[1]Li Jijun,Wen Shixuan,Zhang Qingsong,et al. A discussion on Time, amplitude and type of the Qinghai-Tibet plateau[J].Science in China(Series B),1979,9(6):608-616.[李吉均,文世宣,张青松,等.青藏高原隆升的时代、幅度和形式探讨[J].中国科学:B辑，1979，9（6）：608-616.]
[2]Quade J, Cerling T E, Bowman J R. Development of Asian monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan[J].Nature,1989,342:163-166.
[3]Raymo M F, Ruddiman W F. Tectonic forcing of late Cenozoic ulimate[J]. Nature,1992,359: 117-122.
[4]Edmonds J. Himalayan tectonics, weathering processes, and the strontium isotope record in marine limestones[J].Science,1992 ,258: 1 594-1 597.
[5]Prell W L, Kutzbach J E. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution[J]. Nature, 1992,360 :647-652.
[6]Richter F, Rowley D B, DePaolo D J. Sr isotope evolution of seawater the role of tectonics[J].Earth and Planet Science Letter,1992,109 :11-23. 
[7]Derry L A, France-Lanord C. Neogene Himalayan weathering history and river ⁸⁷Sr/⁸⁶Sr: Impact on the marine Sr record[J].Earth and Planet Science Letter,1996,142:59-74.
[8]Ramstein G, Fluteau F,Besse J, et al. Effects of orogeny, plate motion and land-sea distribution on Eurasian climate change over the past 30 million years[J].Nature,1997,386:788-795.
[9]Ruddiman W. Early uplift in Tibet?[J].Nature,1998,394:723-725.
[10]An Z, Kutzbach J E, Prell W L, et al. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since Late Miocene times[J].Nature, 2001,411:62-66.
[11]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, 2002,416:159-163.
[12]England P, Housemann G. Finite strain calculations of continental deformation Ⅱ: Application to the India-Asia plate collision[J].Journal Geophysical Research,1986,91:3 664-3 676.
[13]Harrison T M, Copeland P, Kidd W S F,et al. Raising Tibet[J].Science,1992,255:1 663-1 670.
[14]Molnar P, England P, Martinod J. Mantle dynamics, uplift of the Tibetan plateau, and the Indian Monsoon[J]. Review Geophysics,1993,31:357-396.
[15]Royden L H, Burchfiel B C, King K W, et al. Surface deformation and lower crustal flow in eastern Tibet[J].Science,1997,276: 788-790.
[16]Tapponnier P, Xu Zhiqin, Roger F, et al. Oblique stepwise rise and growth of the Tibet plateau[J].Science,2001,294:1 671-1 677.
[17]Beaumont C, Jamieson R A, Nguyen M H, et al. Crustal channel flows: 1. Numerical models with applications to the tectonics of the Himalayan-Tibetan orogen[J]. Geophysical Research,2004,109, B06406, doi:10:1029/2003JB002809.
[18]Rowley D B,Currie B S.Paleoaltimetry of the late Eoene to Miocene unpola basin,central Tibet[J].Nature,2006,439:677-681.
[19]Mulch A, Graham S A, Chamberlain C P. Hydrogen isotopes in Eocene River Gravels and paleoelevation of the sierra nevada[J].Science,2006,313:87-89.
[20]Forest C E, Emanuel K A, Molnar P,et al. Paleoaltimetry incorporating atmospheric physics and botanical estimates of paleoclimate[J].Geology Society of America Bulletin,1999,111:497-511. 
[21]Spicer R A, Harris N B W, Widdowson M, et al. Constant elevation of southern Tibet over the past 15 million years[J].Nature,2003,421:622-624 .
[22]Sahagian D L, Maus J E. Basalt vesicularity as a measure of atmospheric pressure and paleoelevation[J].Nature,1994,372:449-551.
[23]Drummond C N,Wilkinson B H,Lohmam K C,et al.Effect of regional topography and hydrology on the lacustrine isotopic record of Miocene paleoclimate in the Rocky Mountains[J].Palaeogeography,Palaeoclimatoloty,Palaeoecology,1993,101:67-79.
[24]Chamberlain C P, Poage M A. Reconstructing the paleotopography of mountain belts from the isotopic composition of authigenic minerals[J].Geology,2000,28:115-118.
[25]Dettman D L, Lohmann K. Oxygen isotope evidence for high-altitude snow in the Laramide Rocky Mountains of North America during the Late Cretaceous and Paleogene[J].Geology,2000,28:243-246.
[26]Garzione C N, Quade J, DeCelles P G, et al. Predicting paleoelevation of Tibet and the Himalaya from δ¹⁸O  vs altitude gradients in meteoric water across the Nepal Himalaya[J].Earth and Planet Science Letter,2000,183:215-229.
[27]Poage M A, Chamberlain C P. Empirial relationship between elevation and the stable isotope composition of precipitation: Considerations for studies of paleoelevation change[J].America Journal of Science (in review),2001,301:1-15.
[28]Poage M A, Chamberlain C P. Stable isotopic evidence for a pre-Middle Miocene rain shadow  in the western Basin and Range: Implications for the surface uplift of the Sierra Nevada[J].Tectonics,2002,21:16-1-16-10.
[29]Kohn M J, Miselis J L, Fremd T J.Oxygen isotope evidence for progressive uplift of the Cascade Range, Oregon[J].Earth and Planet Science Letter,2002,204:151-165.
[30]Dettman D L,Fang X M, Garzione C N. Uplift-driven climate change at 12Ma: A long δ¹⁸O record from the NE margin of the Tibetan Plateau[J].Earth and Planet Science Letter,2003,214:267-277.
