波堆藏布谷地白玉冰期冰川与气候变化
|
摘要
青藏高原东南部地理位置独特,深受南亚季风的影响,发育了我国最大规模的海洋性冰川(温冰川),末次冰期盛冰期更留下了规模宏大的冰碛地貌,其中波密境内波堆藏布谷地的冰川地貌形态最为典型,侧碛、终碛的沉积特征非常显著,具有完整的冰碛序列。我们选取波堆藏布主谷内的冰川堆积地貌作为研究对象,运用多种测年技术(ESR、CRN、OSL和14C等)对具有代表性的冰碛序列和冰水阶地进行定年,重建青藏高原东南部地区第四纪冰川演化历史。利用GIS和RS等技术对现代冰川与气候因子之间的关系进行了深入研究,对第四纪冰川波动与气候变化之间的关系进行了初步探讨。
对波堆藏布谷地中的冰碛进行了系统的采集CRN测年样品,特别是白玉沟口附近的典型终碛和达卡桥西侧的冰碛。通过CRN测年技术所得到的冰碛形成的年龄,检测到了两次规模较大的冰川前进,一次是较老的古乡冰期,年龄为113±12.6 ka BP和97.4±10.8 ka BP,对应于深海氧同位素(MIS)6阶段;另一次是以白玉沟口数道高大冰碛垄为代表的冰期,从外到内(即从老到新)冰碛序列的年代为9-11ka BP,12-15.5 ka BP,分别对应于晚冰期的新仙女木事件(YD)和Heirichl事件(也可能是LGM持续到16 KaBP所致)。
对谷地中白玉沟内及其附近的冰水阶地中的显著的二层古土壤采集了6个~(14)C样品,获得下层古土壤的2个年龄分别为7190±120a BP,5230±120 a BP:上层古土壤的年龄分别为3755±125 a BP,2670±130 a BP,3450±70 a BP和3335±85 a BP。这些年龄数据揭示了藏东南地区在中全新世早期(7.2—5.5ka)和晚期(3.3-3.8 ka)发育了红色古土壤,代表了温暖湿润的气候,与河北平原河流湖泊所反映的气候相一致。
本文以1:10地形图和1987年、1999年陆地卫星图像及区域范围内9个气象站气象观测资料为基础数据,进行了详细的地形分析比较和数据空间结构的探索。基于GIS空间分析和遥感目视解译定量分析,我们选取了3条典型的冰川,分别计算其地形参数(包括长度、面积,高度及梯度等),重建白玉冰期时三条冰川的规模,详细剖析了朱西沟和白玉沟的冰川发育特点,并分析其形态差异、ELA差异的原因,认为地形因素是影响冰川形态的重要因素。
The last glacial maximum presents the dramatically drop in temperature throughout the world, which enlarges the areas of the ice sheets in two poles, extends the alpine glaciers and reduces the equilibrium line altitude of glaciers. But the dropping of the equilibrium line altitude in different areas is not consistent, and there are two reasons for it. On the one hand, the dropping extents in temperature are different;on the other, the equilibrium line altitude is the result of temperature and precipitation, and the influence of topography in the glacial developing area. After the last glacial maximum, the global temperature increases, resulting in the retreats of alpine glaciers, which shaped inimitable glacial landscapes. These various and majestic landforms are of natural landscape, and in different areas and positions, the glacial landforms are different. The study on the style, scale and area of moraines, which are formed by glacial erosion and accumulation in the last glacial maximum, is important for studying the quality, process and erosive accumulation of glaciers in the last glacial maximum. According to the relationship between variations of modern glaciers and climatic conditions, the climatic conditions in the last glacial maximum were reconstructed, in order to understand the effect of temperature, precipitation and topography on glaciers, and the influence of the south Asia monsoon on glaciers, especially on variations of the equilibrium line altitude, to infer the regional climatic change in the future, its contributions to the global climatic change, and the effect of global climatic change on regional climatic change.The southeast Nyanqingtanggula Mountains in the Tibetan plateau develop modern glaciers in large scale, and the last glacial maximum remains large-scale moraines, typically that in the valley of Boduizangbo in Bomi, and that in modern glaciers in the drainage area. Lateral and terminal moraines are very prominent sediments, and they can be used to completely reconstruct the scale, size, length and thickness of the typical glaciers in the valley during the last glacial maximum.The 11 samples of ESR were collected in the Baiyugou valley and in the
neighboring fluvioglacial terrace, the age of the sample BYG -1(ESR) at the first moraine is ll.l±1.6ka BP;the age of sample XM -1 at the hummocky moraine is 12.3±1.8ka BP. So the hummocky moraine represented by the sample suggested it may be formed in Boiling event or Allerod warming period in the lateglacial.The 614Csamples were collected in the 2-layer palaeo-soils in the fluvioglacial sediment of Baiyugou valley and neighboring Buduizangbu valley. The two sample ages in the lower layer were 7190±120a BP and 5230±120a BP;the 4 sample ages in the upper layer were 3755±125aBP, 2670±130aBP, 3450±70 a BPand 3335±85 a BP. The sample ages suggest southeast Tibetan Plateau had developed palaeo-soil during the early mid-Holocene(7.2 - 5.5ka) and during the late mid-Holocene, representing warm and moist climate, which is mutually consistent with the climate of the Hebei plain.Late Quaternary glacier fluctuations in the Boduizangbu valley were reconstructed using relative and absolute dating techniques. Our results indicate that younger moraine complexes were left by YD event (cal 11 ka BP) and Lateglacial (ca 13 cal. ka BP) ice advances. Older Late Quaternary glacier advances occurred during Marine Oxygen Isotope Stages (MIS) 6. No relics of Middle or Early Pleistocene glaciations could be found. During MIS6, glaciers advanced down to an altitude of at least 2600m a.s.l., corresponding to an ELA depression of approximately 1300 m. At about 2700m a.s.l., the YD glacier reached almost the thickness of the former MIS2 glacier and retreated some time before 16 cal. ka BP. The Lateglacial glacier advanced again several times to altitudes between 2700 and 2800m a.s.l.Based on the map of 1:100,000, the satellite images in 1987 and 1999, and the meteorologic data gathered from 34 weather stations in research areas, a detailed topography analysis and comparison was made to explore the data's spatial feature. According to the spatial analysis of GIS and the quantitative analysis of the remote sensing, three typical glaciers were chosen, in order to respectively calculate the terrain parameters, including length, area, height and gradient and so on. The characteristics of the vertical sections and cross-sections of Zhuxigou and Baiyugou were discussed in detail, and the feature was analyzed. At the end, the effect of the
bedrock and its topography on the glaciers was discussed.ELA was calculated through the weighted average and three different methods. The height of ELA of Baiyu ice age can be got, respectively 4004m asl, 3827m asl and 3882m asl, and each of them descend down 602 m, 380m and 372m, compared with that of modern times. By analyzing the statistics of temperature and precipitation in the nine weather stations around the research area, a distributed model of temperature and precipitation based on DEM was established, and the results show the gradient of summer average temperature in the southeast Tibet is lower than the vertical gradient of annual average temperature. According to the relationship between ELA and temperature (summer temperature) & precipitation (solid precipitation), the variation of climatic factors (temperature and precipitation) in the research area in the last glacial maximum were discussed.
对波堆藏布谷地中的冰碛进行了系统的采集CRN测年样品,特别是白玉沟口附近的典型终碛和达卡桥西侧的冰碛。通过CRN测年技术所得到的冰碛形成的年龄,检测到了两次规模较大的冰川前进,一次是较老的古乡冰期,年龄为113±12.6 ka BP和97.4±10.8 ka BP,对应于深海氧同位素(MIS)6阶段;另一次是以白玉沟口数道高大冰碛垄为代表的冰期,从外到内(即从老到新)冰碛序列的年代为9-11ka BP,12-15.5 ka BP,分别对应于晚冰期的新仙女木事件(YD)和Heirichl事件(也可能是LGM持续到16 KaBP所致)。
对谷地中白玉沟内及其附近的冰水阶地中的显著的二层古土壤采集了6个~(14)C样品,获得下层古土壤的2个年龄分别为7190±120a BP,5230±120 a BP:上层古土壤的年龄分别为3755±125 a BP,2670±130 a BP,3450±70 a BP和3335±85 a BP。这些年龄数据揭示了藏东南地区在中全新世早期(7.2—5.5ka)和晚期(3.3-3.8 ka)发育了红色古土壤,代表了温暖湿润的气候,与河北平原河流湖泊所反映的气候相一致。
本文以1:10地形图和1987年、1999年陆地卫星图像及区域范围内9个气象站气象观测资料为基础数据,进行了详细的地形分析比较和数据空间结构的探索。基于GIS空间分析和遥感目视解译定量分析,我们选取了3条典型的冰川,分别计算其地形参数(包括长度、面积,高度及梯度等),重建白玉冰期时三条冰川的规模,详细剖析了朱西沟和白玉沟的冰川发育特点,并分析其形态差异、ELA差异的原因,认为地形因素是影响冰川形态的重要因素。
The last glacial maximum presents the dramatically drop in temperature throughout the world, which enlarges the areas of the ice sheets in two poles, extends the alpine glaciers and reduces the equilibrium line altitude of glaciers. But the dropping of the equilibrium line altitude in different areas is not consistent, and there are two reasons for it. On the one hand, the dropping extents in temperature are different;on the other, the equilibrium line altitude is the result of temperature and precipitation, and the influence of topography in the glacial developing area. After the last glacial maximum, the global temperature increases, resulting in the retreats of alpine glaciers, which shaped inimitable glacial landscapes. These various and majestic landforms are of natural landscape, and in different areas and positions, the glacial landforms are different. The study on the style, scale and area of moraines, which are formed by glacial erosion and accumulation in the last glacial maximum, is important for studying the quality, process and erosive accumulation of glaciers in the last glacial maximum. According to the relationship between variations of modern glaciers and climatic conditions, the climatic conditions in the last glacial maximum were reconstructed, in order to understand the effect of temperature, precipitation and topography on glaciers, and the influence of the south Asia monsoon on glaciers, especially on variations of the equilibrium line altitude, to infer the regional climatic change in the future, its contributions to the global climatic change, and the effect of global climatic change on regional climatic change.The southeast Nyanqingtanggula Mountains in the Tibetan plateau develop modern glaciers in large scale, and the last glacial maximum remains large-scale moraines, typically that in the valley of Boduizangbo in Bomi, and that in modern glaciers in the drainage area. Lateral and terminal moraines are very prominent sediments, and they can be used to completely reconstruct the scale, size, length and thickness of the typical glaciers in the valley during the last glacial maximum.The 11 samples of ESR were collected in the Baiyugou valley and in the
neighboring fluvioglacial terrace, the age of the sample BYG -1(ESR) at the first moraine is ll.l±1.6ka BP;the age of sample XM -1 at the hummocky moraine is 12.3±1.8ka BP. So the hummocky moraine represented by the sample suggested it may be formed in Boiling event or Allerod warming period in the lateglacial.The 614Csamples were collected in the 2-layer palaeo-soils in the fluvioglacial sediment of Baiyugou valley and neighboring Buduizangbu valley. The two sample ages in the lower layer were 7190±120a BP and 5230±120a BP;the 4 sample ages in the upper layer were 3755±125aBP, 2670±130aBP, 3450±70 a BPand 3335±85 a BP. The sample ages suggest southeast Tibetan Plateau had developed palaeo-soil during the early mid-Holocene(7.2 - 5.5ka) and during the late mid-Holocene, representing warm and moist climate, which is mutually consistent with the climate of the Hebei plain.Late Quaternary glacier fluctuations in the Boduizangbu valley were reconstructed using relative and absolute dating techniques. Our results indicate that younger moraine complexes were left by YD event (cal 11 ka BP) and Lateglacial (ca 13 cal. ka BP) ice advances. Older Late Quaternary glacier advances occurred during Marine Oxygen Isotope Stages (MIS) 6. No relics of Middle or Early Pleistocene glaciations could be found. During MIS6, glaciers advanced down to an altitude of at least 2600m a.s.l., corresponding to an ELA depression of approximately 1300 m. At about 2700m a.s.l., the YD glacier reached almost the thickness of the former MIS2 glacier and retreated some time before 16 cal. ka BP. The Lateglacial glacier advanced again several times to altitudes between 2700 and 2800m a.s.l.Based on the map of 1:100,000, the satellite images in 1987 and 1999, and the meteorologic data gathered from 34 weather stations in research areas, a detailed topography analysis and comparison was made to explore the data's spatial feature. According to the spatial analysis of GIS and the quantitative analysis of the remote sensing, three typical glaciers were chosen, in order to respectively calculate the terrain parameters, including length, area, height and gradient and so on. The characteristics of the vertical sections and cross-sections of Zhuxigou and Baiyugou were discussed in detail, and the feature was analyzed. At the end, the effect of the
bedrock and its topography on the glaciers was discussed.ELA was calculated through the weighted average and three different methods. The height of ELA of Baiyu ice age can be got, respectively 4004m asl, 3827m asl and 3882m asl, and each of them descend down 602 m, 380m and 372m, compared with that of modern times. By analyzing the statistics of temperature and precipitation in the nine weather stations around the research area, a distributed model of temperature and precipitation based on DEM was established, and the results show the gradient of summer average temperature in the southeast Tibet is lower than the vertical gradient of annual average temperature. According to the relationship between ELA and temperature (summer temperature) & precipitation (solid precipitation), the variation of climatic factors (temperature and precipitation) in the research area in the last glacial maximum were discussed.
