生代地层绝对年龄测定与划分. 科学通报, 42(14):1457-1471
方小敏,宋春晖,高军平, 等. 2003. 青藏高原东北边缘晚新生代哺乳动物化石的磁性地层学. 科学通报, 47(23): 1824-1828
方小敏和李吉均. 1998. 3.4 百万年来青藏高原隆升的阶段性与环境演变. 施雅风、李吉均和李炳元主编, 青藏高原晚新生代隆升与环境变化. 广州: 广东科技出版社. 394-414
冯益民. 1997. 祁连造山带研究概况, 历史, 现状及展望. 地球科学进展, 12(4): 307-314
冯有良, 周海民, 李思田, 等. 2004. 陆相断陷盆地层序类型与构造特征. 地质论评, 50(1): 43-49
符超峰, 方小敏, 宋友桂, 等. 2005. 盆山沉积耦合原理在定量恢复造山带隆升剥蚀过程中的应用. 海洋地质与第四纪地质,25(1): 105-112
甘肃省地质矿产局. 1989. 甘肃省区域地质志. 北京: 地质出版社
高长林, 叶德燎, 钱一雄. 2000. 前陆盆地的类型及油气远景. 石油实验地质, 22(2): 99-104
高红山, 潘保田, 邬光剑, 等. 2004. 祁连山东段剥蚀面与青藏高原隆升. 冰川冻土, 26(5): 540-544
高星, 王卫民, 姚振兴. 2005. 中国及邻近地区地壳结构. 地球物理学报, 48(3): 591-601
葛肖虹, 刘俊来. 1999. 北祁连造山带的形成与背景. 地学前缘, 6(4): 223-230
顾家裕, 张兴阳. 2005. 中国西部陆内前陆盆地沉积特征与层序格架. 沉积学报,23(2): 187-193
国家地震局地质研究所, 宁夏回族自治区地震局. 1990. 海原活动断裂带. 北京: 地震出版社, 1-286
韩建恩, 余佳, 孟庆伟, 等. 2005. 西藏阿里地区札达盆地第四纪砾石统计及其意义. 地质通报, 24(7): 630-636
何登发,李德生,吕修祥. 1996. 中国西北地区含油气盆地构造类型. 石油学报,17( 4):8-18
何光玉, 卢华复, 杨树锋, 等. 2004. 库车中新生代盆地沉降特征. 浙江大学学报(理学版), 21(1): 110-113
侯明才, 陈洪德, 田景春. 2003. 层序充填动力学——层序地层研究的新方向. 地层学杂志, 27(4): 358-364
侯明才, 伊海生, 刘与安, 等. 2002. 测老庙盆地层序地层格架与其幕式构造演化. 地球学报, 23(1): 63-66
胡见义,赵文智,钱凯等. 1996. 中国西北地区石油天然气地质基本特征. 石油学报,17(3):1-11
胡玲, 何登发, 胡道功. 2005. 准噶尔盆地南缘霍尔果斯-玛纳斯-吐谷鲁断裂晚新生代构造变形的 ESR 测年证据. 地球学报, 26(2): 121-126
黄宝春, Yo-Ichiro O, 杨振宇, 等. 2000. 河西走廊和阿拉善东缘地区中寒武世古地磁研究的初步结果. 地球物理学报, 43(3): 393-401
黄华芳,彭作林,卢伟, 等. 1993. 酒西盆地、酒东盆地第三系磁性地层的划分与对比. 甘肃地质学报, 2(1): 6-16
黄继钧. 2000. 羌塘盆地性质及构造演化. 地质力学学报, 6(1): 58-66
黄立功, 钟建华, 郭泽清, 等. 2004. 阿尔金造山带中、新生代的演化. 地球学报, 25(3): 287-294
吉让寿, 刘光祥, 潘文蕾, 等. 2003. 试论前陆-伸展盆地. 石油实验地质, 25(增刊): 539-542
吉让寿,钱一雄,范小林等. 2000. 中国西北地区中生代盆地与油气. 西安:西安地图出版社,239
贾承造, 何登发, 陆洁民. 2004. 中国喜马拉雅运动的期次及其动力学背景. 石油与天然气地质, 25(2): 121-169
蒋晓玮, 王江海, 张会化. 2003. 西秦岭断裂走滑与盆地的耦合——西秦岭—松甘块体新生代向东走滑挤出的证据. 地学前缘(中国地质大学,北京), 10(3): 207-208
靳久强. 1997. 中国中西部前陆盆地的油气勘探. 石油勘探与开发,24(5):11-14
康来迅. 1990. 西秦岭北缘断裂带晚更新世晚期以来断裂运动的基本特征及运动机理. 中国地震, 6(3): 53-61
