参考文献/References:
[1] Lee C S, Louis L T. A quantitative analysis for geomorphic indices of longitudinal river profile: a case study of the Choushui River, Central Taiwan[J]. Environmental Earth Sciences, 2010, 59(7): 1549-1558
[2] Ferraris F, Firpo M, Pazzaglia FJ. DEM analyses and morphotectonic interpretation: the Plio-Quaternary evolution of the eastern Ligurian Alps, Italy[J]. Geomorphology, 2012, (149-150): 27-40
[3] Wobus C, Whipple K X, Kirby E,et al. Tectonics from topography: procedure, promise, and pitfalls[J]. Geological Society American Special Paper, 2006, 398: 55-74
[4] Whipple K X. Bedrock rivers and the geomorphology of active orogens[J]. Annual Review of Earth Planetary Sciences, 2004, (32):151-185
[5] Kirby E,Whipple K X, Tang W,et al. Distribution of active rock uplift along the eastern margin of the Tibetan Plateau: inferences from bedrock channel longitudinal profles[J]. Journal of Geophysical Research, 2003, 108(B4): 2217
[6] Kirby E,Whipple K X. Expression of active tectonics in erosional landscapes[J]. Journal of Structural Geology, 2012, 44: 54-75
[7] Ismail E H, Abdelsalam M G. Morphotectonic analysis of the Tekeze River and the Blue Nile drainage systems on the Northwestern Plateau, Ethiopia[J].Journal of African Earth Sciences, 2012, 69: 34-47
[8] Brookfield M E. The evolution of the great river systems of southern Asia during the Cenozoic India-Asia collision: rivers draining southwards[J]. Geomorphology,1998(22): 285-312
[9] RAdoane M, RAdoane N, Dumitriu D. Geomorphological evolution of longitudinal river profiles in the Carpathians[J]. Geomorphology,2003, 50: 293-306
[10] Tapponnier P, Xu Z Q, Roger F,et al. Oblique stepwise rise and growth of the Tibet Plateau[J]. Science, 2001, 294: 1671-1677
[11] Jia Yingying, Fu Bihong, Wang Yan,et al. Late Cenozoic Tectonogeomorphic growth and drainage response in the Longmen shan fault zone, East margin of Tiben[J]. Quaternary Sciences,2010, 30(4):825-836[贾营营, 付碧宏, 王岩石, 等. 青藏高原东缘龙门山断裂带晚新生代构造地貌生长及水系响应[J]. 第四纪研究, 2010, 30(4):825-836]
[12] Zhang Huiping,Yang Nong,Zhang Yueqiao,et al. Geomorphology of the Minjiang drainage system(Sichuan,China)and its structural implications[J]. Quaternary Sciences,2006,26(1):126-135[张会平,杨农,张岳桥,等. 岷江水系流域地貌特征及其构造指示意义[J].第四纪研究,2006,26(1):126-135]
[13] Zhang Huiping, Zhang Peizhen, Wu Qinglong,et al. Characteristics of the Huanghe River longitudinal profiles around Xunhua-Guide Area(NE Tibet) and their tectonic significance[J]. Quaternary Sciences,2008, 28(2): 299-309.[张会平, 张培震, 吴庆龙, 等.循化- 贵德地区黄河水系河流纵剖面形态特征及其构造意义[J]. 第四纪研究, 2008, 28(2): 299-309]
[14] Wang Yan, Liu Shaofeng, Gao Mingxing,et al. Geomorphology of the Taohe River drainage system and its structural implications[J]. Earth Science Frontiers, 2010, 17(4): 43-49[王岩, 刘少峰, 高明星, 等. 洮河水系流域地貌特征及其构造指示意义[J].地学前缘, 2010, 17(4): 43-49]
[15] Hu Xiaofei, Pan Baotian, Kirby E,et al. Spatial difference in rock uplift rates inferred from channel steepness indices along the northern flank of the Qilian Mountain, northeast Tibetan Plateau[J].Chinese Sci Bull, 2010,55(23): 2329-2338[胡小飞, 潘保田, Kirby E, 等.河道陡峭指数所反映的祁连山北翼抬升速率的东西差异[J]. 科学通报, 2010,55(23): 2329-2338]
[16] Ji Yapeng, Gao Hongshan, Pan Baotian,et al. Implication of active structure in the upper reaches of Weihe river basin from stream lengthgradient index(SL index) and Hack profiel[J]. Journal of Lanzhou University:Natural Sciences,2011, 47(4):1-6[吉亚鹏, 高红山, 潘保田, 等.渭河上游流域河长坡降指标SL参数与Hack剖面的新构造意义[J].兰州大学学报:自然科学版,2011, 47(4): 1-6]
[17] Cheng Sanyou, Wang Hongmei, Li Yingjie. Geomorphology Characteristics of the Wei River Basin and Its Formation Reasons[J]. Geography and GeoInformation Science,2011, 27(3): 45-49.[程三友, 王红梅, 李英杰. 渭河水系流域地貌特征及其成因分析[J]. 地理与地理信息科学, 2011, 27(3): 45-49]
[18] Yan Zhaokun, Liyong, Huang Runqiu,et al. Geomorphic evolution process of Pingtong River watershed in the north Longmenshan, China[J]. Mountain Research, 2012, 30(2): 136-146.[颜照坤, 李勇, 黄润秋, 等. 龙门山北段平通河流域地貌演化过程[J].山地学报, 2012, 30(2): 136-146]
