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    中国百强科技报刊

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    Volume 35 Issue 5
    Sep.  2010
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    Article Contents
    ZHANG Ke-xin, WANG Guo-can, LUO Man-sheng, JI Jun-liang, XU Ya-dong, CHEN Rui-ming, CHEN Fen-ning, SONG Bo-wen, LIANG Yin-ping, ZHANG Jian-yu, YANG Yong-feng, 2010. Evolution of Tectonic Lithofacies Paleogeography of Cenozoic of Qinghai-Tibet Plateau and Its Response to Uplift of the Plateau. Earth Science, 35(5): 697-712. doi: 10.3799/dqkx.2010.085
    Citation: ZHANG Ke-xin, WANG Guo-can, LUO Man-sheng, JI Jun-liang, XU Ya-dong, CHEN Rui-ming, CHEN Fen-ning, SONG Bo-wen, LIANG Yin-ping, ZHANG Jian-yu, YANG Yong-feng, 2010. Evolution of Tectonic Lithofacies Paleogeography of Cenozoic of Qinghai-Tibet Plateau and Its Response to Uplift of the Plateau. Earth Science, 35(5): 697-712. doi: 10.3799/dqkx.2010.085

    Evolution of Tectonic Lithofacies Paleogeography of Cenozoic of Qinghai-Tibet Plateau and Its Response to Uplift of the Plateau

    doi: 10.3799/dqkx.2010.085
    • Received Date: 2010-05-31
    • Publish Date: 2010-09-01
    • By doing an integrated research on the types of 98 remnant basins, tectonic setting and lithostratigraphic sequence, we studied the evolution of tectonic lithofacies paleogeography of the Paleocene—Eocene, Oligocene, Miocene and Pliocene of Qinghai-Tibet plateau, dividing it into four stages: (1) The Paleocene to Eocene characterized by an uplift and erosional area in Songpan—Garzê and Gangdisê, depressed basins (lakes and pluvial plain) in eastern Tarim, Qaidam, Qiangtang and Hoh Xil, and Neo-Tethys sea in western and southern Qinghai-Tibet plateau; (2) The Oligocene characterized by an uplift area in Gangdisê-Himalaya and Karakorum (marked by the absence of the sediments), rivers (originated from east and flew to west) in Yarlung Zangbo Jiang (marked by the deposition of Dazhuka conglomerate), an uplift and erosional area in western Kunlun and Songpan-Garzê, and depressed basins (lakes) in Tarim, Qaidam, Qiangtang and Hoh Xil. Besides, it is also featured with a depressed littoral and neritic basin in southwestern Tarim and the termination of marine-facies deposition at the end of the Oligocene; (3) The Miocene characterized with the widespread of regional unconformity in the plateau, the overall uplift of the plateau in its adjacent area ca. 23 Ma, depressed basins (lakes) in Tarim, Qaidam, Xining-Nanzhou, Qiangtang, Hoh Xil, lacustrine-facies deposition expanding to its peak in the plateau and its adjacent area ca. 18—13 Ma, and the formation of south-north fault basins in southern Tibet ca. 13—10 Ma, all indicating that the plateau uplifted to its peak and began to collapse; (4) The Pliocene characterized by an uplift and erosional area in most part of the plateau except in Hoh Xil-Qiangtang, Tarim and Qaidam. The continuing uplift and intensive fault in plateau elevated and divided the original large basin into small basins. The lacustrine-facies deposition prominently shrank and boulderstones accumulated, indicating a response to the overall uplift of the plateau. The plateau, which was higher in east and lower in west in physiognomy in the Paleogene, experienced a process of uneven uplift and sag in the Neogene and finally became higher in west and lower in east in physiognomy. This process indicates that a great physiognomy-reverse event happened in the Qinghai-Tibet plateau.

       

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    • Burbank, D.W., Johnson, G.D., 1982. Intermontane-basin development in the past 4 Myr in the North-West Himalay. Nature, 298(5873): 432-436. doi: 10.1038/298432a0
      Bureau of Geology and Mineral Resoures of Gansu Province, 1997. Stratigraphy (Lithostratic) of Gansu Province. China University of Geosiences Press, Wuhan, 1-288 (in Chinese).