赖绍聪, 秦江锋, 李永飞. 2005. 青藏北羌塘新第三纪玄武岩单斜辉石地球化学. 西北大学学报(自然科学版),35(5): 611-615
雷振宇,何登发,张朝军. 2001. 中国中西部类前陆盆地与典型前陆盆地类比及其油气勘探前景. 地球学报,22(2): 169-174
李才, 翟明国, 程立人, 等. 2005. 青藏高原羌塘地区几个关键地质问题的思考. 地质通报, 24(4): 295-301
李春昱,刘仰文,朱宝清,等. 1978. 秦岭及祁连山构造发展史. 西北地质科技情报,4: 1-12
李大荣. 2004. 陆相层序地层学研究新进展. 江汉石油学报, 14(2): 13-17
李德威. 2003. 青藏高原隆升机制新模式. 地球科学——中国地质大学学报, 28(6): 593-600
李奋其, 王成善, 朱利东, 等. 2002. 区域挤压体制下盆-山耦合关系探讨——以河西走廊和北祁连山为例. 沉积与特提斯地质, 22(4): 17-25
李吉均, 方小敏, 马海洲, 等. 1996. 晚新生代黄河上游地貌演化与青藏高原隆起. 中国科学(D), 26(4): 316-322
李吉均, 方小敏, 潘保田, 等. 2001. 新生代晚期青藏高原强烈隆起及其对周边环境的影响. 第四纪研究, 21(5): 381-391
李吉均, 方小敏, 朱俊杰, 等. 1995. 临夏盆地新生代地层古地磁年代与模式序列. 见: 青藏项目专家委员会编, 青藏高原形成演化、环境变迁与生态系统研究学术论文年刊(1994). 北京: 科学出版社, 41-54
李吉均, 施雅风, 方小敏, 等. 1998. 青藏高原晚新生代隆生与环境变化. 广东科技出版社
李吉均, 文世宣, 张青松, 等. 1979. 青藏高原隆起的时代、幅度和形式的探讨. 中国科学, 6: 608-616
李吉均. 1999. 青藏高原的地貌演化与亚洲季风. 海洋地质与第四纪地质, 19(1): 1-11
李吉均和方小敏. 1998. 青藏高原隆起与环境变化研究. 科学通报, 43(15): 1569-1574
李继亮, 肖文交, 闫臻. 2003. 盆山耦合与沉积作用. 沉积学报, 21(1): 52-60
李江海, 牛向龙, 陈征, 等. 2004. 太行山区深层次推覆构造的发现及其地质意义. 自然科学进展, 14(10): 1118-1127
李前裕, 郑洪波, 钟广法, 等. 2005. 南海晚渐新世滑塌沉积指示的地质构造事件. 地球科学——中国地质大学学报, 30(1): 19-24
李儒峰, 马永生, 汤良杰, 等. 2004. 云南楚雄盆地波动特征及构造沉积演化. 地球科学-中国地质大学学报, 29(3): 309-316
李双泉. 2005. 潮水盆地与酒西盆地中新生代构造对比. 天然气地球科学, 16(4): 464-468
李双应, 岳书仓, 王道轩, 等. 2002. 大别造山带北缘中生代地层格架厘定. 地层学杂志, 26(3): 178-186
李喜臣, 王永, 丁孝忠. 2005. 西昆仑山前晚新生代磨拉石时代及意义. 地质力学学报,11(2): 181-186
李向东和王克卓. 2000. 塔里木盆地西南及邻区特提斯格局和构造意义. 新疆地质, 18(2): 113-120
李孝泽, 董光荣, 陈惠中, 等. 2001. 从青藏高原南北两个磨拉石削面的对比看青藏高原的隆升过程. 中国沙漠, 21(4): 354-360
李勇, 曹叔尤, 周荣军, 等. 2005. 晚新生代岷江下蚀速率及其对青藏高原东缘山脉隆升机制和形成时限的定量约束. 地质学报, 79(1): 28-37
李勇, 侯中健, 司光影, 等. 2002. 青藏高原东缘新生代构造层序与构造事件. 中国地质, 29(1): 30-36
李勇, 王成善, 伊海生, 等. 2001. 青藏高原中侏罗世 —早白垩世羌塘复合型前陆盆地充填模式. 地层学杂志, 19(1): 20-27
李勇, 王成善, 伊海生. 2002. 中生代羌塘前陆盆地充填序列及演化过程. 地层学杂志, 26(1): 62-67
李勇, 王成善, 曾允孚, 等. 2000. 造山作用与沉积响应. 矿物岩石, 20(2): 49-56
李勇和孙爱珍. 2000. 龙门山造山带构造地层学研究. 地层学杂志, 24(3): 202-206
李云通, 孙秀玉, 王大宁, 等. 1984. 中国地层(13)——中国的第三系. 北京: 地质出版社, 1-362.
