Ollier C D, Pain C F. The Origin of Mountains[M]. Routledge, London. 2000.
[3]
Markley M, Norris R J. Structure and neotectonics of the Blackstone Hill antiform, Central Otago, New Zealand [J].New Zealand Journal of Geology and Geophysics, 1999, 42: 205-218.
[4]
Ruddiman W F, Kutzbach J E. Forcing of late Cenozoic northern hemisphere climate by plateau uplift in southern Asia and the American West[J]. J. Geophys. Res., 1989, 94(D): 18409-18427.
[5]
Coleman M, Hodges K. Evidence for Tibetan Plateau uplift before 14 Myr ago from a new minimum age of east-west extension[J]. Nature, 1995, 374: 49-52.
[6]
Harrison T, Copeland P, Kidd W S F, et al. Raising Tibet [J]. Science, 1992, 255: 1663-1670.
Judson S, and Ritter D F. Rates of regional denudation in the United States[J]. Jour. Geophys. Res., 1964, 69: 3359-3401.
[10]
Schumm S A. The disparity between present rates of denudation and orogeny[J]. U.S. Geol. Survey Prof. Paper, 1963,454-H,13pp.
[11]
Ahnert F. Functional relationships between denudation, relief and uplift in large mid-latitude drainage basins[J]. American Journal of Science, 1970, 268: 243-263.
[12]
King L C. Fair T J D. Hillslopes and dongas[J]. Trans.Proc. Geol. Soc. S. Africa, 1944,47: 1-4.
[13]
Young A, Saunders 1. Rates of surface processes and denudation[A]. In: A.D. Abrahams (ed.) Hill slope processes[C].Allen & Unwin, Inc. Boston and New York, 1986, 3-27.
[14]
Budel J. Double Surfaces of Leveling in the humid tropics[A].Adams G. Planation Surfaces[C]. Halsted Press, 1975, 361-366.
[15]
French H M. The Periglacial Environment[M]. London:Longrnan, 1976.
[16]
Czudek T, Demek J. Thermokarst in Siberia and its influence on the development of lowland relief [ J]. Quaternary Research, 1970, 1: 103-120.
[17]
Rapp A. Recent development of mountain slopes in Karkevagge and surroundings, northern Scandinavia[J]. Geografiska Annaler, 1960, 42:71-200.
Coltori M, Ollier C D. Geomorphic and tectonicevolution of the Ecuadoran Andes[J]. Geomorphology, 2000, 32: 1-19.
[26]
Eder N, Neubauer F. On the edge of the extruding Wedge:neogene kinematics and geomorphology along the southern Niedere Tauern, eastern Alps [ J]. Eclogae Geologicae Helvetiae,2000, 93: 81-92.
[27]
Stirling M W. The Old Man Range and Garvie Mountains-tectonic geomorphology of the central Otago peneplain, New Zealand[J].New Zealand Journal of Geology and Geophysics,1990, 33:233-243.
[28]
Guo Z T, Ruddiman W F. Onset of Asian desertification by 22Myr ago inferred from loess deposits in China [J]. Nature,2002, 416: 159-163.
Li J J et al. Uplift of the Qinghai-Xizang (Tibet) Plateau and global change [ M]. Lanzhou: Lanzhou University Press,1995.
[31]
Davis W M. The Geographical Cycle[J]. Geogr. J., 1899,14(A): 481-503.
[32]
Bloom A L. Geomorphology: a systematic analysis of late Cenozoic landforms (2nd ed. )[M]. Pretice-Hall, Inc. 1991.
[33]
崔之久,李德文,伍永秋,等关于夷平面[J].科学通报,1998,43(17):1794～1804
[34]
Ruxton B P, and McDougall I. Denudation rates in northeast Papua from potassium-argon dating of lavas[J]. American Journal of Science, 1967, 265:545-561.
[35]
Molnar P, England P. Late Cenozoic Uplift of the mountain range and global climatic change: Chicken or egg? [J]. Nature, 1990, 346: 29-34.
[36]
Young A. Slopes[M]. London and New York: Longman,1972.
[37]
Shockleton R M, Chang C F. Cenozoic uplift and deformation of the Tibetan Plateau: the geomorphologic evidence[J]. Phil.Trans. R. Soc. Lond., 1988, A: 327-377.