      Chang, H., Fang, X.M., An, Z.S., et al., 2001. Miocene-Pliocene strata features in the Suerkal basin and the palaeo-environment significance. Marine Geology & Quaternary Geology, 21(3): 107-111 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ200103019.htm
      Chen, Z.X., Jia, D., Wei, G.Q., et al., 2008. Meso-Cenozoic sediment transport and tectonic transition in the western Sichuan foreland basin. Geology in China, 35(3): 472-481 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200803013.htm
      Clark, M.K., Schoenbohm, L.M., Royden, L.H., et al., 2004. Surface uplift, tectonics, and erosion of eastern Tibet from large-scale drainage patters. Tectonics, 23: TC1006. doi: 10.1029/2002TC001402
      Cui, J.W., Tang, Z.M., Deng. J.F., et al., 1999. Altun fault system. Geological Publishing House, Beijing, 1-315 (in Chinese).
      Cui, J.W., Zhang, X.W., Tang, Z.M., 2006. Tectonic divisions of the Qinghai-Tibet plateau and structural characteristics of deformation on their boundaries. Geology in China, 33(2): 256-267 (in Chinese with English abstract).
      Deng, Z.L., Hou, Y.C., Gu, F.B., 2000. Filling characteristics, sporopollen assemblage and palaeoclimate variation of Tertiary basins in the northeastern Qinghai-Tibet plateau. Qinghai Geology, (1): 43-53 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GTJL200001006.htm
      Ding, L., 2003. Paleocene deep-water sediments and radiolarian faunas: implications for evolution of Yarlung-Zangbo foreland basin, southern Tibet. Science in China (Ser. D), 46(1): 84-91. doi: 10.1360/03yd9008
      Fan, M.J., Song, C.H., 2003. A sedimentary environment analysis and the tectonic uplift of Linxia basin in the northeast margin of Tibetan plateau. Journal of Lanzhou University (Natural Science), 39(3): 84-89 (in Chinese).
      Fang, X.M., Carmala, G., Van der Voo, 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(3-4): 545-560. doi: 10.1016/S0012-821X(03)00142-0
      Fang, X.M., Song, C.H., Dai, S., et al., 2007. Cenozoic deformation and uplift of the NE Qinghai-Tibet plateau: evidence from high-resolution magnetostratigraphy and basin evolution. Earth Science Frontiers, 14(1): 230-242 (in Chinese with English abstract).
      Fang, X.M., Zhao, Z.J., Li, J.J., et al., 2005. Magnetostratigraphy of Late Cenozoic Laojunmiao anticline in the northern Qilian Mountains and its implications for the northern Tibetan plateau uplift. Science in China (Ser. D), 48(7): 1040-1051. doi: 10.1360/03yd0188
      Ge, X.H., Ren, S.M., Ma, L.X., et al., 2006. Multi-stage uplifts of the Qinghai-Tibet plateau and their environmental effects. Earth Science Frontiers, 13(6): 118-130.
      Han, J.E., 2006. Sequence stratigraphy of Pliocene-Eopleistocene epoch and its paleoenvironmental significance in Zanda basin, Tibet (Dissertation). Chinese Academy of Geological Sciences, Beijing (in Chinese).
      Hao, Y.C., Guan, S.Z., Ye, L.S., et al., 2002. Neogene stratigraphy and palaeogeography in the western Tarim basin. Acta Geologica Sinica, 76(3): 289-298 (in Chinese with English abstract).
      He, K.Z., Zhao, C.H., He, H.S., et al., 1996. Intracontinental rift and orogeny in western Yunnan. China University of Geosciences Press, Wuhan, 1-141 (in Chinese).
      Hong, H.L., Zhang, K.X., Li, Z.H., 2009. Climatic and tectonic uplift evolution since ~7 Ma in Gyirong basin, southwestern Tibet plateau: clay mineral evidence. International Journal of Earth Sciences, doi: 10.1007/s00531-009-0457-x
      Hoorn, C., Ohja, T., Quade, J., 2000. Palynological evidence for vegetation development and climatic change in the Sub-Himalayan zone (Neogene, Central Nepal). Palaeogeography, Palaeoclimatology, Palaeoecology, 163(3-4): 133-161. doi: 10.1016/S0031-0182(00)00149-8
      Ji, J.L., Qiang, T., Kou, X.H., et al., 2010. Magnetostratigraphy of the Neogene strata in the Xunhua basin, Qinghai Province. Earth Science—Journal of China University of Geosciences, 35(5): 803-810 (in Chinese with English abstract). doi: 10.3799/dqkx.2010.093
      Jia, C.Z., Zhang, S.B., Wu, S.Z., 2004. Stratigraphy of the Tarim basin and adjacent areas. Science Press, Beijing (in Chinese).