梁忠和邓涛. 2005. 甘肃临夏盆地晚中新世大唇犀化石的年龄结构与生活环境. 古脊椎动物学报, 43(3): 219-230
刘朝露, 贾承造, 夏斌, 等. 2005. 塔东地区盆山耦合与油气成藏模式研究. 天然气地球科学,16(5): 552-558
刘池洋, 赵红格, 王锋, 等. 2005. 鄂尔多斯盆地西缘(部)中生代构造属性. 地质学报, 79(6): 737-745
刘池洋, 赵红格, 杨兴科, 等. 2002. 前陆盆地及其确定和研究. 石油与天然气地质, 23(4): 307-313
刘德民和李德威. 2002. 造山带与沉积盆地的耦合——以青藏高原周边造山带与盆地为例. 西北地质, 35(1): 15-21
刘耕武. 1996. 青藏高原东部地区晚新生代孢粉组合特征及其古地理意义. 微体古生物学报, 13(4): 363-372
刘和甫, 李晓青, 刘立群, 等. 2004. 走滑构造体系盆山耦合与区带分析. 现代地质, 18(2): 139-150
刘和甫, 汪泽成, 熊保贤, 等. 2000. 中国中西部中、新生代前陆盆地与挤压造山带耦合分析. 地学前缘(中国地质大学学报,北京), 7(3): 55-72
刘和甫. 1995. 前陆盆地类型及褶皱-冲断层样式. 地学前缘(中国地质大学, 北京), 2(3-4): 59-68
刘和甫. 2000. 盆山耦合类型. 地学前缘,7(4 ):469
刘和甫. 2001. 盆地—山岭耦合体系与地球动力学机制. 地球科学——中国地质大学学报, 26(6): 582-596
刘少峰, 李思田, 庄新国, 等. 1996. 鄂尔多斯西南缘前陆盆地沉降和沉降过程模拟. 地质学报, 70(1): 12-22
刘树根, 罗志立, 赵锡奎, 等. 2005. 试论中国西部陆内俯冲型前陆盆地的基本特征. 石油与天然气地质, 26(1): 37-48
刘志飞, 王成善, 金玮, 等. 2004. 可可西里盆地早渐新世雅西措群爬升沙纹层理及其沉积环境意义. 沉积学报, 22(4): 560-565
刘志宏, 卢华复, 李西建, 等. 2000. 库车再生前陆盆地的构造演化. 地质科学, 35(4): 482-492
柳益群, 李文厚, 冯乔. 1997. 鄂尔多斯盆地东部上三叠统含油砂岩的古地温及成岩阶段. 地质学报, 71(1): 65-74
吕连清,方小敏,鹿化煜,等. 2004. 青藏高原黄土末次冰期千年尺度冬季风变化的粒度记录. 科学通报, 49:1091-1098
罗开平和范小林. 2004. 河西走廊及邻区中新生代成盆背景与盆地原型. 石油实验地质, 26(5): 432-436
罗志立, 李景明, 李小军, 等. 2004. 中国前陆盆地特征及含油气远景分析. 石油地质, 2: 1-11
马华东和扬子江. 2003. 塔里木盆地西南新生代盆地演化特征. 新疆地质, 21(1): 92-95
马钦忠, 李吉均. 2003. 晚新生代青藏高原北缘构造变形和剥蚀变化及其与山脉隆升关系. 海洋地质与第四纪地质, 23(1): 27-34
马寅生, 施炜, 张岳桥, 等. 2005. 东昆仑活动断裂带玛曲段活动特征及其东延. 地质通报, 24(1): 30-35
马玉贞, 李吉均, 方小敏. 1998. 临夏地区 30.6-5.0Ma 红层孢粉植物群与气候演化记录. 科学通报, 43(3): 301-304
毛明陆, 刘池洋. 1995. 河西走廊东部晚古生代前陆盆地演化特征. 甘肃地质学报, 4(2): 55-61
聂军胜, 宋春晖, 方小敏, 等. 2002. 贵德盆地黄河出现的古地磁年代及其意义. 海洋地质与第四纪地质, 23(2): 59-64
宁夏回族自治区地质局. 1990. 宁夏回族自治区地质志. 北京: 地质出版社, 47-85
宁夏回族自治区地质矿产局. 1996. 宁夏回族自治区岩石地层(全国地层多重划分和对比 64). 北京: 中国地质大学出版社, 1-32
潘安定. 1998. 临夏东山顶剖面的第四纪孢粉记录及其古环境研究. 海洋地质与第四纪地质, 18(1): 89-96