引文
Anderson J.G. Topographical and archaeological studies in the Far East. Oslasialiska Sam Lingarna Bull, 1939, 11:110.
Augustin L.et al., Eight glacial cycles from an Antarctic ice core. Nature 2004;429 (6992):623-8.
Bamard, P. L., L. A. Owen, et al. Quaternary fans and terraces in the Khumbu Himal south of Mount Everest: their characteristics, age and formation. Journal of the Geological Society, 2006, 163: 383-399.
Barnard, P.L., Owen, L.A., Finkel, R.C. Style and timing of glacial and paraglacial sedimentation in a monsoonal influenced high Himalayan environment, the upper Bhagirathi Valley, Garhwal Himalaya. Sedimentary Geology, 2004a, 165:199-221.
Barnard, P.L., Owen, L.A., Sharma, M.C., Finkel, R.C. Late Quaternary landscape evolution of a monsoon-influenced high Himalayan valley, Gori Ganga, Nanda Devi, NE Garhwal. Geomorphology, 2004b, 61: 91-110.
Barrows, T. T., Stone, J. O., Fifield, L. K., et al. Late Pleistocence glaciation of the Kosciuszko Massif, Snowy Mountains, Australia. Quaternary Research, 2001, 55:179-189.
Ben W.M. Richards et al. Timing of Late Quaternary glaciations in the Himalayas of northern Pakistan. Journal of Quaternary Science, 2000, 15 (3):283-297.
Benn, D.I., Lehmkuhi, F. Mass balance and equilibrium-line altitudes of glaciers in high mountain environments. Quaternary International, 2000, 65/66:15-29.
Benn, D.I., Owen, L.A. Himalayan glacial sedimentary environments: a framework for reconstructing and dating former glacial extents in high mountain regions. Quaternary International, 2002, 97-98: 3-26.
Benn, D.I., Owen, L.A. The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation: review and speculative discussion. Journal of the Geological Society, 1998,155:353-363.
Benn, D.I., Owen, L.A., Osmaston, H.A., Seltzer, G.O., Porter, S.C., Mark, B. Reconstruction of equilibrium-line altitudes for tropical and sub-tropical glaciers. Quaternary International, 2005,138:8-21.
Berger, A., Loutre, M.F. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews, 1991,10:297-317.
Bierman, P R, Marsella, K A, Patterson, C, et al. M id-Pleistocene cosmogenic minimum-age limits for pre-W isconsinan glacial surfaces in southwestern Minnesota and southern Baffin Island: a multiple nuclide approach. Geomorphology, 1999, 27: 25-39.
Bierman, P R. Using in situ produced cosmogenic isotopes to estimate rates of landscape evoluation: A review from the geomorphic perspective. Journal of Geophysical Research, 1994, 99 (B7):13885-13896.
Bohner, J. and F. Lehmkuhl. Environmental change modelling for Central and High Asia: Pleistocene, present and future scenarios. Boreas, 2005, 34(2): 220-231.
Bose, M., Hirakawa, K., Matsuoka, N., Sawagaki, T. Glaciation and periglaciation in Asian high Mountains. Zeitsehriftfur Geomorphologie, 2003 (Eds.), 130, 276pp.
Briner, J P, Swanson, T W. Late Pleistocene cosmogenic 36Cl glacial chronology of the Southwestern Ahklun Mountains. Alaska. Quaternary Research, 2001, 56:148-154.
Briner, J P, Swanson, T W. U sing inherited cosmogenic 36Cl to const rain glacial erosion rates of the Cordilleran ice sheet. Geology, 1998, 26:3-6.
Brown E T, Trull T W, Jean-Baptiste P, ct al. Determination of cosmogenic production rates of 10 Be, 3He and 3H in water. Nucl Instr Methods Phys Res, 2000, 172B: 873-883.
Bush, A. B. G. Modelling of late Quaternary climate over Asia: a synthesis. Boreas, 2004, 33(2): 155-163.
Bush, A.B.G. A comparison of simulated monsoon circulations and snow accumulation in Asia during the mid-Holocene and at the Last Glacial Maximum. Global and Planetary Change, 2002, 32:331-347.
Bush, A.B.G. A comparison of simulated monsoon circulations and snow accumulation in Asia during the mid-Holocene and at the Last Glacial Maximum. Global and Planetary Change, 2002, 32:331-347.
Bush, A.B.G. A positive climatic feedback mechanism for Himalayan glaciation. Quaternary International, 2000, 65/66: 3-13.
Ceding T E, Craig H. Cosmogenic 3He production rates from 39°N to 46°N latitude, western USA and France. Geochim Cosmochim Acta, 1994, 58 : 249-255.
Clark,D H,Bierman, P, Gillespie,A R. 10Be and 26Al product ion rates and a revised glacial chronology for the Sierra Nevada. Radiocarbon, 1996, 38 (1): 152.
Dep,L , Elmore, D,Lipschutz, M , et al. Depth dependence of cosmogenic neutron capture produced 36Cl in a terrestrial rock. Nuclear Instruments and Methods in Physics Research B, 1994b, 92:301-307.
Derbyshire, E. Glacier regime and glacial sediment facies: a hypothetical framework for the Qinghai-Xizang Plateau. In: Proceedings of the Symposium on Qinghai-Xizang (Tibet) Plateau, Beijing China. Vol. 2—Geological and Ecological Studies of Qinghal-Xizangf Plateau. Science Press, Beijing. 1981: 1649-1656.
Derbyshire, E. Quaternary glacial sediments, glaciation style, climate and uplift in the Karakoram and northwest Himalaya: Review and speculations. Palaeogeography Palaeoclimatology Palaeoecology ,1996, 120(1-2): 147-157.
Derbyshire, E., Shi, Y., Li, J., Zheng, B., Li, S., Wang, J. Quaternary glaciation of Tibet: the geological evidence. Quaternary Science Reviews. 1991, 10:485-510.
Desilets,D, Zreda, M. On scaling cosmogenic nuclide production rates for altitude and latitude using cosmic-ray measurements. Earth and Planetary Science Letters, 2001, 193: 213-225.
Dey, B., Bhanu Khumar, O.S.R.U. An apparent relationship between Eurasian spring snow cover and the advance period of the Indian summer monsoon. Journal of Applied Meteorology, 1982, 21:1923-1929.
Dey, B., Kathuria, S.N., Bhanu Khumar, O.S.R.U. Himalayan snow cover and withdrawal of the Indian summer monsoon. Journal of Climatology and Applied Meteorology, 1985, 24: 865-868.
Dickson, R.R. Eurasian snow cover versus Indian monsoon rainfall—an extension of the Hahn-Shukla results. Journal of Climatology and Applied Meteorology, 1984, 23: 171-173.
Dunai, T J. Sealing factors for product ion rates of in situ produced eosmogenie nuclides: a critical reevaluation. Earth and Planetary Science Letters, 2000, 176: 157-169.
Dyke AS, Andrews JT, Clark PU, England JH, Miller GH, Shaw J, Veillette JJ. The Laurentide and Innuitian ice sheets during the Last Glacial Maximum. Quaternary Science Reviews 2002;21 (1-3):9-31.
Easterbrook, D.J., Pierce, K., Gosse, J.C., Gillespie, A., Evenson, E.B., Hamblin, K. Quaternary geology of the western United States. In: Easterbrook, DJ. (Ed.), Quaternary Geology of the United States. Geological Society of America, Denver, 2003:19-80.
Fabel,D, Harbor, J. The use of in situ produced cosmogenic radionuclides in glaciology and glacial geomorphology.Annals of Glaciology, 1999,28: 103-110.
Fabel,D, St roeven,A P,Harbo r, J. Landscape preservat ion under Fennoscandian ice sheets determined from in situ produced 10Be and 26A1. Earth and Planetary Science Letters, 2002,201:397-406.
Finkel, R.C., Owen, L.A., Barnard, P.L., Caffee, M.W. Beryllium-10 dating of Mount Everest moraines indicates a strong monsoonal influence and glacial synchroneity throughout the Himalaya. Geology, 2003,31:561-564.
Fushimi H. Glaciations in the Khumbu Himal (2). Seppyo, 1978,40: 71-77.
Gasse F, Vancampo E. Abrupt Postglacial Climate Events in West Asia and North-Africa Monsoon Domains. Earth and Planetary Science Letters 1994;126 (4):435-56.
Gibbons, A.B., Megeath, J.D., Pierce, K.L. Probability of moraine survival in a succession of glacial advances. Geology, 1984,12, 327-330.
Gillesp ie A, Molnar P. Asynchronous maximum advances of Mountain and continental glacials. Review of Geophysics, 1995, 33(3): 311-364.
Gillespie,A R, Bierman, P R. Precision of terrestrial exposure ages and erosion rates estimated from analysis of cosmogenic isotopes produced in situ. Journal of Geophysical Research, 1995, 100 (B12):24637-24649.
Gosse, J C, Klein, J , Evenson, et al. Beryllium - 10 dating of the duration and retreat of the Last Pinedale Glacial sequence. Science, 1995,268:1329-1333.
Gosse, J C, Phillip s, F M. Terrestrial cosmogenic nuclides: theory and applications. Quaternary Sciences Review, 2001,20:1475-1560.
Gosse, J.C., Evenson, E.B., Klein, J., Lawn, B., Middleton, R. Precise cosmogenic 10Be measurements in western North America: support for a global younger Dryas cooling event. Geology, 1995a, 23: 877-880.
Gosse, J.C., Klein, J., Evenson, E.B., Lawn, B., Middleton, R. Beryllium-10 dating of the duration and retreat of the Last Pinedale glacial sequence. Science, 1995b, 268:1329-1333.
Gosse, J.C., Phillips, F.M. Terrestrial in situ cosmogenic nuclides: theory and application. Quaternary Science Reviews, 2001,20:1475-1560.
Granger DE, Muzikar PF. Dating sediment burial with in situ-produced cosmogenic nuclides: theory, techniques, and limitations. Earth and Planetary Science Letters 2001;188(1-2):269-81.
Hahn, D.G, Shukla, J. An apparent relationship between Eurasian snow cover and Indian monsoon rainfall. Journal of Atmospheric Science, 1976, 33: 2461-2462.
Hallet,B, Putkonen, J. Surface dating of dynamic landforms: young boulders and aging moraines. Science, 1994,265:937- 940.
Heisinger,B, Nolte, E. Cosmogenic in situ product ion of radionuclides: exposure ages and erosion rates. Nuclear Instruments and Methods in Physics Research B, 2000,172:790-795.
Kaulback R. A journey in t he Salween and Tsangpo Basins ,Sout h Eastern Tibet [J ] . Geogr . Jour., 1938,91 (2) : 96-98.
Kodrau, O.D. Climatic Atlas of Asia. World Meteorological Organisation (UNESCO), Geneva, 1981.
Kohl, C.P., Nishiizumi, K. Chemical isolation of quartz for measurement of in-situ produced cosmogenic nuclides. Geochimica et Cosmochimica Acta, 1992,56:3583-3587.
Kuhle, M. Geomorphological findings on the built-up of Pleistocene glaciation in Southern Tibet and on the problem of inland ice. GeoJournal, 1988,17: 457-512.
Kuhle, M. Glacial isostatic uplift of Tibet as a consequence of a former ice sheet. GeoJournal, 1995,37:431-449.
Kuhle, M. Glaciation Research in the Himalayas: a new ice age theory. Universitas, 1985, 27:281-294.
Kuhle, M. Observations supporting the Pleistocene inland glaciation of High Asia. GeoJournal, 1991,25:131-231.
Kukla, G and V. Cilek. Plio-pleistocene megacycles: Record of climate and tectonics. Palaeogeography Palaeoclimatology Palaeoecology, 1996,120(1-2): 171-194.
Kurz M D. In situ production of terrestrial cosmogenic helium and some applications to geochronology. Geochim Cosmochim Acta, 1986,50 :2855-2862.
Lal D. Cosmogenic nuclide production rate systematics in terrestrial materials: present knowledge, needs and future actions for improvement. Nucl Instr Methods Phys Res, 2000, 172B: 772-781.
Lal, D. Cosmic ray labeling of erosion surfaces: in situ nuclide product ion rates and erosion models. Earth and Planetary Science Letters, 1991,104:424-439.
Lal, D., Peters, B. Cosmic ray produced radioactivity on the Earth. In: Flugge, S. (Ed.), Handbueh der Physik, 1967,46( 12): 551-612.