      Jin, W., 2007. Research on sedimentary response to uplifting of Tibetan plateau hinterland and oil-gas reservation during the Late Cretaceous-Paleogene period (Dissertation). Chengdu University of Technology, Chengdu (in Chinese).
      Jin, X.C., Wang, J., Chen, B.W., 2003. Cenozoic depositional sequences in the piedmont of the West Kunlun and their paleogeographic and tectonic implications. Journal of Asian Earth Sciences, 21(7): 755-765. doi: 10.1016/S1367-9120(02)00073-1
      Kirby, E., Reiners, P.W., Krol, M.A., et al., 2002. Late Cenozoic evolution of the eastern margin of the Tibetan plateau: inferences from 40Ar/39Ar and (U-Th)/He thermochronology. Tectonics, 21(1): doi: 10.1029/2000TC001246
      Kumar, R., Ghosh, S.K., Mazari, R.K., et al., 2003. Tectonic impact on the fluvial deposits of Plio-Pleistocene Himalayan foreland basin, India. Sedimentary Geology, 158(3-4): 209-234. doi: 10.1016/S0037-0738(02)00267-1
      Li, H.B., Valli, F., Xu, Z.Q., et al., 2006. Deformation and tectonic evolution of the Karakorum fault, western Tibet. Geology in China, 33(2): 239-255 (in Chinese with English abstract).
      Li, J.J., Pan, B.T., Chen, F.H., et al., 1995. Uplift of the Qinghai-Tibet plateau and global change. Lanzhou University Press, Lanzhou, 1-207.
      Li, J.J., Fang, X.M., Ma, H.Z., et al., 1996. Geomorphological and environmental evolution in the Upper Reaches of the Yellow River during the Late Cenozoic. Science in China (Ser. D), 39(4): 380-390. http://www.cnki.com.cn/Article/CJFD1996-JDXG199604004.htm
      Li, Y., Zeng, Y.F., 1994. Fill sequence of Longmen Mountains foreland basin. Journal of Chengdu Institute of Technology, 21(3): 46-55 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-CDLG403.006.htm
      Li, Y.X., Pang, X.Q., Tang, L.J., et al., 2002. The S-N tectonic system in the west of Qaidam basin and its control on petroleum. Petroleum Exploration and Development, 29(1): 65-68 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKYK200201015.htm
      Liu, S.F., Zhang, G.W., Heller, P.L., 2007. Evolution of Cenozoic basins in Xunhua-Guide region and implication for plateau accretion. Science in China (Ser. D), 50(Suppl. Ⅱ): 277-291. http://qikan.cqvip.com/Qikan/Article/Detail?id=1000887585
      Liu, Z.F., Wang, C.S., Yi, H.S., et al., 2001. Reconstruction of depositional history of the Cenozoic Hoh Xil basin. Acta Geologica Sinica, 75(2): 250-258 (in Chinese with English abstract). http://www.researchgate.net/publication/283139054_Reconstruction_of_depositional_history_of_the_cenozoic_hoh_xil_basin
      Ma, Y.Z., 2004. Late Cenozoic vegetational evolution and environmental transition of the northeast Tibetan plateau (Dissertation). Lanzhou University, Lanzhou (in Chinese).
      Meng, Q.Q., 2008. High resolution magnetostratigraphy in the north of Qaidam basin and the sedimentary response to tectonic since Late Cenozoic (Dissertation). Lanzhou University, Lanzhou (in Chinese).