潘安定. 2000. 青藏高原东北边缘第四纪孢粉记录的环境意义(英文). 微体古生物学报, 17(2): 178-185
潘保田, 高红山, 李炳元, 等. 2004. 青藏高原层状地貌与高原隆升. 第四纪研究, 24(1): 50-58
潘裕生, 汪一鹏, 常承法. 1980. 喜马拉雅板块活动证据兼论青藏高原形成模式. 地震地质, 2(2): 1-9
潘裕生. 1999. 青藏高原的形成与隆升. 地学前缘(中国地质大学,北京), 6(3): 153-163
裴先治, 吴汉泉, 左国朝. 1999. 北祁连早古生代俯冲杂岩带的变形特征与构造演化. 西安工程学院学报, 21(1): 9-17
钱方. 1999. 青藏高原晚新生代磁性地层研究. 地质力学学报, 5(4): 22-34
钱祥麟. 2004. 新生代板内造山作用研究——认识中国区域地质构造基本特征的关键. 地学前缘(中国地质大学,北京), 11(3): 221-225
邱瑞照, 邓晋福, 周肃, 等. 2005. 青藏高原西部蛇绿岩类型:岩石学与地球化学证据. 地学前缘(中国地质大学,北京,北京大学), 12(2): 277-291
邱占祥, 王伴月, 邓涛. 2004. 甘肃临夏盆地牙沟的哺乳动物化石及有关地层问题. 古脊椎动物学报, 42(4): 276-296
任收麦, 葛肖虹, 刘永江, 等. 2004. 晚白垩世以来沿阿尔金断裂带的阶段性走滑隆升. 地质通报, 23(9-10): 926-932
任战利, 肖晖, 刘丽, 等. 2005. 沁水盆地新生代抬升冷却事件的确定. 石油与天然气地质, 26(1): 109-113
申旭辉, 田勤俭, 丁国瑜, 等. 2001. 宁夏贺家口子地区晚新生代地层序列及其构造意义. 中国地震, 17(2): 156-166
沈正康, 王敏, 甘卫军, 等. 2003. 中国大陆现今构造应变率场及其动力学成因研究. 地学前缘(中国地质大学,北京), 10(增刊): 307-313
施雅风, 李吉均, 李炳元, 等. 1999. 晚新生代青藏高原的隆升与东亚环境变化. 地理学报, 54(1): 10-21
施雅风和刘东生. 1964. 希夏邦马峰地区科学考察报告.科学通报,10: 928-938
舒良树, 郭召杰, 朱文斌, 等. 2004. 天山地区碰撞后构造与盆山演化. 高校地质学报,10(3): 393-404
宋春晖, 方小敏, 高军平, 等. 2001a. 青藏高原东北部贵德盆地新生代沉积演化与构造隆升. 沉积学报, 19(4): 493-500
宋春晖, 方小敏, 李吉均, 等. 2001b. 青藏高原北缘酒西盆地 13Ma 以来沉积演化与构造隆升. 中国科学(D辑), 31(增刊): 155-162
宋春晖, 高东林, 方小敏, 等. 2005. 青藏高原昆仑山垭口盆地晚新生代高精度磁性地层及其意义. 科学通报, 50(19): 2145-2154
宋述光, 张立飞, Niu Y., 等. 2004. 青藏高原北缘早古生代板块构造演化和大陆深俯冲. 地质通报, 23(9-10): 918-925
宋友桂, 方小敏, 李吉均, 等. 2000. 六盘山东麓朝那剖面红粘土年代及其构造意义. 第四纪研究, 20(5): 457-463
宋友桂,方小敏,李吉均,等. 2001. 晚新生代六盘山隆升过程初探. 中国科学(D 辑), 31(增刊): 142-148
孙洪艳, 李志祥, 田明中. 2003. 第四纪测年研究新进展. 地质力学学报, 9(4): 371-378
孙连浦, 马永生, 郭彤楼, 等. 2005. 十万大山盆地中生代沉积充填特征及其演化. 世界地质, 24(1): 30-35
孙素英. 1982. 宁夏同心地区渐新世孢粉组合. 中国地质科学院地质研究所所刊, 4: 127-138
孙知民, 杨振宇, 葛肖虹, 等. 2004. 柴达木盆地西北缘古近系磁性年代研究进展. 地质通报, 23(9-10): 899-902
谭利华, 杨景春, 段烽军. 1998.河西走廊新生代构造运动的阶段划分. 北京大学学报(自然科学版), 34(4): 523-532