Lehmkuhl, F. and F. Haselein. Quaternary paleoenvironmental change on the Tibetan Plateau and adjacent areas (Western China and Western Mongolia). Quaternary International, 2000, 65-66:121-145.
Lehmkuhl, F. Late Pleistocene, Late-Glacial and Holocene glacier advances on the Tibetan Plateau. Quaternary International, 1997,38/39:77-83.
Lehmkuhl, F., Klinge, M., Lang, A. Late Quaternary glacier advances, lake level fluctuations and aeolian sedimentation in Southern Tibet. Zeitschrift fu(?)r Geomorphologie, 2002, 126:183-218.
Lehmkuhl, F., M. Klinge, et al. (2000). Late Quaternary aeolian sedimentation in central and south-eastern Tibet. Quaternary International, 2000,68:117-132.
Libby W F, Anderson E C, Arnold J R. Age determination by radiocarbon content: world-wide assay of natural radiocarbon. Science, 1949,109:227-228.
Licciardi JM, Clark PU, Brook EJ, Pierce KL, Kurz MD, Elmore D, Sharma P. Cosmogenic He-3 and Be-10 chronologies of the late Pinedale northern Yellowstone ice cap, Montana, USA. Geology 2001;29 (12):1095-8.
Ma Qiuhua. Geomorphology and Quaternary Glaciations in Naimonanyi Peak Region. Proceeding of Sino - Japanese JointScientiflc Symposium: Tibetan Plateau. 1989,2:41-54.
Masarik J., Reedy P C. Terrestrial cosmogenic2nuclide production systematics calculated from numerical simulations. Earth Planet Sci Lett, 1995,136: 381-395.
McCabe, A. M. and P. U. Clark. Ice-sheet variability around the north Atlantic Ocean during the last deglaciation. Nature, 1998,392(6674): 373-377.
Molnar, P. The rise of the Tibetan plateau: From mantle dynamics to the Indian monsoon. Astronomy & Geophysics, 1997, 38(3): 10-15.
Molnar, P., England, P. Late Cenozoic uplift of mountain ranges and global climatic change: chicken or egg? Nature, 1990,346: 29-34.
Molnar, P., P. England, et al. Mantle Dynamics, Uplift of the Tibetan Plateau, and the Indian Monsoon. Reviews of Geophysics, 1993, 31(4): 357-396.
Montgomery D R, HalletB,Liu Yup ing et al. Evidence for Holocene megafloods down the Tsangpo River gorge, Southeastern Tibet.Quaternary Research, 2004, 62 (2): 201-207.
Moore, J. M. and A. E. Moore. The roles of primary kimberlitic and secondary Dwyka glacial sources in the development of alluvial and marine diamond deposits in Southern Africa. Journal of African Earth Sciences, 2004, 38(2): 115-134.
Nishiizumi K. Cosmogenic production of 7Be and 10 Be in water targets. J Geophys Res, 1996, 101 (B10): 22225-22232.
Nishiizumi, K, Kohl, C P, Arnold, J R, et al. Cosmicray produced ~10Be and ~26A1 in Antarctic rocks: exposure and erosion history. Earth and Planetary Science Letters, 1991,104:440- 454.
Nishiizumi, K, Winterer, E L, Kohl, C P, et al. Cosmic ray product ion rates of ~10Be and ~26A 1 in quartz from glacially polished rocks. Journal of Geophysical Research, 1989,94 (B12):17907-17915.
O'Connor J E, Baker V R. Magnitudes and implications of peak discharges from Glacial Lake Missoula. Geological Society of America Bulletin, 1992,104:179-267.
Overpeck, J. T., B. L. Otto-Bliesner, et al. Paleoclimatic evidence for future ice-sheet instability and rapid sea-level rise. Science, 2006,311(5768): 1747-1750.
Owen L A, Derbyshire E, Fort M. The Quaternary glacial history of the Himalaya. Quaternary Proceedings, 1998,6: 91-120.
Owen L A, Finkel R C, Caffee MW.A note on the extent of glaciation throughout the Himalaya during the global Last Glacial Maximum. Quaternary Science Reviews, 2002, 21 (1-3): 147-157.
Owen L A, Wishart M, Bailey R M, et al. Style and timing of glaciation in Lahul Himalaya, North India: a framework for reconstructing late Quaternary paleoclimatic change in the Western Himalayas. Journal of Quaternary Science, 1997,12: 83-110.
Owen L A., Kamp U, Joel Q. Spencer and Klaus Haserodt. Timing and style of Late Quaternary glaciation in the eastern Hindu Kush, Chitral, northern Pakistan: a review and revision of the glacial chronology based on new optically stimulated luminescence dating.
Quaternary International, 2002,97/98:41-55.
Owen, L A, F inkel, R C, Caffee,M W, et al. Timing of multiple late Quaternary glaciations in the Hunza V alley, Karakoram Mountains, northern Pakistan: defined by cosmogenic radionuclide dating of moraines. GSA Bulletin, 2002,114 (5):593- 604.
Owen, L. A. and D. I. Benn. Equilibrium-line altitudes of the Last Glacial Maximum for the Himalaya and Tibet: an assessment and evaluation of results. Quaternary International, 2005,138: 55-78.
Owen, L. A., H. Z. Ma, et al. The timing and style of Late Quaternary glaciation in the La Ji Mountains, NE Tibet: evidence for restricted glaciation during the latter part of the Last Glacial. Zeitschrift Fur Geomorphologie, 2003,47:263-276.
Owen, L. A., M. W. Caffee, et al. Terrestrial cosmogenic nuclide surface exposure dating of the oldest glacial successions in the Himalayan orogen: Ladakh Range, northern India. Geological Society of America Bulletin, 2006,118(3-4): 383-392.
Owen, L. A., R. C. Finkel, et al. Climatic and topographic controls on the style and timing of Late Quaternary glaciation throughout Tibet and the Himalaya defined by Be-10 cosmogenic radionuclide surface exposure dating. Quaternary Science Reviews, 2005, 24(12-13): 1391-1411.
Owen, L.A., Benn, D.I. Equilibrium-line altitudes of the Last Glacial Maximum for the Himalaya and Tibet: an assessment and evaluation of methods and results. Quaternary International, 2005,138:55-78.
Owen, L.A., Finkel, R.C., Caffee, M.W. A note on the extent of glaciation in the Himalaya during the global Last Glacial Maximum. Quaternary Science Reviews, 2002b, 21:147-157.
Owen, L.A., Finkel, R.C., Caffee, M.W., Gualtieri, L. Timing of multiple glaciations during the Late Quaternary in the Hunza Valley, Karakoram Mountains, Northern Pakistan: defined by cosmogenic radionuclide dating of moraines. Geological Society of America Bulletin, 2002a. 114,593-604.
Owen, L.A., Finkel, R.C., Ma, H., Spencer, J.Q., Derbyshire, E., Barnard, P.L., Caffee, M.W. Timing and style of Late Quaternary glaciations in NE Tibet. Geological Society of America Bulletin, 2003c, 115:1356-1364.
Owen, L.A., Gualtieri, L., Finkel, R.C., Caffee, M.W., Benn, D.I., Sharma, M.C. Cosmogenic radionuclide dating of glacial landforms in the Lahul Himalaya, Northern India: defining the timing of Late Quaternary glaciation. Journal of Quaternary Science, 2001, 16, 555-563.
Owen, L.A., Kamp, U., Spencer, J.Q., Haserodt, K. Timing and style of Late Quaternary glaciation in the eastern Hindu Kush, Chitral, northern Pakistan: a review and revision of the glacial chronology based on new optically stimulated luminescence dating. Quaternary International, 2002c. 97/98:41-56.
Owen, L.A., Lehmkuhl, F. (Eds.) Late Quaternary glaciation and palaeoclimate of the Tibetan Plateau and bordering mountains. Quaternary International, 2000, 65/66:212.
Owen, L.A., Ma, H., Derbyshire, E., Spencer, J.Q., Barnard, P.L., Zeng Yong Nian, Finkel, R.C., Caffee, M.W. The timing and style of Late Quaternary glaciation in the La Ji Mountains, NE Tibet: evidence for restricted glaciation during the latter part of the Last Glacial. Zeitschrift fur Geomorphologie, 2003b, 130: 263-276.
Owen, L.A., Spencer, J.Q., Ma, H., Barnard, P.L., Derbyshire, E., Finkel, R.C., Caffee, M.W., Zeng Yong, N. Timing of Late Quaternary glaciation along the southwestern slopes of the Qilian Shan. Boreas, 2003a, 32:281-291.
Owen, L.A., Teller, J.T., Rutter, N.W. Glaciation and reorganization of Asia's network of drainage. Global and Planetary Change, 2002d, 30:289-374.
Owen, L.A., Zhou, S. (Eds.) Glaciation in Monsoon Asia, Quaternary International, 2002, 97/98:179.
Patrick M.Colgan, Jeffrey S.Munroe,Zhou Shangzhe. Cosmogenic radionuclide evidence for the limited extent of last glacial maximum glaciers in the Tanggula Shan of the central Tibetan Plateau. Quaternary Research, 2006,65(2): 336-339
Phillips, F M, Zreda, M G, Benson, L V, et al. Chronology for Fluctuation in Late Pleistocence Sierra Nevada Glaciers and Lakes. Science, 1996,274: 749- 751.
Phillips, F M, Zreda, M G, Smith, S S, et al. Cosmogenic Chlorine- 36 chronology for glacial deposits at Bloody Canyon, Eastern Sierra Nevada. Science, 1990,248: 1529-1532.
Phillips, W.M., Sloan, V.F., Shroder, J.F., Sharma, P., Clarke, M.L., Rendell, H.M. Asynchronous glaciation at Nanga Parbat, northwestern Himalaya Mountains, Pakistan. Geology, 2000, 28:431-434.
Pollard, D. and S. L. Thompson. Climate and ice-sheet mass balance at the last glacial maximum from the genesis version 2 global climate model. Quaternary Science Reviews, 1997, 16(8): 841-863.
Poreda R J, Cerlingt E. Cosmogenic neon in recent lavas from the western United States. Geophys Res Lett, 1992, 19: 1863-1866.
Prell, W.L., Kutzbach, J.F. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution. Nature, 1992, 360:647-652.
Pu, J.C., Su, Z., Yao, T.D., Xie, Z. C. Mass balance on Xiao Dorigkemadi Glacier and Hailuoguo Glacier. Journal of Glaciology and Geocryology, 1998,12:408-412.
Putkonen, J., Swanson, T. Accuracy of cosmogenic ages for moraines. Quaternary Research, 2003, 59:255-261.
R. V. Joshi, S. N. Rajaguru Quaternary Glaciation and Palaeolithic Sites in the Liddar Valley (Jammu-Kashmir) World Archaeology, 1974,5 (3) :369-379
Richards BWM, Benn DI, Owen LA, Rhodes EJ, Spencer JQ. Timing of late Quaternary laciations south of Mount Everest in the Khumbu Himal, Nepal. Geological Society of America Bulletin 2000;l 12 (10):1621-32.
Richards, B.W., Owen, L.A., Rhodes, E.J. Timing of Late Quaternary glaciations in the Himalayas of northern Pakistan. Journal of Quaternary Science, 2000b, 15:283-297.
Richards, B.W.M., Benn, D.I., Owen, L.A., Rhodes, E.J., Spencer,J.Q. Timing of Late Quaternary glaciations south of Mount Everest in the Khumbu Himal, Nepal. Geological Society of American Bulletin, 2000a, 112:1621-1632.
Rinterknecht VR, Clark PU, Raisbeck GM, Yiou F, Bitinas A, Brook EJ, Marks L, Zelcs V, Lunkka JP, Pavlovskaya IE, Piotrowski JA, Raukas A. The last deglaciation of the southeastern sector of the Scandinavian Ice Sheet. Science 2006;311 (5766): 1449-52.
Licciardi JM, Clark PU, Brook EJ, Elmore D, Sharma P. Variable responses of western US glaciers during the last deglaciation. Geology 2004;32 (1):81-4.
Robert C. Finkel Lewis A. Owen Patrick L. Barnard et al .Beryllium-10 dating of Mount Everest moraines indicates a strong monsoon influence and glacial synchroneity throughout the Himalaya. Geology;2003,31(6):561-564.
Roland Zech. Late Quaternary glacial and climate history of the Pamir Mountains derived from cosmogenic 10Be exposure ages. Quaternary Research, 2005,64:212-220.
Ruddiman, W. F. and J. E. Kutzbach. Plateau Uplift and Climatic-Change. Scientific American, 1991,264(3): 66-&.
Ruddiman, W.F., Kutzbach, J.E. Forcing of Late Cenozoic Northern Hemisphere climate by plateau uplift in southern Asia and the America west. Journal of Geophysical Research, 1989,94:409.
S.Tsukamoto, K.Asahi et al. Time of past glaciations in Kanchenjunga Himal, Nepal by optically stimulated luminescece dating of tills. Quaternary International, 2002,97/98:57-67.