      Quade, J., Cater, J.M.L., Ojha, T.P., et al., 1995. Late Miocene environmental change in Nepal and the northern Indian subcontinent: stable isotopic evidence from paleosols. GSA Bulletin, 107(12): 1381-1397. doi: 10.1130/0016-7606(1995)
      Sanyal, P., Bhattacharya, S.K., Prasad, M., 2005. Chemical diagenesis of Siwalik sandstone: isotopic and mineralogical proxies from Surai Khola Section, Nepal. Sedimentary Geology, 180(1-2): 57-74. doi: 10.1016/j.sedgeo.2005.06.005
      Shao, L.Y., He, Z.P., Gu, J.Y., et al., 2006. Lithofacies palaeogeography of the Paleogene in Tarim basin. Journal of Palaeogeography, 8(3): 353-364 (in Chinese with English abstract). http://epub.cnki.net/grid2008/docdown/docdownload.aspx?filename=GDLX200603008&dbcode=CJFD&year=2006&dflag=pdfdown
      Shi, J.A., 2001. Sequence stratigraphy and sedimentary, diagenetic evolution of western Tarim basin. Science Press, Beijing, 147-156 (in Chinese).
      Si, J.L., 2008. Cenozoic uplift and growth of northwestern margin of the Tibetan plateau (Dissertation). China University of Geosciences, Beijing (in Chinese).
      Song, C.H., 2006. Tectonic uplift and Cenozoic sedimenatary evolution in the northern margin of the Tibetan plateau (Dissertation). Lanzhou University, Lanzhou (in Chinese).
      Song, C.H., Fang, X.M., Gao, J.P., et al., 2003. Magnetostratigraphy of Late Cenozoic fossil mammals in the northeastern margin of the Tibetan plateau. Chinese Science Bulletin, 48(2): 188-193. doi: 10.1360/03tb9039
      Song, C.H., Fang, X.M., Li, J.J., et al., 2001. Tectonic uplift and sedimentary evolution of the Jiuxi basin in the northern margin of the Tibetan plateau since 13 MaBP. Science in China (Ser. D), 44(Suppl. ): 197-202.
      Song, C.H., Fang, X.M., Li, J.J., et al., 2003. Pliocene sedimentary environment of the Guide basin on the northeast margin of the Qinghai-Tibetan plateau and its significance. Quaternary Sciences, 23(1): 92-102 (in Chinese with English abstract).
      Sun, J.M., Zhang, Z.Q., Zhang, L.Y., 2009. New evidence on the age of the Taklimakan desert. Geology, 37(2): 159-162. doi: 10.1130/G25338A.1
      Tang, T.F., Xue, Y.S., Yu, C.L., et al., 1992. Marine sedimentary characteristics and environments from Late Cretaceous to Early Tertiary in the west part of Talimu basin of Xinjiang. Science Press, Beijing, 1-138 (in Chinese).
      Valdiya, K.S., 2002. Emergence and evolution of Himalaya: reconstructing history in the light of recent studies. Progress in Physical Geography, 26(3): 360-399. doi: 10.1191/0309133302pp342ra
      Wang, C.S., Zhao, X.X., Liu. Z.F., et al., 2008. Constraints on the early uplift history of the Tibetan plateau. PNAS, 105 (13): 4987-4992. doi: 10.1073/pnas.0703595105
      Wang, D.C., Zhang, J.J., Yang, X.Y., et al., 2009. Tectonic and environmental evolution of Gyirong basin, and its relationship to the uplift of Tibetan plateau. Acta Scientiarum Naturalium Universitatis Pekinensis, 45(1): 79-89 (in Chinese with English abstract).
      Wang, G.C., Garver, J.I., Liu, C., 2008. Cenozoic tectonic history in the Gyirong-Nyalam area, south Tibet: evidence from fission-track thermochronology. In: Garver, J.I., Montario, M., eds., Proceedings from the 11th international conference on thermochronometry, Anchorage Alaska, Sept., 2008.
      Wang, Y., Deng, T., Biasatti, D., 2006. Ancient diets indicate significant uplift of southern Tibet after ca 7 Ma. Geology, 34(4): 309 - 312. doi: 10.1130/G22254.1
      Wu, L.C., Yue, L.P., Wang, J.Q., et al., 2006. Magnetostratigraphy of stratotype section of the Neogene Xiejian Stage. Journal of Stratigraphy, 30(1): 50-53 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DCXZ200601007.htm
      Wu, Z.H., Wu, Z.H., Hu, D.G., et al., 2006. Features of Early Miocene large paleolakes in the interior of the Qinghai-Tibet plateau and their tectonic significance. Geological Bulletin of China, 25(7): 782-791 (in Chinese with English abstract).
