青藏高原隆生演化变形模式研究进展
Summary and Current Status of the Research Models for the Tibetan Plateau Uplift

作者: 马钦忠 :上海市地震局,上海;

关键词: 青藏高原印度板块欧亚板块隆升机制Tibetan Plateau India Plate Eurasian Plate Uplift Mechanism

摘要:
多半个世纪以来国内外许多地球科学家对青藏高原的形成和演化进行多学科研究,各种构造变形模式的观点和假设相继出现,随着科学技术的发展和最新资料的不断积累,已有的一些模式不断被质疑、修正,新的模式不断出现。本文对11种模式进行追踪梳理、简洁综述,对一些模式的不足和质疑问题也予以简介,并对青藏高原构造演化变形模式研究现状进行了梳理,以期对全面认识青藏高原构造演化变形模式研究的过程有所裨益。

Abstract: For more than half a century, many geoscientists at home and abroad have carried out multi-dis- ciplinary research on the formation and evolution of the Tibetan Plateau. Various views and hy-pothesis of the tectonic formation models appeared successively. With the development of science and technology as well as the steady accumulation of the latest data, some existing models constantly are challenged and corrected, and new models unceasing put forward. In this paper the tracks of eleven models are followed and reviewed concisely, and the problem of the lack of some patterns and questions also are introduced briefly. The research status about the tectonic evolution and deformation models are also teased. It is hoped to benefit to comprehensively understanding the tectonic evolution and deformation models of the Tibetan Plateau.

文章引用: 马钦忠 (2016) 青藏高原隆生演化变形模式研究进展。 自然科学, 4, 229-241. doi: 10.12677/OJNS.2016.42028

参考文献

[1] Willett, S.D. and Beaumont, C. (1994) Subduction of Asian Lithospheric Mantle Beneath Tibet Inferred from Models of Continental Collision. Nature, 369, 642-645.
http://dx.doi.org/10.1038/369642a0

[2] 李廷栋. 青藏高原隆升的过程和机制[J]. 地球学报: 中国地质科学院院报, 1995(1): 1-9.

[3] 钟大赉, 丁林. 青藏高原的隆起过程及其机制探讨[J]. 中国科学, 1996, 26(4): 289-295.

[4] Mattauer, M (1986) Intracontinental Subduction, Crust-Mantle Décollement and Crustal-Stacking Wedge in the Himalayas and Other Collision Belts. Geological Society of London Special Publication, 19, 37-50.
http://dx.doi.org/10.1144/GSL.SP.1986.019.01.02

[5] 曾融生, 丁志峰, 吴庆举. 喜马拉雅–祁连山地壳构造与大陆–大陆碰撞过程[J]. 地球物理学报, 1998, 41(1): 49-60.

[6] 孙鸿烈, 郑度. 青藏高原形成演化与发展[M]. 广州: 广东科技出版社, 1998.

[7] 施雅风, 李吉均, 李炳元, 等. 青藏高原晚新生代隆升与环境变化[M]. 广州: 广东科技出版社, 1998.

[8] Owens, T.J. and Zandt, G. (1997) Implications of Crustal Property Variations for Models of Tibetan Plateau Evolution. Nature, 387, 37-43.
http://dx.doi.org/10.1038/387037a0

[9] Kosarev, G., Kind, R., Sobolev, S.V., Yuan, X., Hanka, W. and Oreshin, S. (1999) Seismic Evidence for a Detached Indian Lithospheric Mantle beneath Tibet. Science, 283, 1306-1309.
http://dx.doi.org/10.1126/science.283.5406.1306

[10] 滕吉文, 张中杰, 王光杰, 等. 喜马拉雅碰撞造山带的深层动力过程与陆–陆碰撞新模型[J]. 地球物理学报, 1999, 42(4): 481-494.

[11] 许志琴, 姜枚, 杨经绥, 等. 青藏高原的地幔结构: 地幔羽、地幔剪切带及岩石圈俯冲板片的拆沉[J]. 地学前缘, 2004, 11(4): 329-343.

