[1]
|
[1]Molnar P, Tapponier P. Cenozoic tectonics of Asia: Effects of a continental collision[J]. Science, 1975, 189(4201): 419~426
[2]Tapponier P, Molnar P. Active faulting and Cenozoic tectonics of the Ti an Shan, Mongolia and Baykal regions [J]. Journal of Geophysical Research, 197 9, 84: 3425~3459
[3]中国科学院新疆地理研究所. 天山山体演化[M]. 北京: 科学出版社, 1986, 17 8~187 [Xinjiang Institute of Geography, CAS. Tianshan mountain evolution[M]. Beijin g: Science Press, 1986.178~187]
[4]Nelson M, McCaffrey R, Molnar P. Source parameters for 11 earthquakes i n the Tian Shan, Central Asia, determined by P and SH waveform inversion[J]. J ournal of Geophysical Research, 1987, 92(B12):12629~12648
[5]Avouac J P, Tapponier P, Bai M, et al. Active thrusting and folding along the northern Tian Shan and Late Cenozoic rotation of the Tarim relative t o Dzungaria and Kazakhstan[J]. Journal of Geophysical Research, 1993, 98: 6755 ~6804
[6]高长林,崔可锐,钱一雄等. 天山微板块构造与塔北盆地[M]. 北京: 地质出版社, 1993.229~270. [Gao C, Cui K, Qian Y. Microplate tectonics in the Tians han and the northern Tarim basin[M]. Beijing: Geological Press, 1993. 229~270 ]
[7]Yin A, Nie S, Craig P, et al. Late Cenozoic tectonic evolution of t he southern Chinese Tian Shan [J]. Tectonics, 1998, 17(1): 1~27
[8]Burtman V S, Skobelev S F, Molnar P. Late Cenozoic slip on the Talas-Fe rghana fault, the Tian Shan, Central Asia[J]. Geological Society of America Bu lletin, 1996, 108: 1004~1021
[9]Burtman V S. Cenozoic crustal shortening between the Pamir and Tian Sha n and a reconstruction of the Pamir-Tian Shan transition zone for the Cretaceou s and Paleogene[J]. Tectonophysics, 2000, 319: 69~92
[10]Allen M B, Vincent S J, Wheeler P J. Late Cenozoic tectonics of the Kepingta ge thrust zone: Interpretation of the Tian Shan and Tarim Basin, Northwest China [J]. Tectonics, 18: 639~654
[11]陈杰,丁国瑜,Burbank D W,等. 中国西南天山山前的晚第三纪构造与地震活动[J] .中国地震,2001,17(2):134~155[Chen J, Ding G, Burbank D W, et al. Late C enozoic Tectonics and Seismicity in the southwestern Tianshan, China[J]. Earth quake Research in China, 2001, 17(2): 134~155]
[12]贾承造. 中国塔里木盆地构造特征与油气[M]. 北京: 石油工业出版社,1997.348~ 364[Jia C. Structure and oil-gas in Tarim basin, China[M]. Beijing: Petroleu m Industry Press, 1997. 348~364]
[13]Lu H, Howell D G, Jia D, et al. Rejuvenation of the Kuqa foreland basin, northern flank of the Tarim basin, northwest China[J]. International Geolog y Review, 1994, 36: 1151~1158]
[14]刘和甫,汪泽成,熊宝贤等. 中国中西部中、新生代前陆盆地与挤压造山带耦合分析 [J]. 地学前缘,2000,7(3):55~72[Liu H, Wang Z, Xiong B, et al. Coupling analysis of Mesozoic- Cenozoic foreland basin and mountain system in central and western China[J]. Earth Science Frontiers, 2000, 7(3): 55~72]
[15]刘和甫,梁慧社,蔡立国等. 天山两侧前陆冲断系构造样式与前陆盆地演化[J]. 地球科学,1994,19(6):727~741[Liu H, Liang H, Cai L, et al. Foreland thrus t system and basin evolution on both sides of Tianshan Mountains[J]. Earth Sci ence Journal of China University of Geosciences, 1994,19(6):727~741]
[16]何登发,李德生. 塔里木盆地构造演化与油气[M]. 北京: 地质出版社,1996. 44~6 7[He D, Li D. Tectonic evolution and oil-gas in the Tarim basin[M]. Beijing: Geological Press, 1996. 44~67]
[17]Lin C, Liu J, Zhang Y, et al. Depositional architecture of the Tertiary tectonic sequences and their response to foreland tectonism in the Kuqa depressi on, the Tarim Basin[J]. Science in China, Series D, 2002, 45(3): 250~258
[18]康志宏. 塔里木原型盆地分析[A]. 见: 康玉柱主编. 中国塔里木盆地石油地质文集 [C]. 北京: 地质出版社,1996.136~145[Kang Z. Proto-basin analysis in the Tar im[A]. In: Kang Y, ed. Symposium on petroleum geology in the Tarim basin, Chin a[C]. Beijing: Geological Press, 1996. 136~145]
[19]邓秀芹,岳乐平,滕志宏. 塔里木盆地周缘库车组、西域组磁性地层学初步划分[J]. 沉积学报,1998,16(2): 82~86[Deng X, Yue L, Teng Z, et al. A Primary Magne tostratigraphy Study on Kuche and Xiyu Formations on the Edge of Tarim Basin. Ac ta Sedimentologica Sinica, 1998, 16(2): 82~86]