      Xiang, F., Wang, C.S., Zhu, L.D., 2002. Feature of Cenozoic molasse at the south edge of Qinghai-Tibetan plateau. Journal of Chengdu University of Technology, 29(5): 515-520 (in Chinese with English abstract).
      Xie, G.P., 2004. The Tertiary and local mammalian faunas in Lanzhou basin, Gansu. Journal of Stratigraphy, 28(1): 67-80 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DCXZ200401010.htm
      Yang, P., 2007. Study on Tertiary sequence biostratigraphy in Qigequan-Hongliuquan region, western Qaidam basin (Dissertation). China University of Geosciences, Beijing, 1-101 (in Chinese).
      Yin, A., Rumelhart, P.E., Butler, R., et al., 2002. Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation. Geological Society of America Bulletin, 114(10): 1257-1295. doi: 10.1130/0016-7606(2002)
      Yue, L.P., Deng, T., Zhang, R., et al., 2004. Paleomagnetic chronology and records of Himalayan uplift on the Longgugou Section of Gyirong-Oma basin in Xizang (Tibet). Chinese Journal of Geophysics, 47(6): 1009-1016 (in Chinese with English abstract).
      Yue, L.P., Qiu, Z.X., Xie, G.P., 2003. Sedimentary environment of Tertiary recorded in the Yongdeng Section of Lanzhou basin. Acta Sedimentologica Sinica, 21(4): 683-687, 694 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB200304021.htm
      Zhang, J., Ma, Z.J., Ren, W.J., 2005. The sedimentary characteristics of Cenozoic strata in central and southern Ningxia and their relationships with the development of the Qinghai-Tibetan plateau. Acta Geologica Sinica, 79(6): 757-773 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200506012.htm
      Zhang, K.X., Wang, G.C., Cao, K., et al., 2008. Cenozoic sedimentary records and geochronological constraints of differential uplift of the Qinghai-Tibet plateau. Science in China (Ser. D), 51(11): 1658-1672. doi: 10.1007/s11430-008-0132-2
      Zhang, K.X., Wang, G.C., Chen, F.N., et al., 2007. Coupling between the uplift of Qinghai-Tibet plateau and distribution of basins of Paleogene-Neogene. Earth Science—Journal of China University of Geosciences, 32(5): 583-597 (in Chinese with English Abstract).
      Zhang, K.X., Wang, G.C., Ji, J.L., et al., 2010. Stratigraphic realm and sedimentary sequence of paleogene-Neogene of Qinghai-Tibet plateau and sedimentary response to the uplift of the plateau. Science in China (Earth Sciences), 53(9): 1271-1294. doi: 10.1007/s11430-010-4048-2
      Zhang, Y.D., Song, J.G., Zhu, R.K., 1999. Characteristics of sedimentary facies and lithofacies paleogeography of Upper Tertiary in southwest depression, Tarim basin. Xinjiang Petroleum Geology, 20(2): 123-126, 171 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XJSD902.009.htm
      Zhao, J.F., Chen, X.H., Du, Y.B., 2004. The Tertiary sedimentary evolution of the Qaidam basin, Northwest China. Petroleum Exploration and Development, 31(3): 41-44 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKYK200403010.htm
      Zhou, Z.Y., Zhao, Z.X., Hu, Z.X., et al., 2001. Stratigraphy of the Tarim basin. Science Press, Beijing, 1-359 (in Chinese).
      Zhu, L.D., 2004. Uplift of the north of Qinghai-Tibet plateau and record in basins and geomorphy (Dissertation). Chengdu University of Technology, Chengdu (in Chinese).
      常宏, 方小敏, 安芷生, 等, 2001. 索尔库里盆地中-上新世地层特征及其环境意义. 海洋地质与第四纪地质, 21(3): 107-111. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200103019.htm
      陈竹新, 贾东, 魏国齐, 等, 2008. 川西前陆盆地中-新生代沉积迁移与构造转换. 中国地质, 35(3): 472-481. doi: 10.3969/j.issn.1000-3657.2008.03.011
      崔军文, 唐哲明, 邓晋福, 等, 1999. 阿尔金断裂系. 北京: 地质出版社, 1-315.