唐领余和汪世兰. 1988. 青海共和盆地共和组抱粉植物群. 古生物学报, 27(5): 583- 606
汪泽成, 刘和甫, 熊宝贤, 等. 2001. 从前陆盆地充填地层分析盆山耦合关系. 地球科学——中国地质大学学报, 26(1): 33-39
王伴月, 邱占祥, 王晓鸣, 等. 2003. 甘肃省党河地区的新生代地层和青藏高原隆升. 古脊椎动物学报, 41(1): 66-75
王伴月, 阎志强, 陆俊彦, 等. 1994. 宁夏海原两个中期哺乳动物群的发现. 古脊椎动物学报, 32(4): 285-296
王成善, 刘志飞, 王国芝, 等. 2000. 新生代青藏高原三维古地形再造. 成都理工学院学报, 27(1): 1-7
王成善, 朱利东, 刘志飞. 2004. 青藏高原北部盆地构造沉积演化与高原向北生长过程. 地球科学进展, 19(3): 373-381
王成善和丁学林. 1998. 青藏高原隆升研究新进展综述. 地球科学进展, 13(6): 526-532
王崇孝, 马国福, 周在华. 2005. 酒泉盆地中、新生代构造演化及沉积充填特征. 石油勘探与开发, 32(1):33-42
王二七, 孟庆任, 陈智, 等. 2001. 龙门山断裂带印支期左旋走滑运动及其大地构造成因. 地学前缘(中国地质大学,北京), 8(2): 376-384
王二七. 2004. 山盆耦合的一种重要形式:造山带及其侧陆盆地. 科学通报, 49(4): 370-374
王峰, 王驹, 范洪海, 等. 2005. 甘肃北山旧井地区晚第四纪活动断裂分布及其构造意义. 地质论评, 51(3): 250-258
王红亮, 邓宏文, 孙德军, 等. 2000. 准噶尔盆地南缘层序地层特征与有利含气区带预测. 石油实验地质, 22(4): 336-340
王萍和王增光. 1997. 阿拉善活动块体的划分和归宿. 地震, 17(1): 103-112
王清晨, 李忠. 2003. 盆山耦合与沉积盆地成因. 沉积学报, 21(1): 24-30
王双绪, 张希, 张四新, 等. 2005. 青藏高原东北缘现今构造变动与地震活动特征. 地球学报, 26(3): 209-216
王训练. 1999. 露头层序地层学研究的几个基本理论问题. 中国科学(D 辑), 29(1): 22-30
王永, 李德贵, 王彦斌, 等. 2000. 西天山两侧前陆盆地晚新生代沉积特征及构造意义. 新疆地质, 18(3): 254-251
吴孔友, 查明, 王绪龙, 等. 2005. 准噶尔盆地构造演化与动力学背景再认识. 地球学报, 26(3): 217-222
吴因业, 宋岩, 贾承造, 等. 2005. 柴北缘地区层序格架下的沉积特征. 地学前缘(中国地质大学(北京),北京大学),12(3): 105-112
吴玉书. 2001. 甘肃灵台雷家河地区中新世晚期-上新世早期孢粉植物群. 植物学报, 43(7): 750-756
伍杨洋和冯军. 2003. 前陆盆地研究进展. 新疆石油地质, 24(1): 87-91
夏邦栋, 张开均, 孔庆友, 等. 1999. 青藏高原内部三条磨拉石带的确定及其构造意义. 地学前缘, 6(3): 173-177
夏林圻, 夏祖春, 徐学义. 1995. 北祁连山构造-火山岩浆演化动力学. 西北地质科学, 16(1): 1-28
向芳, 王成善, 朱利东. 2002. 青藏高原南缘新生代磨拉石的沉积特征. 成都理工学院学报, 29(5): 515-519
向树元, 喻建新, 王国灿, 等. 2005. 东昆仑阿拉克湖盆地1.85～1.58MaBP间植被演替及高原隆升启示. 海洋地质与第四纪地质, 25(5): 47-53
肖爱芳, 黎敦朋, 张汉军, 等. 2003. 新疆库木库里盆地渐新-上新统孢粉组合特征与古气候演变. 陕西地质, 21(1): 36-44
肖序常, 王军, 苏犁, 等. 2003. 再论西昆仑库地蛇绿岩及其构造意义. 地质通报, 22(10): 745-750
谢富仁, 舒塞兵, 窦素芹, 等. 2000. 海原、六盘山断裂带至银川断陷第四纪构造应力场分析. 地震地质, 22(2): 139-146