[12] Xiao, X.C., Liu, X., Gao, R., Kao, H. and Luo, Z.H. (2001) Collision Tectonics between the Tarim Block (Basin) and the Northwestern Tibet Plateau: New Observations from a Multidisciplinary Geoscientific Investigation in the Western Kunlun Mountains. Acta Geologica Sinica (English Edition), 75, 126-132.
http://dx.doi.org/10.1111/j.1755-6724.2001.tb00514.x

[13] 肖序常, 刘训, 高锐, 等. 西昆仑及邻区岩石圈结构构造演化[J]. 地质通报, 2002, 21(2): 63-68.

[14] 肖序常, 王军. 西昆仑–喀喇昆仑及其邻区岩石圈结构、演化中几个问题的探讨[J]. 地质论评, 2004, 50(3): 285- 294.

[15] Clark, M.K. and Royden, L.H. (2000) Topographic Ooze: Building the Eastern Margin of Tibet by Lower Crustal Flow. Geology, 28, 703-706.
http://dx.doi.org/10.1130/0091-7613(2000)28<703:TOBTEM>2.0.CO;2

[16] 滕吉文, 宋鹏汉, 毛慧慧. 当代大陆内部物理学与动力学研究的导向和科学问题[J]. 中国地质, 2014, 41(3): 675- 697.

[17] 张万平, 袁四化, 刘伟. 青藏高原南部雅鲁藏布江蛇绿岩带的时空分布特征及地质意义[J]. 西北地质, 2011, 44(1): 1-9.

[18] Yang, J.-S., Robinson, P.T., Jiang, C.-F. and Xu, Z.-Q. (1996) Ophiolites of the Kunlun Mountains, China and Their Tectonic Implications. Tectonophysics, 258, 215-231.
http://dx.doi.org/10.1016/0040-1951(95)00199-9

[19] 滕吉文, 司芗, 王谦身, 等. 青藏高原地球科学研究中的核心问题与理念的厘定[J]. 地球物理学报, 2015, 58(1): 103-124.

[20] Argrand, E. (1924) In Comptes Rendus. Con-gress Geologique International, The Proceedings of the 13th International Geological Congress, Liege, Belgium, Vol. 1, 171.

[21] Powell, C.M. and Conaghan, P.J. (1973) Plate Tectonics and the Himalayas. Earth and Planetary Science Letters, 20, 1-12.
http://dx.doi.org/10.1016/0012-821X(73)90134-9

[22] L. 利布特里, 著. 大地构造物理学和地球动力学[M]. 孙坦, 译. 北京: 地质出版社, 1986: 148-152.

[23] 滕吉文, 王绍舟, 姚振兴, 等. 青藏高原及其邻近地区的地球物理场特征与大陆板块构造[J]. 地球物理学报, 1980, 23(3): 254-268.

[24] Dewey, J.F. and Burke, K.C.A. (1973) Tibetan, Variscan and Precambrian Reactivation: Products of Continental Collision. The Journal of Geology, 81, 683-692.
http://dx.doi.org/10.1086/627920

[25] England, P. and Mckenzie, D. (1982) A Thin Viscous Sheet Model for Continental Deformation. Geophysical Journal International, 70, 295-321.
http://dx.doi.org/10.1111/j.1365-246X.1982.tb04969.x

[26] Vilotte, J.P., Daignieres, M. and Madariaga, R. (1982) Numerical Modeling of Intraplate Deformation: Simple Mechanical Models of Continental Collision. Journal of Geophysical Research, 87, 10709-10728.
http://dx.doi.org/10.1029/JB087iB13p10709

[27] Harrison, T.M., Copeland, P., Kidd, W.S.F. and Yin, A. (1992) Raising Tibet. Science, 255, 1663-1670.
http://dx.doi.org/10.1126/science.255.5052.1663

[28] Zhao, W.L. and Morgan, W.J. (1985) Uplift of Tibetan Plateau. Tectonics, 4, 359-369.