      崔军文, 张晓卫, 唐哲民, 2006. 青藏高原的构造分区及其边界的变形构造特征. 中国地质, 33(2): 256-267. doi: 10.3969/j.issn.1000-3657.2006.02.003
      邓中林, 侯元才, 古凤宝, 2000. 青海东北部第三纪西宁-贵德-化隆盆地充填特征、孢粉组合方式与古气候演变. 青海地质, (1): 43-53. https://www.cnki.com.cn/Article/CJFDTOTAL-GTJL200001006.htm
      丁林, 2003. 西藏雅鲁藏布江缝合带古新世深水沉积和放射虫动物群的发现及对前陆盆地演化的制约. 中国科学(D辑), 33(1): 47-58. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200301005.htm
      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(自然科学版), 39(3): 84-89. doi: 10.3321/j.issn:0455-2059.2003.03.023
      方小敏, 宋春晖, 戴霜, 等, 2007. 青藏高原东北部阶段性变形隆升: 西宁、贵德盆地高精度磁性地层和盆地演化记录. 地学前缘, 14(1): 230-242. doi: 10.3321/j.issn:1005-2321.2007.01.022
      方小敏, 宋春晖, 高军平, 等, 2002. 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. doi: 10.3321/j.issn:0023-074X.2002.23.015
      方小敏, 赵志军, 李吉均, 等, 2004. 祁连山北缘老君庙背斜晚新生代磁性地层与高原北部隆升. 中国科学(D辑), 34(2): 97-106. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200402000.htm
      甘肃省地质矿产局, 1997. 甘肃省岩石地层. 武汉: 中国地质大学出版社, 1-288.
      葛肖虹, 任收麦, 马立祥, 等, 2006. 青藏高原多期次隆升的环境效应. 地学前缘, 13(6): 118-130. doi: 10.3321/j.issn:1005-2321.2006.06.015
      韩建恩, 2006. 西藏札达盆地上新世-早更新世层序地层学及其古环境意义(硕士学位论文). 北京: 中国地质科学院.
      郝诒纯, 关绍曾, 叶留生, 等, 2002. 塔里木盆地西部地区新近纪地层及古地理特征. 地质学报, 76(3): 289-298. doi: 10.3321/j.issn:0001-5717.2002.03.001
      何科昭, 赵崇贺, 何浩生, 等, 1996. 滇西陆内裂谷与造山作用: 滇西地区印支期后的构造演化. 武汉: 中国地质大学出版社, 1-141.
      季军良, 强泰, 寇晓虎, 等, 2010. 青海循化盆地新近纪磁性地层学研究. 地球科学——中国地质大学学报, 35(5): 803-810. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201005008.htm
      贾承造, 张师本, 吴绍祖, 2004. 塔里木盆地及周边地层(上、下册). 北京: 科学出版社.
      金玮, 2007. 青藏高原腹地晚白垩-古近纪高原隆升的沉积响应与油气后期保存(博士学位论文). 成都: 成都理工大学.
      李海兵, Valli, F., 许志琴, 等, 2006. 喀喇昆仑断裂的变形特征及构造演化. 中国地质, 33(2): 239-255. doi: 10.3969/j.issn.1000-3657.2006.02.002
      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辑), 26(4): 316-322. doi: 10.3321/j.issn:1006-9267.1996.04.005
      李勇, 曾允孚, 1994. 龙门山前陆盆地充填序列. 成都理工学院学报, 21(3): 46-55. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG403.006.htm
      李玉喜, 庞雄奇, 汤良杰, 等, 2002. 柴西地区近南北向构造系统及其控油作用分析. 石油勘探与开发, 29(1): 65-68. doi: 10.3321/j.issn:1000-0747.2002.01.016
      刘少峰, 张国伟, Heller, P.L., 2007. 循化-贵德地区新生代盆地发育及其对高原增生的指示. 中国科学(D辑), 37(增刊Ⅰ): 235-248. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2007S1025.htm
      刘志飞, 王成善, 伊海生, 等, 2001. 可可西里盆地新生代沉积演化历史重建. 地质学报, 75(2): 250-258. doi: 10.3321/j.issn:0001-5717.2001.02.015
      马玉贞, 2004. 青藏高原东北部晚新生代植被演化和环境变迁(博士学位论文). 兰州: 兰州大学.
      孟庆泉, 2008. 柴达木盆地北缘晚新生代精细磁性地层学与沉积对构造的响应(博士学位论文). 兰州: 兰州大学.
