Brook J E, Brown E T, Kurz M D, Ackert Jr R P, Raisbeck G M,Yiou F. 1995.Constraints on age,erosion,and uplift of Neogene glacial deposits in the TransantarcticMountains determined from in situ cosmogenic 10Be and 26A1. Geology, 23(12):1063~1066.
[7]
Brook E J, Nesje A, Lehman S J, Raisbeck G M, Yiou F. 1996.Cosmogenic nuclideexposure ages along a vertical transect in western Norway:Implications for the height ofthe Fennoscandian ice sheet. Geology, 24(3) :207~210.
[8]
Cui Z J. 1964. On the Quaternary glacier types of Western China. Acta GeologicalSinica, 44 (2): 229~ 246 (in Chinese with English abstract).
[9]
Garzione C N, Quade J, DeCelles P G, English N B. 2000. Predicting paleoelevationof Tibet and the Himalaya from δ 18O vs altitude gradients in meteoric water across theNepal Himalaya. Earth and Planetary Science Letter, 183: 215~ 229.
[10]
Harrison T M, Copeland P, Kidd W S F, Yin A. 1992. Rising Tibet.Science, 255:1663~1670.
[11]
Li B Y, Li J J. 1991. Map of the Quaternary Glaciers Distribution on theQinghai-Tibetan Plateau. Beijing: Science Press of China (in Chinese).
[12]
Li J J. 1999. Landform evolution of the Qinghai-Xizang Plateau and the AsianMonsoon. Marine Geology and Quaternary Geology, 19(2):60~ 72 (in Chinese with Englishabstract).
[13]
Nishiizumi K, Kohl C P, Arnold J R, Klein J, Fink D, Middleton R.1991. Cosmic rayproduced 10Be and 26Al in Antarctic rocks:exposure and erosion history. Earth andPlanetary Science Letter,104:440~454.
[14]
Prell W L, Kutzbach J E. 1992. Sensitivity of the Indian Monsoon to forcingparameters and implications for its evolution. Nature, 36:647~652.
[15]
Shi Y F. 1998. Middle Quaternary crysphere evolution of the Qinghai Xizang Plateauand its relationship to the global change.J. of Glaciology and Geocrylogy, 20 (3): 197 ~207 (in Chinese with English abstract).
[16]
Stone J O. 2000. Air presure and cosmogenic isotope production. Journal ofGeophysical Research, 105(B10):23753~23759.
[17]
Wang J, Wang Y J, Liu Z C, Li J Q, Xi P. 1999. Cenozoic environmental evolution ofthe Qaidam Basin and its implications for the uplift of the Tibetan Plateau and the dryingof the central Asia. Palaeogeography, Palaeoclimatology, Palaeoecology, 152:37~47.
[18]
Wang J, Xi P, Liu Z C, Wang Y J. 1996. Cenozoic environmental and topographicalevolution of Qaidam Basin. Geological Review,42(2): 166~173 (in Chinese with Englishabstract).
[19]
Wu X H, Li Y Z. 1990. Moraines and environments of the Qinghai Xizang Plateau.Quaternary Science in China, 2: 146~ 158 (inChinese with English abstract).
[20]
Yiou F, Raisbeck G M, Bourles D, Lestringuez J, Deboffle D. 1986.Measurement of10Be and 26A1 with a Tandetron accelerator mass spectrometer facility. Radiocarbon, 2A:198~203.
[21]
Zhou S Z, Li J J. 2001. A new study on Qinghai- Tibetan Plateau in Ice Ages. EarthScience Frontiers, 8 (1): 67~ 75 (in Chinese with English abstract).
Bierman P R, Marsella K A, Patterson C, Davis P T, Caffee M.1999. Mid-Pleistocenecosmogenic minimum-age limits for preWisconsinan glacial surfaces in southwesternMinnesota and southern Barf in Island: a multiple nuclide approach.Geomorphology, 27:25~39.
[30]
Briner J, Swanson T W. 1998. Using inherited cosmogenic 36C1 to constrain glacoalerosion rate of the cordilleran ice sheet. Geology,26(1):3~6.
[31]
Brown E T, Edmond J M, Raisbeck G M, Yiou F, Kurz M D, Brook E J. 1991.Examination of surface exposure ages of Antarctic moraines using in situ produced 10 Beand 26 Al. Geochimica et Cosmochimica Acta, 55: 2269 ~ 2283.
[32]
Bruno L A, Baur H, Graf T, Schluchter C. 1997. Dating of Sirius Group tillites inthe Antarctic Dry Valleys with cosmogenic 3He and 21Ne. Earth and Planetary ScienceLetter, 147:37~54.
[33]
Dunai T J. 2000. Scaling factors for production rates of in situ producedcosmogenic nuclides: a critical reevaluation. Earth and Planetary Science Letter, 176:157~169.
[34]
Dunne J, Elmore D, Muzikar P. 1999. Scaling factors for the rates of production ofcosmogenic nuclides for geometric shieling and attenuation at depth on sloped surfaces.Geomorphology, 27:3~11.
[35]
Gosse J C, Phillips F M. 2001. Terrestrial in situ cosmogenic nuclides: theory andapplication. Quaternary Science Reviews. 20:1475~1560.
[36]
Guo Z T, Wu H B, WeiJJ, Jiang W Y, Zhao X T. 2001. Uplift amplitude of thesouthern part of the Tibetan Plateau based on the carbon isotope of the paleosols.Quaternary Science in China, 21(5):392~398 (in Chinese with English abstract).
[37]
Lal D. 1991. Cosmic ray labeling of erosion surface: in situ nuclide productionrates and erosion models. Earth and Planetary Science Letter, 104:424~439.
[38]
Li J J, Feng Z D, Zhou S Z. 1996. Glaciers of Hengduan Mountains.Beijing: SciencePress of China (in Chinese).
[39]
Molnar P,England P, Martinod J. 1993. Mantle dynamics, uplift of the TibetanPlateau, and the Indian Monsoon. Reviews of Geophysics, 31 (4): 357~396.
[40]
Owen A L, Finkel C R, Caffee W M. 2002. A note on the extent of glaciationthroughout the Himalaya during the Global Last Glacial Maximum. Quaternary ScienceReviews, 21:147~157.
[41]
Schafer J M, Ivy-Ochs S, Weiler R, Leya I, Baur H, Denton G H,Schluchter C. 1999.Cosmogenic noble gas studies in the oldest landscape on earth: surface exposure ages ofthe Dry Valleys,Antarctic. Earth and Planetary Science Letter, 167:215~226.
[42]
Steig E J, Wolfe A P, Miller G H. 1998. Wisconsinan refugia and the glacialhistory of eastern Baffin Island, Arctic Canada: coupledevidence from cosmogenic isotopesand lake sediments. Geology,26(9) :835~838.
[43]
Wang J, Xu X R. 2000. A now technique for surface dating:cosmogenic isotopedating. Progress in Earth Science, 15 (2):237~240 (in Chinese with English abstract).
[44]
Wu X H, An Z S. 1996. 1oess-paleaosol sequences and the uplift of theQinghai-Tibetan Plateau. Science in China (Series D), 26(2):103~110 (in Chinese withEnglish abstract).
[45]
Zhang Q S, Zhou Y F, Lu X S, Xu Q L. 1990. Modern uplifting rates of theQinghai-Tibetan Plateau. Chinese Science Bullitin,7:529~531 (in Chinese).