[20]滕志宏,岳乐平,何登发等. 南疆库车河新生界剖面磁性地层研究[J]. 地层学杂志,1997,21(1): 55~62[Teng Z, Yue L, He D, et al. Magnetostratigraphic re search of Cenozoic section of Kuqa river area, South Xinjiang[J]. Journal of s tratigraphy, 1997, 21(1): 55~62]
[21]Dickinson W R, Suczek C A. Plate tectonics and sandstone compositions[J]. AAPG Bull., 1979, 63(12): 2164~2182
[22]李忠,李任伟,孙枢等. 合肥盆地南部侏罗系砂岩碎屑组分特征及其物源构造属性[ J]. 岩石学报,1999,(3):438~445[Li Z, Li R, Sun S, et al. Detrital compo sition and provenance tectonic attributes of Jurassic sandstones, South Hefei Ba sin[J]. Acta Petrologica Sinica, 1999, 15(3): 438~445]
[23]Reading H G. 沉积环境和相(周明鉴,陈昌明,张疆,等译)[M]. 北京: 科学出版社 ,1991. 552~553[Reading H G. Sedimentary environments and facies[M]. Beijing : Science Press, 1991. 552~553]
[24]Zhang P, Molnar P, Downs W R. Increased sedimentation rates and grain sizes 2±4 Myr ago due to the infuence of climate change on erosion rates[J]. Natur e, 2002, 410: 891~897
[25]Hendrix M S, Graham S A, Carrol A R, et al. Sedimentary record and clima tic implication of recurrent deformation of the Tian Shan: Evidence from Mesozoi c strata of the north Tarim, south Junggar and Turpan basins[J]. Geol Soc Am Bull,1992,104:53~79
[26]Hendrix M S. Evolution of Mesozoic sandstone compositions, southern Junggar, northern Tarim, and western Turpan basins, Northwest China: A detrital record o f the ancestral Tian Shan[J]. Journal of Sedimentary Research, 2000,70(3): 52 0~532
[27]An Z, Kutzbach J E, Prell W L, et al. Evolution of Asian monsoons and ph ased uplift of theHimalaya-Tibetan plateau since Late Miocene times [J]. Natu re, 2001, 411: 62~66
[28]Guo Z T, Ruddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China[J]. Nature, 2001, 416: 159~ 163
[29]Zheng H, Chen H, Cao J. Palaeoenvironmental implication of the Plio-Pleisto cene loess deposits in southern Tarim Basin[J]. Chinese Science Bulletin, 2002 , 47(8): 700~704
[30]Dumitru T A, Zhou D, Chang E, et al. Uplift, exhumation, and deformation in the Chinese Tian Shan[A]. In: Hendrix M S, Davis G A, eds. Paleozoic and M esozoic Tectonic Evolution of Central and Eastern Asia: From Continental Assembl y to Intra-continental Deformation[C]. Geological Society of America Memoir 1 94, 2001. (in press)
[31]杨庚,钱祥麟.中新生代天山板内造山带隆升证据: 锆石、磷灰石裂变径迹年龄测定[ J]. 北京大学学报(自然科学版), 1995, 31(4): 473~478[Yang G, Qian X. Mesozoic- Cenozoic uplift of the Tianshan intraplate orogenic belt: evidence from zircon a nd apatite fission track datin[J]. Acta Scientiarum Naturalium, Universitatis Pekinensis, 1995, 31(4): 473~478]
[32]王永兴,王树基. 天山南北麓山前坳陷的第四纪构造变动[J]. 干旱区地理,1994,1 7(4):38~45[Wang Y, Wang S. Quaternary tectonism in the foredepression of Tians han mountains[J]. Arid Land Geography, 1994, 17(4): 38~45]
[33]Zhou S, Jiao K, Zhao J, et al. Geomorphology of the Urümqi River Valley and the uplift of the Tianshan Mountains in Quaternary[J]. Science in China Series D, 2002, 45(11): 961~968
[34]Rea D K. Delivery of Himalayan sediment to the northern Indian Ocean and its relation to global climate, sea level, uplift, and seqwater strontium[J]. Geo phys Monogr, 1992, 70: 387~402
[35]钟大赉,丁林. 青藏高原隆升过程及其机制的探讨[J]. 中国科学,D辑,1996,26( 4):289~295[Zhong D, Ding L. A research on uplift process of the Tibetan Platea u and their mechanism[J]. Science in China Series D, 1996, 26(4): 289~295]
[36]李吉均,方小敏,马海洲等. 晚第三纪黄河上游地貌演化与青藏高原隆起[J]. 中国科学,D辑,1996,26(4): 316~322[Li J, Fang X, Ma H, et al. Late Tertiar y relief evolution in the upstream of Huang river and uplift of the Tibetan Plat eau[J]. Science in China Series D, 1996, 26(4): 316~322]
[37]李吉均,方小敏. 青藏高原隆起与环境变化研究[J]. 科学通报,1998,13(15): 156 9~1574[Li J, Fang X. A research on Uplift of the Tibetan Plateau and environme nt change[J]. Chinese Science Bulletin, 1998, 13(15): 1569~1574]
[38]England P, Molnar P. Inferences of deviatoric stress in actively deforming b elts from simple physical models[J]. Phil Trans R Soc Lond A,1991,337,151~ 164
[39]Gawthorpe R L, Leeder M R. Tectono-sedimentary evolution of active extensio nal basins[J]. Basin Research,2000,12:195~218 |