[19] Zhang Maosheng,Li Zhiheng,Wang Genlong,et al. The geological hazard characteristics and exploration ideas of the Bailong River Basin[J]. Northwestern Geology,2011,44(3):1-9[张茂省,黎志恒,王根龙,等. 白龙江流域地质灾害特征及勘查思路[J]. 西北地质, 2011,44(3):1-9]
[20] Zhan Wenwu. The research of Engineering geological problems in the section of gansu province of Lanzhou-Haikou highway[M]. Lanzhou:Lanzhou University Press, 2006: 8-44[谌文武,等. 兰州-海口高速公路甘肃段工程地质问题研究[M].兰州:兰州大学出版社,2006:8-44]
[21] Zhao Hongzhuang, Li Youli, Yang Jingchun,et al. The longitudinal profiles of the Ten Rivers in North Tianhan Mountains and their tectonic significance[J]. Acta Geographica Sinica, 2009, 64(5): 563-570[赵洪壮, 李有利, 杨景春, 等. 天山北麓河流纵剖面与基岩侵蚀模型特征分析[J]. 地理学报, 2009, 64(5): 563-570]
[22] Howard A D, Kerby G. Channel changes in badlands[J]. Geological Society American Bulletin, 1983, 94:739-752
[23] Whipple K X, Hancock G S, Anderson R A. River incisions into bedrock:Mechanics and relative efficacy of plucking abrasion, and cavitations[J].Geological Society of America Bulletin, 2000, 112(3): 490-503
[24] Flint J J. Stream gradient as a function of order, magnitude, and discharge[J]. Water Resources Research,1974,10:969-973
[25] Hack J T. Streamprofile analysis and streamgradient index[J]. Journal of Research of the U.S. Geological Survey, 1973, 4:421-429
[26] Snyder N P, Whipple K X, Tucker G E,et al. Landscape response to tectonic forcing: Digital elevation model analysis of stream profiles in the Mendocino triple junction region, northern California[J]. Geological Society of American Bulletin, 2000, 112:1250-1263
[27] Zhang Huiping,Zhang Peizhen,Yuan Daoyang,et al. Differential landscape development of the central N-S seismic zone and its relation to the west Qinling tectonic belt[J]. Quaternary Science,2010,30(4):803-811[张会平,张培震,袁道阳,等. 南北地震带中段地貌发育差异性及其与西秦岭构造带关系初探[J]. 第四纪研究,2010,30(4):803-811]
[28] Li Zhiwu,Liu Shugen,Chen Hongde,et al. Structural segmentation and zonation and differential deformation across and along the Longmen thrust belt,West Sichuan,China[J]. Journal of Chengdu university of technology:Science&Technology Edition,2008,35(4):440-454[李智武,刘树根,陈洪德,等. 龙门山冲断带分段-分带构造格局及其差异变形特征[J].成都理工大学学报:自然科学版,2008,35(4):440-454]
[29] Li Chuanyou,Song Fangmin,Ran Yongkang. Late quaternary activity and age constraint of the northern longmenshan fault zone[J]. Seismology And Geology,2004,26(2):248-257[李传友,宋方敏,冉永康. 龙门山断裂带北段晚第四纪活动性讨论[J]. 地震地质,2004,26(2):248-257]
[30] Chen Lichun,Chen Jie,Liu Jinfeng,et al. Investigation of late quaternary activity along the northern rangefront fault,longmenshan[J]. Seismology and Geology,2008,30(3):710-722 [陈立春, 陈杰, 刘进峰, 等. 龙门山前山断裂北段晚第四纪活动性研究[J]. 地震地质, 2008, 30(3): 710-722]
[31] Deng Qidong,Chen Shefa,Zhao Xiaolin. Tectonics,scismisity and dynamics of Longmenshan mountains and its adjacent regions[J]. Seismology and geology,1994,16(4):389-403[邓起东,陈社发,赵小麟. 龙门山及其邻区的构造和地震活动及动力学[J].地震地质,1994,16(4): 389-403]
[32] Duvall A, Kirby E, Burbank D. Tectonic and lithologic controls on bedrock channel profiles and processes in coastal California[J]. Journal of Geophysical Research, 2004, 109: F03002.
[33] Yuan Daoyang,Zhang Peizhen,Liu Baichi,et al. Geometrical imagery and Tectonic transformation of late Quaternary active Tectonics in Northeastern Margin of Qinghai-Xizang Plateau[J]. Acta Geologica Sinica,2004,78(2):270-278[袁道阳,张培震,刘百篪,等.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[J].地质学报,2008,78(2):270-278]
[34] Yu Jingxing,Zheng Wenjun,Yuan Daoyang,et al. Late Quaternary active characteristics and sliprate of pingdinghuama fault,the eastern segment of guanggaishandieshan fault zone(West Qinling Mountain)[J]. Quaternary Sciences,2012,32(5):957-967[俞晶生,郑文俊,袁道阳,等. 西秦岭西段光盖山-迭山断裂带坪定-化马断裂的新活动性与滑动速率[J].第四纪研究,2012,32(5):957-967]
[35] Snyder N P, Whipple K X, Tucker G E,et al. Importance of a stochastic distribution of floods and erosion thresholds in the bedrock river incision problem[J]. Geophysics Res., 2003, 108(B2): 2117