Schafer, J.M., Tschudi, S., Zhao, Z., Wu, X., Ivy-Ochs, S., Wider, R., Baur, H., Kubik, P.W., Schluchter. The limited influence of glaciations in Tibet on global climate over the past 170000 yr. Earth and Planetary Science Letters, 2001, 60/69:1-11.
Seltzer GO. Climatic Interpretation of Alpine Snowline Variations on Millennial Time Scales. Quaternary Research 1994;41 (2): 154-9.
Sharma, M.C., Owen, L.A. Quaternary glacial history of the Garhwal Himalaya, India. Quaternary Science Reviews, 1996,15:335-365.
Shi, Y. Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia. Quaternary International, 2002,97/98:79-91.
Shi, Y., Ge, Y, Xiaodong, L., Bingyuan, L., Tandong, Y. Reconstruction of the 30-40 ka BP enhanced Indian monsoon climate based on geological records from the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 169:69-83.
Shiraiwa T, Watanabe T. Late Quaternary glacial fluctuation in the Langtang Valley, Nepal Himalaya, teconstructed by relative dating methods. Arctic and Alpine Research, 1991,23: 404-416.
Silvio Tschudi, Jorg M. Schafer, Zhizong Zhao et al. Glacial advances in Tibet during the Younger Dryas? Evidence from cosmogenic ~10Be, ~26A1, and ~21Ne. Journal of Asian Earth Sciences, 2003, 22: 301-306.
Sirocko, F., Sarnthein, M., Lange, H., Mayayewski, P.A. Atmospheric summer circulation and coastal upwelling in the Arabian Sea during the Holocene and the Last Glaciation. Quaternary Research, 1991,36:72-93.
Soman, M.K., Slingo, J. Sensitivity of the Asian summer monsoon to aspects of sea-surface-temperature anomalies in the tropical Pacific Ocean. Quarterly Journal of the Royal Meteorological Society, 1997,123:309-336.
Steig, E J ,Wolfe,A P,Miller, G H. Wisconsinan refugia and the glacial history of eastern Baffin Island, Arctic Canadaxoupled evidence from cosmogenic isotopes and lake sediments. Geology, 1998, 26: 835- 838.
Stone, J O. Air pressure and cosmogenic isotope production. Journal of Geophysical Research, 2000, 105 (B10): 23753- 23759.
Stroeven,A P, Fabel,D, Habttestrand, C, et al. A relict landscape in the centre of Fennoscandian glaciation: cosmogenic radionuclide evidence of tors preserved through multip le glacial cycles. Geomorphology, 2002,44:145-154.
Su, Z., Shi, Y. Response of monsoonal temperate glaciers to global warming since the Little Ice Age. Quaternary International, 2002, 97/98:123-131.
Svendsen, J. I., Alexanderson H., et al. Late quaternary ice sheet history of northern Eurasia. Quaternary Science Reviews, 2004,23(11-13): 1229-1271.
Taylor,P.J, Mitchell,W.A., Late Quaternary glacial history of the Zanskar Range, North-west Indian Himalaya. Quaternary International, 2000,65/66:81-100.
Thomp son L G, Yao T, Davis M K et al. Trop ical climate instability: The last glacial cycles from a Qinghai-Tibetan ice core. Science, 1997,276:1821-1825
Thompson, L.G, Thompson, E.M., Davies, M.E., Bolzn, J.F., Dai, J., Gunderstrup, N., Wu, X., Klein, L., Xie, Z. Holocene-Late Pleistocene climatic ice core records from the Qinghai-Tibet Plateau. Science, 1989,246:474-477.
Trinkler.E The ice-age on the Tibetan plateau and in the adjacent regions. The Geogr.J. , 1930, 75(3):225-232.
Tsukamoto, S., Asahi, K., Watanabe, T., Rink, W.J. Timing of past glaciations in Kanchenjunga Himal, Nepal by optically stimulated luminescence dating of tills. Quaternary International, 2002, 97/98: 57-67.
Tsukamoto, S., Asahi, K., Watanabe, T., Rink, W.J. Timing of past glaciations in Kanchenjunga Himal, Nepal by optically stimulated luminescence dating of tills. Quaternary International, 2002, 97/98:57-67.
W. R. Rickmers The Pamir Glaciers Geographical Journal, 1965,131 (2):217-220
W.M. Richards, Douglas I. Benn et al. Timing of late Quaternary glaciations south of Mount Everest in the Khumbu Himal, Nepal. Ben GSA Bulletin. 2000, 112(10): 1621-1632.
Wake, C.P., Mayewski, P.A., Dahe, Q., Qinzhao, Y., Sichang, K., Whitlow, S., Meeker, L.D. Changes in atmospheric circulation over the south-eastern Tibetan Plateau over the last two centuries from a Himalayan ice core. PAGES News, 2001, 9:14-16.
Wang, Y. J., H. Cheng, et al. A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China. Science, 2001, 294(5550): 2345-2348.
William M. Phillips, Valerie F. Sloan et al. Asynchronous glaciation at Nanga Parbat, northwestern Himalaya Mountains, Pakistan. Geology;2000, 28(5): 431-434.
Winograd, I.J., Landwehr, J.M., Ludwig, K.R., Coplen, T.B., Riggs, A.C. Duration and structure of the past four interglacials. Quaternary Research, 1997, 48:141-154.
Winograd, I.J., Landwehr, J.M., Ludwig, K.R., Coplen, T.B., Riggs, A.C. Duration and structure of the past four interglacials. Quaternary Research, 1997,48:141-154.
Wissmann.h.von. The Pleistocene glaciation in China. Bull. Geol. Sol. China, 1937, 5:3-6.
Wu Yongqiu, Cui Zhijiu, Liu Gengnian et al. Quaternary geomorphological actions evolution of the Kunlun Pass area and up lift of the Qinghai2Xizang (Tibet) Plateau. Geomorphology, 2001, 36(3-4): 203-216.
Yi Chaolu, J iao Keqin, Liu Kexin et al. ESR Dating of the sediments of the Last Glaciation at the source area of the Brümqi River, Tian Shan Mountains, China. Quaternary International, 2002, 97/98: 141-146.
Yi Chaolu, Liu Kexin, Cui Zhijiu et al. AMS radiocarbon dating of Late Quaternary glacial landforms, source of the Brümqi River, Tien Shan—A pilot study of 14C dating on inorganic carbon. Quaternary International, 2004, 121 (1) : 99-107.
Yi, C., Li, X., Qu, J. Quaternary glaciation of Puruogangri-the largest modern ice field in Tibet. Quaternary International, 2002, 97/98:111-123.
Yu, Y. T., Yang T. B., et al. (). Millermial-scale Holocene climate variability in the NW China drylands and links to the tropical Pacific and the North Atlantic. Palaeogeography Palaeoclimatology Palaeoecology, 2006, 233(1-2): 149-162.
Zech R., Abramowski U., et al. Late Quaternary glacial and climate history of the Pamir Mountains derived from cosmogenic Be-10 exposure ages. Quaternary Research, 2005, 64(2): 212-220.
Zech, W., Glaser, B., Abrarnowski, U., Dittman, C., Kubik, P.W. Reconstruction of the Late Quaternary Glaciation of the Macha Khola valley (Gorkha Himal, Nepal) using relative and absolute (14C, 10Be, dendrochronology) dating techniques. Quaternary Science Reviews, 2003, 22: 2253-2265.
Zeitler P K, Meltzer A S, Koons P O et al. Erosion, Himalayan geodynamics, and the geomorphology of metamorphism. GSA Today, 2001, 11 (1): 4-9.
Zhao J. D., Zhou S. Z., et al. ESR dating of glacial tills and glaciations in the Urumqi River headwaters, Tianshan Mountains, China. Quaternary International, 2006, 144: 61-67.
Zhao, H., Moore, G.W.K. On the relationship between Tibetan snow cover, the Tibetan plateau monsoon and the Indian summer monsoon. Geophysical Research Letters. 2004, 31, L14204.
Zheng, B. The influence of Himalayan uplift on the development of Quaternary glaciers. Zietschrift fur Geomorphologle, 1989, 76: 89-115.
Zheng, B., Glacier variation in the monsoon maritime glacial region since the last glaciation on the Qinghai-Xizang (Tibetan) Plateau. In: The Changing Face of East Asia During the Tertiary and Quaternary. Center of Asian Studies, The University of Hong Kong, 1997:103-112.
Zhou, S. Z., J. J. Li, et al. Quaternary glaciation of the Bailang River Valley, Qilian Shan. Quaternary International, 2002, 97/98:103-110.
Zhou, S. Z., Jiao, et al. K. Q.. Geomorphology of the Urumqi River Valley and the uplift of the Tianshan Mountains in Quaternary. Science in China Series D-Earth Sciences, 2002, 45(11): 961-937
Zhou, S. Z., Xu L. B., et al. Geomorphologic evolution and environmental changes in the Shaluli Mountain region during the Quaternary. Chinese Science Bulletin, 2005, 50(1): 52-57.
Zreda,M G, Phillips, F M. Insights into alpine moraine development from cosmogenic ~(36)Cl buildup dating. Geomorphology, 1995, 14: 149-156.
陈吉阳.天山乌鲁木齐河源全新世冰川变化地衣年代学若干问题的初步研究.中国科学(B辑),1988,(1):95-104
陈钦峦,赵维成.从航片上观察点苍山冰川地貌.云南地理环境研究,1997,19(2):66-73
陈诗越,王苏民,金章东等.湖泊沉积物记录的藏中地区2.8Ma以来的环境演变历史.地球化学,2004,33(2):159-164
崔建新,周尚哲.对气候突变的初步认识.河北师范大学学报(自然科学版),2001,(2):264-266.
崔之久,杨建强,易朝路.点苍山大理冰期研究进展.见:中国地理学会地貌与第四纪专业委员会编.地貌-环境-发展.北京:中国环境科学出版社,2004:116-722
崔之久,杨健夫,刘耕年等.中国台湾高山第四纪冰川之确证.科学通报,1999,44(20):2220-2224
崔之久.中国西部冰期划分与依据.冰川冻土,1979,1(2):13-21
邓晓峰,张文敬.唐古拉山各拉丹冬峰东坡第四纪冰川与环境演变.冰川冻土,1992,14(2):153.160
丁仲礼,孙继敏,余志伟等.黄土高原过去130ka来古气候事件年表.科学通报,1998,43(6):567-574
段克勤,姚檀栋,蒲健辰.喜马拉雅山中部过去约300年季风降水变化.第四纪研究,2002,22(3):236-242
冯松,汤懋苍,王冬梅.青藏高原是我国气候变化启动区的新证据.科学通报,1998,(6).
贡嘎山第四纪冰川遗迹及冰期划分 苏珍,施雅风,郑本兴,地球科学进展2002,17(5):639-647
顾功树,陈惠琴,张宏伟.冰川冻土地区对碳同位素形成的影响及14C测年采样方法.冰川冻土,1991,13(1):85-90
季建清,钟大赉,丁林等.雅鲁藏布大峡谷地质成因.地学前缘,1999,6(4):231-235
江德昕,杨惠秋.青海达布逊湖50万年以来气候变化的孢粉学证据.沉积学报,2001,19(1):101-106
蒋复初,吴锡浩,肖华国等.川西高原甘孜黄土地层学.地球学报——中国地质科学院院报,1997,18(4):413-420
焦克勤,Shuji Iwata,姚檀栋等.3.2kaBP以来念青唐古拉山东部则普冰川波动与环境变化.冰川冻土,2005,27(1):74-79
焦克勤,岩田修二.昆仑山垭口、唐古拉山垭口和藏东南地区末次冰期以来的冰川变化.见:姚檀栋,上田丰主编.青藏高原冰川气候与环境.北京:科学出版社,1993:120.129
景民昌,杨革联,孙乃达.末次间冰期-末次冰期柴达木盆地东部气候演化形式.地球科学与环境学报,2004,26(3):83-87
康世昌,秦大河,Mayewski P A等.近200a来珠穆朗玛峰北坡远东绒布冰芯气候记录.冰川冻土,2000,22(3):211-217
况明生,李吉均,赵瑜等.云南省东北部拱王山第四纪冰川遗迹研究.冰川冻土,1997,19(4):366-372
李炳元,王富葆,张青松等.西藏第四纪地质.北京:科学出版社,1983.1-179
李承三,郭令智.康定道孚之冰川地形.地质评论,1939,4(1):1-8
李吉均,冯兆东,周尚哲.横断山第四纪冰川作用遗迹.见:李吉均和苏珍编,横断山冰川.北京:科学出版社,1996:157-173
李吉均,宋明琨,秦大河等.贡嘎山冰川考察.见:中国科学院青藏高原综合科学考察队编著.横断山考察专集(一)——青藏高原研究.昆明:云南人民出版社,1983:140-158
李吉均,郑本兴,杨锡金等.西藏冰川.北京:科学出版社,1986:1-328
李世杰,李树德.青海可可西里地区第四纪冰川与环境.冰川冻土,1992,14(4):316-324
刘天仇.雅鲁藏布江水文特征.地理学报,1999,54(增刊):157-163
罗来兴,杨逸畴.川西滇北地貌形成的探讨.地理集刊(古冰川作用遗迹)1963(5):34-46
潘保田,王建民.末次间冰期以来青藏高原东部季风演化的黄土沉积记录.第四纪研究,1999,(4):330-335
任美锷等.丽江和玉龙山地貌的初步研究.云南大学学报,1957(4):9-18
施雅风,姚檀栋.中低纬度M IS 3b(54-44kaBP)冷期与冰川前进.冰川冻土,2002,24(1):1-9
施雅风,郑本兴,苏珍等.天山托木尔峰-汗腾格里地区第四纪冰期探讨.冰川冻土,1984,6(2):1-14
施雅风,黄茂桓,姚檀栋等编.中国冰川与环境——现在、过去和未来.北京:科学出版社,2000:1-402
史正涛,张世强,周尚哲等.祁连山第四纪冰碛物的ESR测年研究.冰川冻土,2000,22(4):353-357
唐领余,沈才明,孔昭宸,等.青藏高原东部末次冰期最盛期气候的花粉证据.冰川冻土,1998,20:133～140
唐领余,沈才明,廖淦标,等.西藏两个小湖高分辨率的花粉记录.植物学报,1999,41(8):896-902
唐领余,沈才明,廖淦标,等.末次盛冰期以来西藏东南部的气候交化.中国科学D,2004,34(5):436-442.