徐建明, 杨振京, 郑宏瑞, 等. 2003. 塔里木盆地第四纪磁性地层学研究. 地层学杂志, 27(4): 276-281
徐强, 廖仕孟, 朱永刚, 等. 2000. 川西龙门山前陆盆地中砂砾质楔形体的定量统计. 沉积与特提斯地质, 20(4): 31-37
徐仁, 陶君容, 孙湘君, 等. 1973. 希夏邦马峰高山栎化石层的发现及其植物学和地质学上的意义. 植物学报, 15(1): 103-119
许效松, 徐强. 1996. 盆山转换和当代盆地分析中的新问题. 岩相古地理,16(2): 24-33
许志琴, 杨经绥, 姜枚, 等. 1999. 大陆俯冲及青藏高原周缘造山带的崛起. 地学前缘, 6(3): 139-152
许志琴, 曾令森, 杨经绥, 等. 2004. 走滑断裂、“挤压性盆—山构造”与油气资源关系的探讨. 地球科学——中国地质大学学报, 29(6): 631-643
许志琴, 张建新, 许慧芬, 等. 1997. 中国主要大陆山链韧性剪切带及动力学. 北京:地质出版社, 28-211
许忠淮和石耀霖. 2003. 岩石圈结构与大陆动力学. 地震学报, 25(5): 512-527
薛祥煦, 李虎侯, 李永项, 等. 2004. 秦岭中更新世以来抬升的新资料及认识. 第四纪研究, 24(1): 82-87
闫小熊和周立发. 2001. 前陆盆地层序地层学研究现状及进展. 沉积与特提斯地质, 21(3): 60-64
闫臻, 方爱民, 潘裕生, 等. 2005. 西藏达金砾岩沉积环境、有孔虫时代及其大地构造意义. 自然科学进展, 15(5): 565-571
杨东, 方小敏, 宋友桂, 等. 2002. 六盘山西侧山麓剥蚀面的发育与新构造隆升. 沉积学报, 20(2): 282-287
杨明慧和刘池洋. 2000. 中国中西部类前陆盆地特征及含油气性. 石油与天然气地质,21(1): 46-49
杨振京, 刘志明, 张俊牌, 等. 2001. 银川盆地中更新世以来的孢粉记录及古气候研究. 海洋地质与第四纪地质, 21(3): 43-49
殷鸿福和童金南. 1995. 层序地层界面与年代地层界线的关系. 科学通报, 40(6): 539-541
尹安. 2001. 喜马拉雅-青藏高原造山带地质演化——显生宙亚洲大陆生长. 地球学报, 22(3): 193-230
余辉龙, 邓宏文, 胡勇. 2002. 从古地磁资料看柴达木盆地古构造环境. 石油勘探与开发, 29(6): 41-44
袁宝印和王振海. 1995. 青藏高原隆起与黄河地文期. 第四纪研究, 4: 353-359
袁道阳, 张培震, 刘百篪, 等. 2004. 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. 地质学报, 78(2): 271-278
岳乐平, Heller F., 邱占祥, 等. 2000. 兰州盆地第三系磁性地层年代与古环境记录. 科学通报, 45(18): 1998-2003
岳乐平, 李智佩, 朱桦, 等. 2002. 全球气候变化、青藏高原隆升与中国北方荒漠化. 地球学报, 23(增刊): 45-50
曾宜君, 杨学俊, 李云泉, 等. 2004. 川西前陆盆地南部中新生代砾岩的构造意义. 四川地质学报, 24(4): 198-201
曾允孚, 覃建雄. 1999. 沉积学发展现状与前瞻. 成都理工学院学报,26(1): 1-7
詹艳, 赵国泽, 王继军, 等. 2005. 青藏高原东北缘海原弧形构造区地壳电性结构探测研究. 地震学报, 27(4): 431-440
张柏桥, 胡望水, 舒志国, 等. 2004. 六盘山盆地与酒西盆地中新生代构造对比. 江汉石油学报, 26(1): 11-14
张波, 张进江, 杨武玲, 等. 2005. 我国中西部前陆盆地归属及其含油气性评述. 高校地质学报, 11(1): 126-136
张光亚和薛良清. 2002. 中国中西部前陆盆地油气分布与勘探方向. 石油勘探与开发,29(1): 1-5
张广良, 张培震, 陈杰. 2006,逆冲-褶皱造山过程中生长地层和生长不整合的识别及意义. 地震地质, 2