      邵龙义, 何志平, 顾家裕, 等, 2006. 塔里木盆地古近纪岩相古地理. 古地理学报, 8(3): 353-364. doi: 10.3969/j.issn.1671-1505.2006.03.008
      史基安, 2001. 塔里木盆地西部层序地层与沉积、成岩演化. 北京: 科学出版社, 147-156.
      司家亮, 2008. 青藏高原西北缘新生代构造隆升及扩展(博士学位论文). 北京: 中国地质大学.
      宋春晖, 2006. 青藏高原北缘新生代沉积演化与高原构造隆升过程(博士学位论文). 兰州: 兰州大学.
      宋春晖, 方小敏, 李吉均, 等, 2001. 青藏高原北缘酒西盆地13 Ma以来沉积演化与构造隆升. 中国科学(D辑), 31(增刊): 155-162. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2001S1023.htm
      宋春晖, 方小敏, 李吉均, 等, 2003. 青藏高原东北部贵德盆地上新世沉积环境分析及其意义. 第四纪研究, 23(1): 92-102. doi: 10.3321/j.issn:1001-7410.2003.01.011
      唐天福, 薛耀松, 俞从流, 等, 1992. 新疆塔里木盆地西部晚白垩世至早第三纪海相沉积特征及沉积环境. 北京: 科学出版社, 1-138.
      王德朝, 张进江, 杨雄英, 等, 2009. 吉隆盆地构造、环境演化与青藏高原隆升. 北京大学学报(自然科学版), 45(1): 79-89. doi: 10.3321/j.issn:0479-8023.2009.01.013
      武力超, 岳乐平, 王建其, 等, 2006. 新近系谢家阶层型剖面古地磁年代学研究. 地层学杂志, 30(1): 50-53. doi: 10.3969/j.issn.0253-4959.2006.01.007
      吴珍汉, 吴中海, 胡道功, 等, 2006. 青藏高原腹地中新世早期古大湖的特征及其构造意义. 地质通报, 25(7): 782-791. doi: 10.3969/j.issn.1671-2552.2006.07.003
      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): 515-520. doi: 10.3969/j.issn.1671-9727.2002.05.008
      颉光普, 2004. 甘肃兰州盆地的第三纪地层及哺乳动物群. 地层学杂志, 28(1): 67-80. doi: 10.3969/j.issn.0253-4959.2004.01.011
      杨平, 2007. 柴达木盆地西部七个泉-红柳泉地区第三系层序生物地层学研究(博士学位论文). 北京: 中国地质大学, 1-101.
      岳乐平, 邓涛, 张睿, 等, 2004. 西藏吉隆-沃马盆地龙骨沟剖面古地磁年代学及喜马拉雅山抬升记录. 地球物理学报, 47(6): 1009-1016. doi: 10.3321/j.issn:0001-5733.2004.06.012
      岳乐平, 邱占祥, 颉光普, 等, 2003. 兰州盆地永登剖面记录的第三纪沉积环境. 沉积学报, 21(4): 683-687, 694. doi: 10.3969/j.issn.1000-0550.2003.04.022
      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. doi: 10.3321/j.issn:0001-5717.2005.06.005
      张克信, 王国灿, 曹凯, 等, 2008. 青藏高原新生代主要隆升事件: 沉积响应与热年代学记录. 中国科学(D辑), 38(12): 1575-1588. doi: 10.3321/j.issn:1006-9267.2008.12.011
      张克信, 王国灿, 陈奋宁, 等, 2007. 青藏高原古近纪-新近纪隆升与沉积盆地分布耦合. 地球科学——中国地质大学学报, 32(5): 583-597. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200705002.htm
      张运东, 宋建国, 朱如凯, 1999. 塔里木盆地西南坳陷上第三系沉积相及岩相古地理特征. 新疆石油地质, 20(2): 123-126, 171. doi: 10.3969/j.issn.1001-3873.1999.02.010
      赵加凡, 陈小宏, 杜业波, 2004. 柴达木第三纪湖盆沉积演化史. 石油勘探与开发, 31(3): 41-44. doi: 10.3321/j.issn:1000-0747.2004.03.011
      周志毅, 赵治信, 胡兆珣, 等, 2001. 塔里木盆地各纪地层. 北京: 科学出版社, 1-359.
      朱利东, 2004. 青藏高原北部隆升与盆地和地貌记录(博士学位论文). 成都: 成都理工大学.
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