唐领余,沈才明,廖淦标,等.南亚古季风的演变:西藏高分辨率古气候记录.科学通报,2000,44(18):2004-2007
王二七,陈良忠,陈智.在构造和气候因素制约下的雅鲁藏布江的演化.第四纪研究,2002,22 (4):365-373
王富葆,张厚生.南迦巴峰地区第四纪地质拾零.山地研究,1985,3(4):321-324
王靖泰.天山乌鲁木齐河源的古冰川.冰川冻土,1981,3:57-63
王明龙,胡发德,李钟武等.贡嘎山地区第四纪冰期探讨.见:高生淮,郑远昌编.横断山研究文集.成都:四川科学技术出版社,1989:50-58
王宁练,姚檀栋,Thomp son L G等.全新世早期强降温事件的古里雅冰芯记录证据.科学通报,2002,47(11):818-823
王苏民,薛滨.中更新世以来若尔盖盆地环境演化与黄土高原比较研究.中国科学(D辑),1996,26(4):323-328
王志超.南迦巴瓦峰地区古冰川遗迹概述.山地研究,1984,2(3):216-220
王宗太.天山中段及祁连山东段小冰期以来的冰川及环境.地理学报,1991,46(2):160-168
邬光剑,潘保田,管清玉等.中更新世全球最大冰期与中国沙漠扩张.冰川冻土,2002,24(5):544-549
吴中海,赵希涛,江万等.念青唐古拉山东南麓更新世冰川沉积物年龄测定.冰川冻土,2003,25(3):272-274
吴中海,赵希涛,朱大岗等.念青唐古拉山西布冰川区的冰碛层.地球学报,2002,23(4):343-348
伍光和.祁连山的第四纪冰期问题.见:中国科学院兰州冰川冻土研究所编辑.中国科学院兰州冰川冻土研究所集刊第5号——祁连山冰川变化及利用.北京:科学出版社,1985.116-123
伍光和.祁连山新冰期的初步观察.冰川冻土,1984,6(2):53-60
伍永秋,崔之久,刘耕年等.昆仑山垭口地区的冰期系列.冰川冻土,1999,21(1):71-76
徐道明,沈永平.青藏高原的泛冰盖遗迹与冰期.冰川冻土,1995,17(3):213-229
许刘兵,周尚哲,崔建新等.稻城冰帽区更新世冰川测年研究.冰川冻土,2004,26(5):528-534
阎顺,陈亚宁.西藏南迦巴瓦峰地区第四纪环境探讨.山地研究,1992,10(3):167-171
杨怀仁.岷江峡谷地理之初步观察.地理学报.1946,12:11-29
杨建强,崔之久,易朝路等.云南点苍山全新世以来的冰川湖泊沉积.地理学报,2004,59(4):525-533
杨建强,崔之久 云南点苍山冰川地貌特征水土保持研究2003 10(3):90-94
杨威,周尚哲,王杰,王孝理,孙爱芝,许刘兵,韩海涛.波堆藏布谷地冰碛丘陵形成机制及其环境意义.冰川冻土,2005,(2):220-225.
杨逸畴,李炳元,尹泽生等.西藏地貌.北京:科学出版社,1985:1-266
杨逸畴,高登义,李渤生.雅鲁藏布江下游河谷水汽通道初探.中国科学(B辑),1987,(8):893-902
杨逸畴.记南迦巴瓦峰科学考察.山地研究,1983,1(1):41-47
杨逸畴.徒步穿越考察世界第一大峡谷最新成果.山地学报,1999,17(3):200-206
杨逸畴.再记南迦巴瓦峰科学考察.山地研究,1984,2(1):43-48
杨逸畴.再论南迦巴瓦峰地区的地貌.山地研究,1985,3(4):237-233
姚檀栋,Thomp son L G,施雅风等.古里雅冰芯中末次间冰期以来气候变化记录研究.中国科学(D辑),1997,27(5):447-452
姚檀栋,谢自楚,武筱舲等.敦德冰帽中的小冰期气候记录.中国科学(B辑),1990,20(11):1196.1201
姚檀栋,上田丰,大哲夫等.1989年中日青藏高原冰川联合考察研究.冰川冻土,1991,13(1):1-8
姚檀栋.古里雅冰芯氧同位素地层学.第四纪研究,2000,20(2):165-170
姚小峰,郭正堂,赵希涛.玉龙山东麓古红壤的发现及其对青藏高原抬升的指示意义.科学通报,2000,45(15):1671-1676
易朝路,焦克勤,刘克新等.冰碛物ESR测年与天山乌鲁木齐河源末次冰期系列.冰川冻土,2001,23(4):389-393
易朝路,刘克新,崔之久.天山乌鲁木齐河河源末次冰期以来冰川沉积物AMS测年及其意义.科学通报,1998,43(6):655-656
易朝路,崔之久,熊黑钢.中国第四纪冰期数值年表初步划分.第四纪研究,2005,(5).609-619
易朝路,焦克勤,刘克新等.冰碛物ESR测年与天山乌鲁木齐河源末次冰期系列.冰川冻土,2001,23(4):389-393
易朝路,李孝泽,屈建军.青藏高原现代最大冰原区第四纪冰川作用.冰川冻土,2003,(5):491-497.
余素华,朱照宇,李炳元等.23万年以来青藏高原甜水海湖岩心铁元素的气候记录刍议.海洋地质与第四纪地质,1998,18(3):63-69
张东启,秦大河,侯书贵等.珠穆朗玛峰东绒布80.36m冰芯δ18O记录的气候意义.中国科学(D辑),2003,33(3):264-270
张文敬,高登义.世界第一大峡谷——雅鲁藏布大峡谷科学考察新进展.山地学报,1999,17(2):99-103
张文敬.南迦巴瓦峰跃动冰川的某些特征.山地研究,1985,3(4):234-238
张祥松,王宗太.西北冰川变化及其趋势.见:施雅风总主编,刘春蓁,张祥松本卷副主编.中国气候与海面变化及其趋势和影响(4)——气候变化对西北华北水资源的影响.济南:山东科学技术出版社,1995.53-78
张振栓.南迦巴瓦峰西北坡末次冰期以来的冰川变化.冰川冻土,1988,10(2):180-188
赵井东,周尚哲,史正涛等.祁连山东段冷龙岭南麓白水河冰碛物ESR测年研究.兰州大学学报(自然科学版),2001,37(4):110-117
赵井东,周尚哲,崔建新,焦克勤,业渝光,许刘兵.乌鲁木齐河源冰碛物的ESR测年研究.冰川冻土,2002,(6):737-743.
赵井东,周尚哲,崔建新,潘小多,许刘兵,张小伟.摆浪河流域的ESR年代学与祁连山第四纪冰期新认识.山地学报,2001,(6):481-488
赵希涛,曲永新,李铁松.玉龙山东麓更新世冰川作用.冰川冻土,1999,21(3):242-248
赵希涛,吴中海,朱大岗等.念青唐古拉山脉西段第四纪冰川作用.第四纪研究,2002,22(5):424-433.
郑本兴,焦克勤,李世杰等.西昆仑山第四纪冰川与环境变化.见:中国第四纪冰川研究中心编.中国西部第四纪冰川与环境.北京:科学出版社,1991:15-23
郑本兴,李世杰,王苏民.若尔盖盆地周围高山第四纪冰川演变历史.见:青藏项目专家委员会编著.青藏高原形成演化、环境变迁与生态系统研究.北京:科学出版社,1995:218-226
郑本兴,马秋华.贡嘎山地区全新世的冰川变化、气候变化与河谷阶地发育.地理学报,1994,49(6):500-508
郑本兴,施雅风.珠穆朗玛峰地区第四纪冰期探讨.见:中国科学院西藏科学考察队编著.珠穆朗玛峰地区科学考察报告(1966-1968):第四纪地质.北京:科学出版社,1976:29-62
郑本兴.贡嘎山东麓第四纪冰川作用与磨西台地成因探讨.冰川冻土,2001,23(3):283-291
郑本兴.云南玉龙雪山第四纪冰期与冰川演化模式.冰川冻土,2000,22(1):53-61
中国科学院青藏高原综合科学考察队编.西藏冰川.北京:科学出版社,1986.117:217-222,226-230,313-327
周尚哲,易朝路,施雅风等.中国西部M IS 12冰期研究.地质力学学报,2001,7(4):321-327
周尚哲,焦克勤,赵井东,张世强,崔建新,许刘兵.乌鲁木齐河河谷地貌与天山第四纪抬升研究.中国科学D辑,2002,(2):157-162.
周尚哲,李吉均,潘保田,张叶春.黄河源区更新世冰盖初步研究.地理学报,1994,(1):64-72.
周尚哲,李吉均.冰期之青藏高原新研究.地学前缘,2001,(1):67-75.
周尚哲,李吉均.第四纪冰川测年研究新进展.冰川冻土,2003,(6):660-660.
周尚哲,许刘兵,崔建新,张小伟,赵井东.沙鲁里山第四纪地貌发育与环境演变.科学通报,2004,(23):660-666.
周尚哲.巴颜喀拉山第四纪冰川序列.冰川冻土,1995,(3):230-240.
Augustin L.et al., Eight glacial cycles from an Antarctic ice core. Nature 2004;429 (6992):623-8.
Bamard, P. L., L. A. Owen, et al. Quaternary fans and terraces in the Khumbu Himal south of Mount Everest: their characteristics, age and formation. Journal of the Geological Society, 2006, 163: 383-399.
Barnard, P.L., Owen, L.A., Finkel, R.C. Style and timing of glacial and paraglacial sedimentation in a monsoonal influenced high Himalayan environment, the upper Bhagirathi Valley, Garhwal Himalaya. Sedimentary Geology, 2004a, 165:199-221.
Barnard, P.L., Owen, L.A., Sharma, M.C., Finkel, R.C. Late Quaternary landscape evolution of a monsoon-influenced high Himalayan valley, Gori Ganga, Nanda Devi, NE Garhwal. Geomorphology, 2004b, 61: 91-110.
Barrows, T. T., Stone, J. O., Fifield, L. K., et al. Late Pleistocence glaciation of the Kosciuszko Massif, Snowy Mountains, Australia. Quaternary Research, 2001, 55:179-189.
Ben W.M. Richards et al. Timing of Late Quaternary glaciations in the Himalayas of northern Pakistan. Journal of Quaternary Science, 2000, 15 (3):283-297.
Benn, D.I., Lehmkuhi, F. Mass balance and equilibrium-line altitudes of glaciers in high mountain environments. Quaternary International, 2000, 65/66:15-29.
Benn, D.I., Owen, L.A. Himalayan glacial sedimentary environments: a framework for reconstructing and dating former glacial extents in high mountain regions. Quaternary International, 2002, 97-98: 3-26.
Benn, D.I., Owen, L.A. The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation: review and speculative discussion. Journal of the Geological Society, 1998,155:353-363.
Benn, D.I., Owen, L.A., Osmaston, H.A., Seltzer, G.O., Porter, S.C., Mark, B. Reconstruction of equilibrium-line altitudes for tropical and sub-tropical glaciers. Quaternary International, 2005,138:8-21.
Berger, A., Loutre, M.F. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews, 1991,10:297-317.
Bierman, P R, Marsella, K A, Patterson, C, et al. M id-Pleistocene cosmogenic minimum-age limits for pre-W isconsinan glacial surfaces in southwestern Minnesota and southern Baffin Island: a multiple nuclide approach. Geomorphology, 1999, 27: 25-39.