张国伟, 郭安林, 刘福田, 等. 1996. 秦岭造山带三维结构及其动力学分析. 中国科学(D), 26(增刊): 1-6
张国伟, 张本仁, 袁学诚, 等. 2001. 秦岭造山带与大陆动力学. 北京: 科学出版社, 421-727
张国伟,张宗清,董云鹏. 1995. 秦岭造山带主要构造岩石地层单元的构造性质及其大地构造意义. 岩石学报, 11(2): 102-114
张建新, 许志琴, 徐慧芬, 等. 1998. 北祁连加里东期俯冲-增生楔结构及动力学. 地质科学, 33(3): 290-299
张进, 马宗晋, 任文军, 等. 2004a. 鄂尔多斯西缘逆冲褶皱带构造特征及其南北差异的形成机制. 地质学报, 78(5): 600-611
张进, 马宗晋, 任文军, 等. 2004b. 宁夏中南部古生代弧型构造. 大地构造与成矿学, 28(1): 29-37
张进, 马宗晋, 任文军. 2005. 宁夏中南部新生界沉积特征及其与青藏高原演化的关系. 地质学报, 79(6): 757-773
张珂, 刘开瑜, 吴加敏, 等. 2004. 宁夏中卫盆地的沉积特征及其所反映的新构造运动. 沉积学报, 22(3): 465-473
张明利, 金之钧, 汤良杰, 等. 2002. 前陆盆地研究的回顾与展望. 地质论评, 48(2): 214-220
张培震, 邓起东, 杨晓平, 等. 1996. 天山的晚新生代构造变形及其地球动力学问题. 中国地震,12(2): 127-140
张培震, 沈正康, 王敏, 等. 2004. 青藏高原及周边现今构造变形的运动学. 地震地质, 26(3): 365-368
张培震, 王敏, 甘卫军, 等. 2003. GPS 观测的活动断裂滑动速率及其对现今大陆动力作用的制约. 地学前缘,10(3): 81-92
张培震, 王琪, 马宗晋. 2002. 中国大陆现今构造运动大的 GPS 速度场与活动地块. 地学前缘, 9(2): 430-441
张旗, 郭原生, 王岳明, 等. 1997. 祁连山地区镁铁-超镁铁岩的多样性. 地球科学进展, 12(5): 324-330
张旗, 王焰, 钱青. 2000. 北祁连早古生代洋盆是裂陷槽还是大洋盆?——与葛肖虹讨论. 地质科学, 35(1): 121-158
张青松,李炳元,景可. 1981. 青藏地区上新世古地理与高原隆起.见.青藏高原隆起的时代、幅度和形式问题. 北京:科学出版社,26-35
张清志, 陈智梁, 刘宇平, 等. 2005. 青藏高原及其东南前陆地壳运动的 GPS 监测. 地球物理学进展, 20(2): 524-527
张希明. 2001. 塔里木盆地中新生代沉积演化特征. 新疆地质, 19(4): 246-250
张行. 2001. 甘肃临夏盆地中新世地层及哺乳动物化石. 兰州大学学报(自然科学版), 37(2): 123-130
张一勇. 1995. 中国早第三纪孢粉植物群纲要. 古生物学报, 34(2): 212-227
张永志, 王卫东, 祝意青, 等. 2004. 青藏高原东北侧断层活动引起的地壳三维变形与重力场变化研究. 地
球学报, 25(5): 583-586
张岳桥, 陈正乐, 杨农. 2001. 阿尔金断裂晚新生代左旋走滑位错的地质新证据. 现代地质, 15(1): 8-12
张岳桥, 杨农, 陈文, 等. 2003. 中国东西部地貌边界带晚新生代构造变形历史与青藏高原东缘隆升过程初
步研究. 地学前缘(中国地质大学,北京), 10(4): 599-612
张招崇, 毛景文, 杨健民, 等. 1998. 北祁连山西段中元古代蛇绿岩的发现及其意义. 矿物岩石地球化学通报, 17(2): 114-118
张振法, 李超英, 牛颖智. 1997. 阿拉善-敦煌陆块的性质/范围及其构造作用和意义. 内蒙古地质, 81(2): 1-14
张振法. 1997. “北山晚华力西地槽褶皱带”(西阿拉善)的性质/归属及有关问题探讨. 内蒙古地质, 84(1): 24-40
张正涛和张永志. 2005. GPS 观测研究青藏东北缘的水平变形特征. 测绘和空间地理信息, 28(3): 6-8