[31]Cyr A J, Currie B S, Rowley D B. ochemical and stable isotopic evaluation of fenghuoshan Group lacustrine carbonates, north-central Tibet:Implications for the paleoaltimetry of Late Eocene Tibetan Plateau [J].Geology,2005,113:517-533.
[32]Takeuchi A, Larson P B. Oxygen isotope evidence for the late Cenozoic development of an orographic rain shadow in eastern Washington[J].Geology,2005,33:313-316.
[33]Garzione C N,Molnar P, Libarkin J C, et al. Rapid late Miocene rise of the Bolivian Altiplano: Evidence for removal of mantle lithosphere[J].Earth and Planet Science Letters,2006,241:543-556.
[34]Rowley D B, Garzione C N. Stable isotopic-based paleoaltimetry[J].The Annual Review of Earth and Planetary Sciences,2007,35:463-508.
[35]Urey H C. The thermodynamic properties of isotopic substances[J].Journal of the Chemical Society(London),1947:562-581.
[36]Benson L V, White L D, Rye R. Carbonate deposition, Pyramid Lake Subbasin, Nevada:Comparison of the stable isotope values of carbonate deposits (tufas) and the Labontan lake-level record[J].Palaeogeography, Palaeoclimatology, Palaeoecology,1996,122:45-76. 
[37]Teranes J L, McKenzie J A, Bernasconi S M, et al. A study of isotopic fractionation during bio-induced calcite precipitation in eutrophic Baldeggersee[J].Geochimica et Cosmochimica Acta,1999,63:1 981-1 989.
[38]Dansgaard W. Stable isotopes in precipitation[J].Tellus,1964,16:436-468.
[39]Ambach W, Dansgaard W, Eisner H, et al. The altitude e ect on the isotopic composition of precipitation and glacier ice in the Alps[J].Tellus,1968,20:595-600.
[40]Joussaume J,Sadourny R,Jouzel J A.General circulation model of water isotopes in the atmosphere[J].Nature,1984,311:24-29.
[41]IAEA. Statistical Treatment of Data on Environmental Isotopes in Precipitation[C]//International Atomic Energy Agency. Vienna, 1992.
[42]Chamberlain C P, Poage M A,Craw D, et al. Topographic development of the southern Alps recorded by the isotopic composition of authigenic clay minerals, South Island, New Zealand[J].Chemical Geology,1999,155:279-294.
[43]Currie B S, Rowley D B, Tabor N J. Middle Miocene paleoaltimetry of southern Tibet: Implications for the role of mantle thickening and delamination in the Himalayan orogen[J].Geology,2005,33:181-184.
[44]Graham S A,Chamberlain P C,Yue Y J,et al.Stable isotope records of Cenozoic climate and topography, Tibetan plateau and Tarim basin[J].American Journal of Science,2005,305:101-118.
[45]Rowley D B, Pierrehumbert R T, Currie B S.A new approach to stable isotope-based paleoaltimetry: Implications for paleoaltimetry and paleohypsometry of the High Himalaya since the Late Miocene[J].Earth and Planet Science Letter,2001,188:253-268.
[46]Cyr A J. Geochemical and stable isotopic evaluation of Fenghuoshan Group lacustrine carbonates,north-central Tibet: Implications for the paleoaltimetry of the mid-Tertiary Tibetan Plateau[D]. Oxford OH:Miami University, 2004.
[47]Turner J V, Fritz P, Karrow P F, et al. Isotopic and geochemical composition of marl lake waters and implications for radio carbon dating of marl lake sediments[J].Canada Journal of Earth Science,1983,20:599-615. 
[48]McKenzie J A. Carbon Isotopes and Productivity in the Lacustrine and Marine Environment[C]//Stumm W,ed. Chemical Processes in Lakes.New York:Wiley,1985:99-118.
[49]Fritz P, Morgan A V, Eicher U, et al. Stable isotope, fossil coleoptera and pollen stratigraphy in Late Quaternary sediments from Ontario and New York state[J].Palaeogeography, Palaeoclimatology, Palaeoecology,1987,58:183-202.
[50]Gasse F, Fontes J C. Paleoenvironments and paleohydrology of a tropical closed lake (Lake Asal, Djibouti) since 10 000 yr BP[J].Palaeogeography, Palaeoclimatology, Palaeoecology,1987,69:67-102.
[51]Talbot M R. 1990. A review of the paleohydrological interpretation of carbon and oxygen isotopic ratios in primary lacustrine carbonates[J].Chemical Geology,1990, 80:261-279.
[52]Drummond C N. Climatic control of fluvial-lacustrine cyclicity in the Cretaceous Cordilleran foreland basin, western United States [J].Sedimentology,1996, 43:677-689.
[53]Kalnay E, Kanamitsu M, Kistler R, et al. The NCEP/NCAR 40-year reanalysis project[J].Bulletin of the America Meteorology Society,1996, 77:437- 471.
[54]Friedman I,O'Neil J R.Compilation of stable isotope fractionation factors of geochemical interest[C]//Fleischer M,ed.Data of geochemistry,US Geology Survey Professor Paper,1977.
[55]Garzione C N, Dettman D L, Horton B K. Carbonate oxygen isotope paleoaltimetry: Evaluating the effect of diagenesis on paleoelevation estimates for the Tibetan Plateau[J].Palaeogeogragy, Palaeoclimatology, Palaeolecology,2004, 212:119-140.
[56]Ghosh P, Garzione C N, Eiler J M. Rapid uplift of the Altiplano revealed in ¹³C-¹⁸O bonds in paleosol carbonates[J].Science,2006,311:511-515.