Bierman, P R. Using in situ produced cosmogenic isotopes to estimate rates of landscape evoluation: A review from the geomorphic perspective. Journal of Geophysical Research, 1994, 99 (B7):13885-13896.
Bohner, J. and F. Lehmkuhl. Environmental change modelling for Central and High Asia: Pleistocene, present and future scenarios. Boreas, 2005, 34(2): 220-231.
Bose, M., Hirakawa, K., Matsuoka, N., Sawagaki, T. Glaciation and periglaciation in Asian high Mountains. Zeitsehriftfur Geomorphologie, 2003 (Eds.), 130, 276pp.
Briner, J P, Swanson, T W. Late Pleistocene cosmogenic 36Cl glacial chronology of the Southwestern Ahklun Mountains. Alaska. Quaternary Research, 2001, 56:148-154.
Briner, J P, Swanson, T W. U sing inherited cosmogenic 36Cl to const rain glacial erosion rates of the Cordilleran ice sheet. Geology, 1998, 26:3-6.
Brown E T, Trull T W, Jean-Baptiste P, ct al. Determination of cosmogenic production rates of 10 Be, 3He and 3H in water. Nucl Instr Methods Phys Res, 2000, 172B: 873-883.
Bush, A. B. G. Modelling of late Quaternary climate over Asia: a synthesis. Boreas, 2004, 33(2): 155-163.
Bush, A.B.G. A comparison of simulated monsoon circulations and snow accumulation in Asia during the mid-Holocene and at the Last Glacial Maximum. Global and Planetary Change, 2002, 32:331-347.
Bush, A.B.G. A comparison of simulated monsoon circulations and snow accumulation in Asia during the mid-Holocene and at the Last Glacial Maximum. Global and Planetary Change, 2002, 32:331-347.
Bush, A.B.G. A positive climatic feedback mechanism for Himalayan glaciation. Quaternary International, 2000, 65/66: 3-13.
Ceding T E, Craig H. Cosmogenic 3He production rates from 39°N to 46°N latitude, western USA and France. Geochim Cosmochim Acta, 1994, 58 : 249-255.
Clark,D H,Bierman, P, Gillespie,A R. 10Be and 26Al product ion rates and a revised glacial chronology for the Sierra Nevada. Radiocarbon, 1996, 38 (1): 152.
Dep,L , Elmore, D,Lipschutz, M , et al. Depth dependence of cosmogenic neutron capture produced 36Cl in a terrestrial rock. Nuclear Instruments and Methods in Physics Research B, 1994b, 92:301-307.
Derbyshire, E. Glacier regime and glacial sediment facies: a hypothetical framework for the Qinghai-Xizang Plateau. In: Proceedings of the Symposium on Qinghai-Xizang (Tibet) Plateau, Beijing China. Vol. 2—Geological and Ecological Studies of Qinghal-Xizangf Plateau. Science Press, Beijing. 1981: 1649-1656.
Derbyshire, E. Quaternary glacial sediments, glaciation style, climate and uplift in the Karakoram and northwest Himalaya: Review and speculations. Palaeogeography Palaeoclimatology Palaeoecology ,1996, 120(1-2): 147-157.
Derbyshire, E., Shi, Y., Li, J., Zheng, B., Li, S., Wang, J. Quaternary glaciation of Tibet: the geological evidence. Quaternary Science Reviews. 1991, 10:485-510.
Desilets,D, Zreda, M. On scaling cosmogenic nuclide production rates for altitude and latitude using cosmic-ray measurements. Earth and Planetary Science Letters, 2001, 193: 213-225.
Dey, B., Bhanu Khumar, O.S.R.U. An apparent relationship between Eurasian spring snow cover and the advance period of the Indian summer monsoon. Journal of Applied Meteorology, 1982, 21:1923-1929.
Dey, B., Kathuria, S.N., Bhanu Khumar, O.S.R.U. Himalayan snow cover and withdrawal of the Indian summer monsoon. Journal of Climatology and Applied Meteorology, 1985, 24: 865-868.
Dickson, R.R. Eurasian snow cover versus Indian monsoon rainfall—an extension of the Hahn-Shukla results. Journal of Climatology and Applied Meteorology, 1984, 23: 171-173.
Dunai, T J. Sealing factors for product ion rates of in situ produced eosmogenie nuclides: a critical reevaluation. Earth and Planetary Science Letters, 2000, 176: 157-169.
Dyke AS, Andrews JT, Clark PU, England JH, Miller GH, Shaw J, Veillette JJ. The Laurentide and Innuitian ice sheets during the Last Glacial Maximum. Quaternary Science Reviews 2002;21 (1-3):9-31.
Easterbrook, D.J., Pierce, K., Gosse, J.C., Gillespie, A., Evenson, E.B., Hamblin, K. Quaternary geology of the western United States. In: Easterbrook, DJ. (Ed.), Quaternary Geology of the United States. Geological Society of America, Denver, 2003:19-80.
Fabel,D, Harbor, J. The use of in situ produced cosmogenic radionuclides in glaciology and glacial geomorphology.Annals of Glaciology, 1999,28: 103-110.
Fabel,D, St roeven,A P,Harbo r, J. Landscape preservat ion under Fennoscandian ice sheets determined from in situ produced 10Be and 26A1. Earth and Planetary Science Letters, 2002,201:397-406.
Finkel, R.C., Owen, L.A., Barnard, P.L., Caffee, M.W. Beryllium-10 dating of Mount Everest moraines indicates a strong monsoonal influence and glacial synchroneity throughout the Himalaya. Geology, 2003,31:561-564.
Fushimi H. Glaciations in the Khumbu Himal (2). Seppyo, 1978,40: 71-77.
Gasse F, Vancampo E. Abrupt Postglacial Climate Events in West Asia and North-Africa Monsoon Domains. Earth and Planetary Science Letters 1994;126 (4):435-56.
Gibbons, A.B., Megeath, J.D., Pierce, K.L. Probability of moraine survival in a succession of glacial advances. Geology, 1984,12, 327-330.
Gillesp ie A, Molnar P. Asynchronous maximum advances of Mountain and continental glacials. Review of Geophysics, 1995, 33(3): 311-364.
Gillespie,A R, Bierman, P R. Precision of terrestrial exposure ages and erosion rates estimated from analysis of cosmogenic isotopes produced in situ. Journal of Geophysical Research, 1995, 100 (B12):24637-24649.
Gosse, J C, Klein, J , Evenson, et al. Beryllium - 10 dating of the duration and retreat of the Last Pinedale Glacial sequence. Science, 1995,268:1329-1333.
Gosse, J C, Phillip s, F M. Terrestrial cosmogenic nuclides: theory and applications. Quaternary Sciences Review, 2001,20:1475-1560.
Gosse, J.C., Evenson, E.B., Klein, J., Lawn, B., Middleton, R. Precise cosmogenic 10Be measurements in western North America: support for a global younger Dryas cooling event. Geology, 1995a, 23: 877-880.
Gosse, J.C., Klein, J., Evenson, E.B., Lawn, B., Middleton, R. Beryllium-10 dating of the duration and retreat of the Last Pinedale glacial sequence. Science, 1995b, 268:1329-1333.
Gosse, J.C., Phillips, F.M. Terrestrial in situ cosmogenic nuclides: theory and application. Quaternary Science Reviews, 2001,20:1475-1560.
Granger DE, Muzikar PF. Dating sediment burial with in situ-produced cosmogenic nuclides: theory, techniques, and limitations. Earth and Planetary Science Letters 2001;188(1-2):269-81.
Hahn, D.G, Shukla, J. An apparent relationship between Eurasian snow cover and Indian monsoon rainfall. Journal of Atmospheric Science, 1976, 33: 2461-2462.
Hallet,B, Putkonen, J. Surface dating of dynamic landforms: young boulders and aging moraines. Science, 1994,265:937- 940.
Heisinger,B, Nolte, E. Cosmogenic in situ product ion of radionuclides: exposure ages and erosion rates. Nuclear Instruments and Methods in Physics Research B, 2000,172:790-795.
Kaulback R. A journey in t he Salween and Tsangpo Basins ,Sout h Eastern Tibet [J ] . Geogr . Jour., 1938,91 (2) : 96-98.
Kodrau, O.D. Climatic Atlas of Asia. World Meteorological Organisation (UNESCO), Geneva, 1981.
Kohl, C.P., Nishiizumi, K. Chemical isolation of quartz for measurement of in-situ produced cosmogenic nuclides. Geochimica et Cosmochimica Acta, 1992,56:3583-3587.
Kuhle, M. Geomorphological findings on the built-up of Pleistocene glaciation in Southern Tibet and on the problem of inland ice. GeoJournal, 1988,17: 457-512.
Kuhle, M. Glacial isostatic uplift of Tibet as a consequence of a former ice sheet. GeoJournal, 1995,37:431-449.
Kuhle, M. Glaciation Research in the Himalayas: a new ice age theory. Universitas, 1985, 27:281-294.
Kuhle, M. Observations supporting the Pleistocene inland glaciation of High Asia. GeoJournal, 1991,25:131-231.
Kukla, G and V. Cilek. Plio-pleistocene megacycles: Record of climate and tectonics. Palaeogeography Palaeoclimatology Palaeoecology, 1996,120(1-2): 171-194.
Kurz M D. In situ production of terrestrial cosmogenic helium and some applications to geochronology. Geochim Cosmochim Acta, 1986,50 :2855-2862.
Lal D. Cosmogenic nuclide production rate systematics in terrestrial materials: present knowledge, needs and future actions for improvement. Nucl Instr Methods Phys Res, 2000, 172B: 772-781.
Lal, D. Cosmic ray labeling of erosion surfaces: in situ nuclide product ion rates and erosion models. Earth and Planetary Science Letters, 1991,104:424-439.
Lal, D., Peters, B. Cosmic ray produced radioactivity on the Earth. In: Flugge, S. (Ed.), Handbueh der Physik, 1967,46( 12): 551-612.
Lehmkuhl, F. and F. Haselein. Quaternary paleoenvironmental change on the Tibetan Plateau and adjacent areas (Western China and Western Mongolia). Quaternary International, 2000, 65-66:121-145.
Lehmkuhl, F. Late Pleistocene, Late-Glacial and Holocene glacier advances on the Tibetan Plateau. Quaternary International, 1997,38/39:77-83.
Lehmkuhl, F., Klinge, M., Lang, A. Late Quaternary glacier advances, lake level fluctuations and aeolian sedimentation in Southern Tibet. Zeitschrift fu(?)r Geomorphologie, 2002, 126:183-218.
Lehmkuhl, F., M. Klinge, et al. (2000). Late Quaternary aeolian sedimentation in central and south-eastern Tibet. Quaternary International, 2000,68:117-132.
Libby W F, Anderson E C, Arnold J R. Age determination by radiocarbon content: world-wide assay of natural radiocarbon. Science, 1949,109:227-228.
Licciardi JM, Clark PU, Brook EJ, Pierce KL, Kurz MD, Elmore D, Sharma P. Cosmogenic He-3 and Be-10 chronologies of the late Pinedale northern Yellowstone ice cap, Montana, USA. Geology 2001;29 (12):1095-8.
Ma Qiuhua. Geomorphology and Quaternary Glaciations in Naimonanyi Peak Region. Proceeding of Sino - Japanese JointScientiflc Symposium: Tibetan Plateau. 1989,2:41-54.
Masarik J., Reedy P C. Terrestrial cosmogenic2nuclide production systematics calculated from numerical simulations. Earth Planet Sci Lett, 1995,136: 381-395.
McCabe, A. M. and P. U. Clark. Ice-sheet variability around the north Atlantic Ocean during the last deglaciation. Nature, 1998,392(6674): 373-377.
Molnar, P. The rise of the Tibetan plateau: From mantle dynamics to the Indian monsoon. Astronomy & Geophysics, 1997, 38(3): 10-15.
Molnar, P., England, P. Late Cenozoic uplift of mountain ranges and global climatic change: chicken or egg? Nature, 1990,346: 29-34.
Molnar, P., P. England, et al. Mantle Dynamics, Uplift of the Tibetan Plateau, and the Indian Monsoon. Reviews of Geophysics, 1993, 31(4): 357-396.
Montgomery D R, HalletB,Liu Yup ing et al. Evidence for Holocene megafloods down the Tsangpo River gorge, Southeastern Tibet.Quaternary Research, 2004, 62 (2): 201-207.
Moore, J. M. and A. E. Moore. The roles of primary kimberlitic and secondary Dwyka glacial sources in the development of alluvial and marine diamond deposits in Southern Africa. Journal of African Earth Sciences, 2004, 38(2): 115-134.
Nishiizumi K. Cosmogenic production of 7Be and 10 Be in water targets. J Geophys Res, 1996, 101 (B10): 22225-22232.
Nishiizumi, K, Kohl, C P, Arnold, J R, et al. Cosmicray produced ~10Be and ~26A1 in Antarctic rocks: exposure and erosion history. Earth and Planetary Science Letters, 1991,104:440- 454.