[29] Zhao, W.L. and Morgan, W.J. (1987) Injection of Indian Crust into Tibetan Lower Crust: A Two-Dimensional Finite Element Model Study. Tectonics, 6, 489-504.
http://dx.doi.org/10.1029/TC006i004p00489

[30] 李吉均, 文世宣, 张青松, 等. 青藏高原隆起的时代、幅度和形式探讨论[J]. 中国科学, 1979(6): 608-616.

[31] 李吉均. 青藏高原隆起的三个阶段及夷平面的高度和年龄[M]//青藏高原隆升与亚洲环境演变: 李吉均院士论文选集. 北京: 科学出版社, 2006: 65-70.

[32] 李吉均. 青藏高原的地貌演化与亚洲季风[J]. 海洋地质与第四纪地, 1999, 19(1): 1-10.

[33] 李廷栋. 青藏高原地质科学研究的新进展[J]. 地质通报, 2002, 21(7): 370-376.

[34] 马钦忠, 李吉均. 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[J]. 海洋地质与第四纪地质, 2003, 23(1): 27-34.

[35] 马钦忠, 李吉均. 青藏高原北缘晚新生代的差异性隆起特征[J]. 地学前缘, 2003, 10(4): 590-598.

[36] 肖序常. 开拓、创新, 再创辉煌——浅议揭解青藏高原之秘[J]. 地质通报, 2006, 25(1): 15-19.

[37] Tapponnier, P. and Molnar, P. (1976) Slip-Line Field Theory and Large-Scale Continental Tectonics. Nature, 264, 319-324.
http://dx.doi.org/10.1038/264319a0

[38] Tapponnier, P. and Molnar, P. (1977) Active Faulting and Tectonics in China. Journal of Geophysical Research, 82, 2905-2930.
http://dx.doi.org/10.1029/JB082i020p02905

[39] Tapponnier, P., Peltzer, G., Le Dain, A.Y., Armijo, R. and Cobbold, P. (1982) Propagating Extrusion Tectonics in Asia: New Insights from Simple Experiments with Plasticine. Geology, 10, 611-616.
http://dx.doi.org/10.1130/0091-7613(1982)10<611:PETIAN>2.0.CO;2

[40] Tapponnier, P., Peltzer, G. and Armijo, R. (1986) On the Mechanics of the Collision between India and Asia. Geological Society of London Special Publication, 19, 113-157.
http://dx.doi.org/10.1144/gsl.sp.1986.019.01.07

[41] 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, 15085-15117.
http://dx.doi.org/10.1029/JB093iB12p15085

[42] Tapponnier, P and Molnar, P. (1979) Active Faulting and Cenozoic Tectonics of the Tien Shan, Mongolia and Baykal Regions. Journal of Geophysical Research: Solid Earth, 84, 3452-3459.
http://dx.doi.org/10.1029/JB084iB07p03425

[43] 嵇少丞, 王茜, 孙圣思, 等. 亚洲大陆逃逸构造与现今中国地震活动[J]. 地质学报, 2008, 82(12): 1644-1667.

[44] Tapponnier, P., Lacassin, R., Leloup, P.H., Schärer, U., Zhong, D.L., Wu, H.W., Liu, X.H., Ji, S.C., Zhang, L.S. and Zhong, J.Y. (1990) The Ailao Shan/Red River Metamorphic Belt: Tertiary Left-Lateral Shear between Indochina and South China. Nature, 343, 431-437.
http://dx.doi.org/10.1038/343431a0

[45] Houseman, G.A., McKenzie, D.P. and Molnar, P. (1981) Convective Instability of A Thickened Boundary Layer and Its Relevance for the Thermal Evolution of Continental Convergent Belts. Journal of Geophysical Research: Solid Earth, 86, 6115-6132.
http://dx.doi.org/10.1029/JB086iB07p06115

[46] Molnar, P., England, P. and Martinod, J. (1993) Mantle Dynamics, Uplift of the Tibetan Plateau, and the Indian Monsoon. Reviews of Geophysics, 31, 357-396.
http://dx.doi.org/10.1029/93RG02030

[47] 恩格斯, 著. 自然辨证法[M]. 中共中央马克思恩格斯列宁斯大林著作编译局, 译. 北京: 人民出版社, 1971.

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