赵培坤和纪有亮. 2005. 鄂尔多斯西缘前陆盆地上古生界沉积相特征研究. 新疆地质, 23(2): 152-158
赵生贵. 1996. 祁连造山带特征及其构造演化. 甘肃地质学报, 5(1): 16-29
赵志军, 方小敏, 李吉均, 等. 2001. 酒泉砾石层的古地磁年代与青藏高原隆升. 科学通报, 46(14): 1208-1212
郑德文, 张培震, 万景林, 等. 2005. 六盘山盆地热历史的裂变径迹证据. 地球物理学报, 48(1): 157-164
郑德文, 张培震, 万景林,等. 2003. 青藏高原东北边缘晚新生代构造变形的时序—临夏盆地碎屑颗粒磷灰石裂变径迹记录. 中国科学(D 辑), 33(增刊): 190-198
郑洪波, Botcher K. and Powell C. 2002a. 新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升—I 地层学与岩石学证据. 沉积学报, 20(2): 274-281
郑洪波, Botcher K. and Powell C. 2003. 新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升-Ⅱ沉积相与沉积盆地演化. 沉积学报, 21(1): 46-51
郑洪波, 陈惠中, 靳鹤龄, 等. 2002b. 上新世—早更新世青藏高原北缘隆升的磁性地层学证据. 海洋地质与第四纪地质, 22(2): 57-62
郑洪波, 黄湘通, 刘锐, 等. 2005. 晚中新世以来亚洲季风阶段性演化的海陆记录. 矿物岩石地球化学通报, 24(2): 103-109
郑洪波. 2002. 从新疆叶城剖面砂岩和砾岩组分看西昆仑山的剥蚀历史. 地质力学学报, 8(4): 297-305
郑民, 孟自芳, 李相博, 等. 2005. 陆内前陆盆地的复合动力演化研究——以库车陆内前陆盆地为例. 新疆石油天然气, 1(1): 12-16
中国岩石圈动力学概论编委会. 1991. 中国岩石圈动力学概论. 北京: 地震出版社, 144-155
钟大赉和丁林. 1996. 青藏高原隆起过程及其机制探讨. 中国科学(D 辑), 26(4): 289-295
钟巍, 李吉均, 方小敏. 2001. 临夏盆地晚新生代沉积特征与青藏高原隆升. 新疆大学学报(理工版), 18(4): 401-407
周鼎武, 董云鹏, 华洪, 等. 1996. “磨拉石建造”和“不整合”在地层对比中的意义. 地质论评, 42(5): 416-423
周江羽, 王江海, 尹安, 等. 2002. 青藏东北缘早第三纪盆地充填的沉积型式及构造背景—以囊谦和下拉秀盆地为例. 沉积学报, 20(1): 85-91
朱大岗, 孟宪刚, 邵兆刚, 等. 2004. 西藏阿里札达盆地上新世—早更新世沉积相及其构造演化特征. 地质力学学报, 10(3): 245-252
朱弟成, 潘桂棠, 莫宣学, 等. 2004. 印度大陆和欧亚大陆的碰撞时代. 地球科学进展, 19(4): 564-571
朱利东, 王成善, 伊海生, 等. 2004. 青藏高原盆地系统演化与高原形成时间. 成都理工大学学报:自然科学版,31(3): 249-255
朱筱敏, 康安, 康强. 2005. 柴达木盆地第四纪底界时代及识别标志. 西安石油大学学报(自然科学版),20(5): 1-5
朱筱敏, 康安, 王贵文. 2003. 陆相坳陷型和断陷型湖盆层序地层样式探讨. 沉积学报, 21(2): 283-287
朱筱敏, 王贵文, 李滨阳, 等. 2002. 开鲁盆地陆西凹陷下白垩统层序地层学和油气评价. 沉积学报, 20(4): 532-567
左国朝, 吴茂炳, 毛景文, 等. 1999. 北祁连西段早古生代构造演化史. 甘肃地质学报, 8(1): 6-13
左国朝和吴汉泉. 1997. 北祁连中段早古生代双向俯冲碰撞造山模式剖析. 地球科学进展, 12(4): 315-332
© 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 |