Nishiizumi, K, Winterer, E L, Kohl, C P, et al. Cosmic ray product ion rates of ~10Be and ~26A 1 in quartz from glacially polished rocks. Journal of Geophysical Research, 1989,94 (B12):17907-17915.
O'Connor J E, Baker V R. Magnitudes and implications of peak discharges from Glacial Lake Missoula. Geological Society of America Bulletin, 1992,104:179-267.
Overpeck, J. T., B. L. Otto-Bliesner, et al. Paleoclimatic evidence for future ice-sheet instability and rapid sea-level rise. Science, 2006,311(5768): 1747-1750.
Owen L A, Derbyshire E, Fort M. The Quaternary glacial history of the Himalaya. Quaternary Proceedings, 1998,6: 91-120.
Owen L A, Finkel R C, Caffee MW.A note on the extent of glaciation throughout the Himalaya during the global Last Glacial Maximum. Quaternary Science Reviews, 2002, 21 (1-3): 147-157.
Owen L A, Wishart M, Bailey R M, et al. Style and timing of glaciation in Lahul Himalaya, North India: a framework for reconstructing late Quaternary paleoclimatic change in the Western Himalayas. Journal of Quaternary Science, 1997,12: 83-110.
Owen L A., Kamp U, Joel Q. Spencer and Klaus Haserodt. Timing and style of Late Quaternary glaciation in the eastern Hindu Kush, Chitral, northern Pakistan: a review and revision of the glacial chronology based on new optically stimulated luminescence dating.
Quaternary International, 2002,97/98:41-55.
Owen, L A, F inkel, R C, Caffee,M W, et al. Timing of multiple late Quaternary glaciations in the Hunza V alley, Karakoram Mountains, northern Pakistan: defined by cosmogenic radionuclide dating of moraines. GSA Bulletin, 2002,114 (5):593- 604.
Owen, L. A. and D. I. Benn. Equilibrium-line altitudes of the Last Glacial Maximum for the Himalaya and Tibet: an assessment and evaluation of results. Quaternary International, 2005,138: 55-78.
Owen, L. A., H. Z. Ma, et al. The timing and style of Late Quaternary glaciation in the La Ji Mountains, NE Tibet: evidence for restricted glaciation during the latter part of the Last Glacial. Zeitschrift Fur Geomorphologie, 2003,47:263-276.
Owen, L. A., M. W. Caffee, et al. Terrestrial cosmogenic nuclide surface exposure dating of the oldest glacial successions in the Himalayan orogen: Ladakh Range, northern India. Geological Society of America Bulletin, 2006,118(3-4): 383-392.
Owen, L. A., R. C. Finkel, et al. Climatic and topographic controls on the style and timing of Late Quaternary glaciation throughout Tibet and the Himalaya defined by Be-10 cosmogenic radionuclide surface exposure dating. Quaternary Science Reviews, 2005, 24(12-13): 1391-1411.
Owen, L.A., Benn, D.I. Equilibrium-line altitudes of the Last Glacial Maximum for the Himalaya and Tibet: an assessment and evaluation of methods and results. Quaternary International, 2005,138:55-78.
Owen, L.A., Finkel, R.C., Caffee, M.W. A note on the extent of glaciation in the Himalaya during the global Last Glacial Maximum. Quaternary Science Reviews, 2002b, 21:147-157.
Owen, L.A., Finkel, R.C., Caffee, M.W., Gualtieri, L. Timing of multiple glaciations during the Late Quaternary in the Hunza Valley, Karakoram Mountains, Northern Pakistan: defined by cosmogenic radionuclide dating of moraines. Geological Society of America Bulletin, 2002a. 114,593-604.
Owen, L.A., Finkel, R.C., Ma, H., Spencer, J.Q., Derbyshire, E., Barnard, P.L., Caffee, M.W. Timing and style of Late Quaternary glaciations in NE Tibet. Geological Society of America Bulletin, 2003c, 115:1356-1364.
Owen, L.A., Gualtieri, L., Finkel, R.C., Caffee, M.W., Benn, D.I., Sharma, M.C. Cosmogenic radionuclide dating of glacial landforms in the Lahul Himalaya, Northern India: defining the timing of Late Quaternary glaciation. Journal of Quaternary Science, 2001, 16, 555-563.
Owen, L.A., Kamp, U., Spencer, J.Q., Haserodt, K. Timing and style of Late Quaternary glaciation in the eastern Hindu Kush, Chitral, northern Pakistan: a review and revision of the glacial chronology based on new optically stimulated luminescence dating. Quaternary International, 2002c. 97/98:41-56.
Owen, L.A., Lehmkuhl, F. (Eds.) Late Quaternary glaciation and palaeoclimate of the Tibetan Plateau and bordering mountains. Quaternary International, 2000, 65/66:212.
Owen, L.A., Ma, H., Derbyshire, E., Spencer, J.Q., Barnard, P.L., Zeng Yong Nian, Finkel, R.C., Caffee, M.W. The timing and style of Late Quaternary glaciation in the La Ji Mountains, NE Tibet: evidence for restricted glaciation during the latter part of the Last Glacial. Zeitschrift fur Geomorphologie, 2003b, 130: 263-276.
Owen, L.A., Spencer, J.Q., Ma, H., Barnard, P.L., Derbyshire, E., Finkel, R.C., Caffee, M.W., Zeng Yong, N. Timing of Late Quaternary glaciation along the southwestern slopes of the Qilian Shan. Boreas, 2003a, 32:281-291.
Owen, L.A., Teller, J.T., Rutter, N.W. Glaciation and reorganization of Asia's network of drainage. Global and Planetary Change, 2002d, 30:289-374.
Owen, L.A., Zhou, S. (Eds.) Glaciation in Monsoon Asia, Quaternary International, 2002, 97/98:179.
Patrick M.Colgan, Jeffrey S.Munroe,Zhou Shangzhe. Cosmogenic radionuclide evidence for the limited extent of last glacial maximum glaciers in the Tanggula Shan of the central Tibetan Plateau. Quaternary Research, 2006,65(2): 336-339
Phillips, F M, Zreda, M G, Benson, L V, et al. Chronology for Fluctuation in Late Pleistocence Sierra Nevada Glaciers and Lakes. Science, 1996,274: 749- 751.
Phillips, F M, Zreda, M G, Smith, S S, et al. Cosmogenic Chlorine- 36 chronology for glacial deposits at Bloody Canyon, Eastern Sierra Nevada. Science, 1990,248: 1529-1532.
Phillips, W.M., Sloan, V.F., Shroder, J.F., Sharma, P., Clarke, M.L., Rendell, H.M. Asynchronous glaciation at Nanga Parbat, northwestern Himalaya Mountains, Pakistan. Geology, 2000, 28:431-434.
Pollard, D. and S. L. Thompson. Climate and ice-sheet mass balance at the last glacial maximum from the genesis version 2 global climate model. Quaternary Science Reviews, 1997, 16(8): 841-863.
Poreda R J, Cerlingt E. Cosmogenic neon in recent lavas from the western United States. Geophys Res Lett, 1992, 19: 1863-1866.
Prell, W.L., Kutzbach, J.F. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution. Nature, 1992, 360:647-652.
Pu, J.C., Su, Z., Yao, T.D., Xie, Z. C. Mass balance on Xiao Dorigkemadi Glacier and Hailuoguo Glacier. Journal of Glaciology and Geocryology, 1998,12:408-412.
Putkonen, J., Swanson, T. Accuracy of cosmogenic ages for moraines. Quaternary Research, 2003, 59:255-261.
R. V. Joshi, S. N. Rajaguru Quaternary Glaciation and Palaeolithic Sites in the Liddar Valley (Jammu-Kashmir) World Archaeology, 1974,5 (3) :369-379
Richards BWM, Benn DI, Owen LA, Rhodes EJ, Spencer JQ. Timing of late Quaternary laciations south of Mount Everest in the Khumbu Himal, Nepal. Geological Society of America Bulletin 2000;l 12 (10):1621-32.
Richards, B.W., Owen, L.A., Rhodes, E.J. Timing of Late Quaternary glaciations in the Himalayas of northern Pakistan. Journal of Quaternary Science, 2000b, 15:283-297.
Richards, B.W.M., Benn, D.I., Owen, L.A., Rhodes, E.J., Spencer,J.Q. Timing of Late Quaternary glaciations south of Mount Everest in the Khumbu Himal, Nepal. Geological Society of American Bulletin, 2000a, 112:1621-1632.
Rinterknecht VR, Clark PU, Raisbeck GM, Yiou F, Bitinas A, Brook EJ, Marks L, Zelcs V, Lunkka JP, Pavlovskaya IE, Piotrowski JA, Raukas A. The last deglaciation of the southeastern sector of the Scandinavian Ice Sheet. Science 2006;311 (5766): 1449-52.
Licciardi JM, Clark PU, Brook EJ, Elmore D, Sharma P. Variable responses of western US glaciers during the last deglaciation. Geology 2004;32 (1):81-4.
Robert C. Finkel Lewis A. Owen Patrick L. Barnard et al .Beryllium-10 dating of Mount Everest moraines indicates a strong monsoon influence and glacial synchroneity throughout the Himalaya. Geology;2003,31(6):561-564.
Roland Zech. Late Quaternary glacial and climate history of the Pamir Mountains derived from cosmogenic 10Be exposure ages. Quaternary Research, 2005,64:212-220.
Ruddiman, W. F. and J. E. Kutzbach. Plateau Uplift and Climatic-Change. Scientific American, 1991,264(3): 66-&.
Ruddiman, W.F., Kutzbach, J.E. Forcing of Late Cenozoic Northern Hemisphere climate by plateau uplift in southern Asia and the America west. Journal of Geophysical Research, 1989,94:409.
S.Tsukamoto, K.Asahi et al. Time of past glaciations in Kanchenjunga Himal, Nepal by optically stimulated luminescece dating of tills. Quaternary International, 2002,97/98:57-67.
Schafer, J.M., Tschudi, S., Zhao, Z., Wu, X., Ivy-Ochs, S., Wider, R., Baur, H., Kubik, P.W., Schluchter. The limited influence of glaciations in Tibet on global climate over the past 170000 yr. Earth and Planetary Science Letters, 2001, 60/69:1-11.
Seltzer GO. Climatic Interpretation of Alpine Snowline Variations on Millennial Time Scales. Quaternary Research 1994;41 (2): 154-9.
Sharma, M.C., Owen, L.A. Quaternary glacial history of the Garhwal Himalaya, India. Quaternary Science Reviews, 1996,15:335-365.
Shi, Y. Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia. Quaternary International, 2002,97/98:79-91.
Shi, Y., Ge, Y, Xiaodong, L., Bingyuan, L., Tandong, Y. Reconstruction of the 30-40 ka BP enhanced Indian monsoon climate based on geological records from the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 169:69-83.
Shiraiwa T, Watanabe T. Late Quaternary glacial fluctuation in the Langtang Valley, Nepal Himalaya, teconstructed by relative dating methods. Arctic and Alpine Research, 1991,23: 404-416.
Silvio Tschudi, Jorg M. Schafer, Zhizong Zhao et al. Glacial advances in Tibet during the Younger Dryas? Evidence from cosmogenic ~10Be, ~26A1, and ~21Ne. Journal of Asian Earth Sciences, 2003, 22: 301-306.
Sirocko, F., Sarnthein, M., Lange, H., Mayayewski, P.A. Atmospheric summer circulation and coastal upwelling in the Arabian Sea during the Holocene and the Last Glaciation. Quaternary Research, 1991,36:72-93.
Soman, M.K., Slingo, J. Sensitivity of the Asian summer monsoon to aspects of sea-surface-temperature anomalies in the tropical Pacific Ocean. Quarterly Journal of the Royal Meteorological Society, 1997,123:309-336.
Steig, E J ,Wolfe,A P,Miller, G H. Wisconsinan refugia and the glacial history of eastern Baffin Island, Arctic Canadaxoupled evidence from cosmogenic isotopes and lake sediments. Geology, 1998, 26: 835- 838.
Stone, J O. Air pressure and cosmogenic isotope production. Journal of Geophysical Research, 2000, 105 (B10): 23753- 23759.
Stroeven,A P, Fabel,D, Habttestrand, C, et al. A relict landscape in the centre of Fennoscandian glaciation: cosmogenic radionuclide evidence of tors preserved through multip le glacial cycles. Geomorphology, 2002,44:145-154.
Su, Z., Shi, Y. Response of monsoonal temperate glaciers to global warming since the Little Ice Age. Quaternary International, 2002, 97/98:123-131.
Svendsen, J. I., Alexanderson H., et al. Late quaternary ice sheet history of northern Eurasia. Quaternary Science Reviews, 2004,23(11-13): 1229-1271.
Taylor,P.J, Mitchell,W.A., Late Quaternary glacial history of the Zanskar Range, North-west Indian Himalaya. Quaternary International, 2000,65/66:81-100.
Thomp son L G, Yao T, Davis M K et al. Trop ical climate instability: The last glacial cycles from a Qinghai-Tibetan ice core. Science, 1997,276:1821-1825
Thompson, L.G, Thompson, E.M., Davies, M.E., Bolzn, J.F., Dai, J., Gunderstrup, N., Wu, X., Klein, L., Xie, Z. Holocene-Late Pleistocene climatic ice core records from the Qinghai-Tibet Plateau. Science, 1989,246:474-477.
Trinkler.E The ice-age on the Tibetan plateau and in the adjacent regions. The Geogr.J. , 1930, 75(3):225-232.
Tsukamoto, S., Asahi, K., Watanabe, T., Rink, W.J. Timing of past glaciations in Kanchenjunga Himal, Nepal by optically stimulated luminescence dating of tills. Quaternary International, 2002, 97/98: 57-67.
Tsukamoto, S., Asahi, K., Watanabe, T., Rink, W.J. Timing of past glaciations in Kanchenjunga Himal, Nepal by optically stimulated luminescence dating of tills. Quaternary International, 2002, 97/98:57-67.
W. R. Rickmers The Pamir Glaciers Geographical Journal, 1965,131 (2):217-220
W.M. Richards, Douglas I. Benn et al. Timing of late Quaternary glaciations south of Mount Everest in the Khumbu Himal, Nepal. Ben GSA Bulletin. 2000, 112(10): 1621-1632.
Wake, C.P., Mayewski, P.A., Dahe, Q., Qinzhao, Y., Sichang, K., Whitlow, S., Meeker, L.D. Changes in atmospheric circulation over the south-eastern Tibetan Plateau over the last two centuries from a Himalayan ice core. PAGES News, 2001, 9:14-16.
Wang, Y. J., H. Cheng, et al. A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China. Science, 2001, 294(5550): 2345-2348.
William M. Phillips, Valerie F. Sloan et al. Asynchronous glaciation at Nanga Parbat, northwestern Himalaya Mountains, Pakistan. Geology;2000, 28(5): 431-434.
Winograd, I.J., Landwehr, J.M., Ludwig, K.R., Coplen, T.B., Riggs, A.C. Duration and structure of the past four interglacials. Quaternary Research, 1997, 48:141-154.
Winograd, I.J., Landwehr, J.M., Ludwig, K.R., Coplen, T.B., Riggs, A.C. Duration and structure of the past four interglacials. Quaternary Research, 1997,48:141-154.
Wissmann.h.von. The Pleistocene glaciation in China. Bull. Geol. Sol. China, 1937, 5:3-6.
Wu Yongqiu, Cui Zhijiu, Liu Gengnian et al. Quaternary geomorphological actions evolution of the Kunlun Pass area and up lift of the Qinghai2Xizang (Tibet) Plateau. Geomorphology, 2001, 36(3-4): 203-216.
Yi Chaolu, J iao Keqin, Liu Kexin et al. ESR Dating of the sediments of the Last Glaciation at the source area of the Brümqi River, Tian Shan Mountains, China. Quaternary International, 2002, 97/98: 141-146.
Yi Chaolu, Liu Kexin, Cui Zhijiu et al. AMS radiocarbon dating of Late Quaternary glacial landforms, source of the Brümqi River, Tien Shan—A pilot study of 14C dating on inorganic carbon. Quaternary International, 2004, 121 (1) : 99-107.
Yi, C., Li, X., Qu, J. Quaternary glaciation of Puruogangri-the largest modern ice field in Tibet. Quaternary International, 2002, 97/98:111-123.
Yu, Y. T., Yang T. B., et al. (). Millermial-scale Holocene climate variability in the NW China drylands and links to the tropical Pacific and the North Atlantic. Palaeogeography Palaeoclimatology Palaeoecology, 2006, 233(1-2): 149-162.
Zech R., Abramowski U., et al. Late Quaternary glacial and climate history of the Pamir Mountains derived from cosmogenic Be-10 exposure ages. Quaternary Research, 2005, 64(2): 212-220.
Zech, W., Glaser, B., Abrarnowski, U., Dittman, C., Kubik, P.W. Reconstruction of the Late Quaternary Glaciation of the Macha Khola valley (Gorkha Himal, Nepal) using relative and absolute (14C, 10Be, dendrochronology) dating techniques. Quaternary Science Reviews, 2003, 22: 2253-2265.
Zeitler P K, Meltzer A S, Koons P O et al. Erosion, Himalayan geodynamics, and the geomorphology of metamorphism. GSA Today, 2001, 11 (1): 4-9.
Zhao J. D., Zhou S. Z., et al. ESR dating of glacial tills and glaciations in the Urumqi River headwaters, Tianshan Mountains, China. Quaternary International, 2006, 144: 61-67.
Zhao, H., Moore, G.W.K. On the relationship between Tibetan snow cover, the Tibetan plateau monsoon and the Indian summer monsoon. Geophysical Research Letters. 2004, 31, L14204.
Zheng, B. The influence of Himalayan uplift on the development of Quaternary glaciers. Zietschrift fur Geomorphologle, 1989, 76: 89-115.
Zheng, B., Glacier variation in the monsoon maritime glacial region since the last glaciation on the Qinghai-Xizang (Tibetan) Plateau. In: The Changing Face of East Asia During the Tertiary and Quaternary. Center of Asian Studies, The University of Hong Kong, 1997:103-112.
Zhou, S. Z., J. J. Li, et al. Quaternary glaciation of the Bailang River Valley, Qilian Shan. Quaternary International, 2002, 97/98:103-110.
Zhou, S. Z., Jiao, et al. K. Q.. Geomorphology of the Urumqi River Valley and the uplift of the Tianshan Mountains in Quaternary. Science in China Series D-Earth Sciences, 2002, 45(11): 961-937
Zhou, S. Z., Xu L. B., et al. Geomorphologic evolution and environmental changes in the Shaluli Mountain region during the Quaternary. Chinese Science Bulletin, 2005, 50(1): 52-57.
Zreda,M G, Phillips, F M. Insights into alpine moraine development from cosmogenic ~(36)Cl buildup dating. Geomorphology, 1995, 14: 149-156.
陈吉阳.天山乌鲁木齐河源全新世冰川变化地衣年代学若干问题的初步研究.中国科学(B辑),1988,(1):95-104
陈钦峦,赵维成.从航片上观察点苍山冰川地貌.云南地理环境研究,1997,19(2):66-73
陈诗越,王苏民,金章东等.湖泊沉积物记录的藏中地区2.8Ma以来的环境演变历史.地球化学,2004,33(2):159-164
崔建新,周尚哲.对气候突变的初步认识.河北师范大学学报(自然科学版),2001,(2):264-266.
崔之久,杨建强,易朝路.点苍山大理冰期研究进展.见:中国地理学会地貌与第四纪专业委员会编.地貌-环境-发展.北京:中国环境科学出版社,2004:116-722
崔之久,杨健夫,刘耕年等.中国台湾高山第四纪冰川之确证.科学通报,1999,44(20):2220-2224
崔之久.中国西部冰期划分与依据.冰川冻土,1979,1(2):13-21
邓晓峰,张文敬.唐古拉山各拉丹冬峰东坡第四纪冰川与环境演变.冰川冻土,1992,14(2):153.160
丁仲礼,孙继敏,余志伟等.黄土高原过去130ka来古气候事件年表.科学通报,1998,43(6):567-574
段克勤,姚檀栋,蒲健辰.喜马拉雅山中部过去约300年季风降水变化.第四纪研究,2002,22(3):236-242
冯松,汤懋苍,王冬梅.青藏高原是我国气候变化启动区的新证据.科学通报,1998,(6).
贡嘎山第四纪冰川遗迹及冰期划分 苏珍,施雅风,郑本兴,地球科学进展2002,17(5):639-647
顾功树,陈惠琴,张宏伟.冰川冻土地区对碳同位素形成的影响及14C测年采样方法.冰川冻土,1991,13(1):85-90
季建清,钟大赉,丁林等.雅鲁藏布大峡谷地质成因.地学前缘,1999,6(4):231-235
江德昕,杨惠秋.青海达布逊湖50万年以来气候变化的孢粉学证据.沉积学报,2001,19(1):101-106
蒋复初,吴锡浩,肖华国等.川西高原甘孜黄土地层学.地球学报——中国地质科学院院报,1997,18(4):413-420
焦克勤,Shuji Iwata,姚檀栋等.3.2kaBP以来念青唐古拉山东部则普冰川波动与环境变化.冰川冻土,2005,27(1):74-79
焦克勤,岩田修二.昆仑山垭口、唐古拉山垭口和藏东南地区末次冰期以来的冰川变化.见:姚檀栋,上田丰主编.青藏高原冰川气候与环境.北京:科学出版社,1993:120.129
景民昌,杨革联,孙乃达.末次间冰期-末次冰期柴达木盆地东部气候演化形式.地球科学与环境学报,2004,26(3):83-87
康世昌,秦大河,Mayewski P A等.近200a来珠穆朗玛峰北坡远东绒布冰芯气候记录.冰川冻土,2000,22(3):211-217
况明生,李吉均,赵瑜等.云南省东北部拱王山第四纪冰川遗迹研究.冰川冻土,1997,19(4):366-372
李炳元,王富葆,张青松等.西藏第四纪地质.北京:科学出版社,1983.1-179
李承三,郭令智.康定道孚之冰川地形.地质评论,1939,4(1):1-8
李吉均,冯兆东,周尚哲.横断山第四纪冰川作用遗迹.见:李吉均和苏珍编,横断山冰川.北京:科学出版社,1996:157-173
李吉均,宋明琨,秦大河等.贡嘎山冰川考察.见:中国科学院青藏高原综合科学考察队编著.横断山考察专集(一)——青藏高原研究.昆明:云南人民出版社,1983:140-158
李吉均,郑本兴,杨锡金等.西藏冰川.北京:科学出版社,1986:1-328
李世杰,李树德.青海可可西里地区第四纪冰川与环境.冰川冻土,1992,14(4):316-324
刘天仇.雅鲁藏布江水文特征.地理学报,1999,54(增刊):157-163
罗来兴,杨逸畴.川西滇北地貌形成的探讨.地理集刊(古冰川作用遗迹)1963(5):34-46
潘保田,王建民.末次间冰期以来青藏高原东部季风演化的黄土沉积记录.第四纪研究,1999,(4):330-335
任美锷等.丽江和玉龙山地貌的初步研究.云南大学学报,1957(4):9-18
施雅风,姚檀栋.中低纬度M IS 3b(54-44kaBP)冷期与冰川前进.冰川冻土,2002,24(1):1-9
施雅风,郑本兴,苏珍等.天山托木尔峰-汗腾格里地区第四纪冰期探讨.冰川冻土,1984,6(2):1-14
施雅风,黄茂桓,姚檀栋等编.中国冰川与环境——现在、过去和未来.北京:科学出版社,2000:1-402
史正涛,张世强,周尚哲等.祁连山第四纪冰碛物的ESR测年研究.冰川冻土,2000,22(4):353-357
唐领余,沈才明,孔昭宸,等.青藏高原东部末次冰期最盛期气候的花粉证据.冰川冻土,1998,20:133～140
唐领余,沈才明,廖淦标,等.西藏两个小湖高分辨率的花粉记录.植物学报,1999,41(8):896-902
唐领余,沈才明,廖淦标,等.末次盛冰期以来西藏东南部的气候交化.中国科学D,2004,34(5):436-442.
唐领余,沈才明,廖淦标,等.南亚古季风的演变:西藏高分辨率古气候记录.科学通报,2000,44(18):2004-2007
王二七,陈良忠,陈智.在构造和气候因素制约下的雅鲁藏布江的演化.第四纪研究,2002,22 (4):365-373
王富葆,张厚生.南迦巴峰地区第四纪地质拾零.山地研究,1985,3(4):321-324
王靖泰.天山乌鲁木齐河源的古冰川.冰川冻土,1981,3:57-63
王明龙,胡发德,李钟武等.贡嘎山地区第四纪冰期探讨.见:高生淮,郑远昌编.横断山研究文集.成都:四川科学技术出版社,1989:50-58
王宁练,姚檀栋,Thomp son L G等.全新世早期强降温事件的古里雅冰芯记录证据.科学通报,2002,47(11):818-823
王苏民,薛滨.中更新世以来若尔盖盆地环境演化与黄土高原比较研究.中国科学(D辑),1996,26(4):323-328
王志超.南迦巴瓦峰地区古冰川遗迹概述.山地研究,1984,2(3):216-220
王宗太.天山中段及祁连山东段小冰期以来的冰川及环境.地理学报,1991,46(2):160-168
邬光剑,潘保田,管清玉等.中更新世全球最大冰期与中国沙漠扩张.冰川冻土,2002,24(5):544-549
吴中海,赵希涛,江万等.念青唐古拉山东南麓更新世冰川沉积物年龄测定.冰川冻土,2003,25(3):272-274
吴中海,赵希涛,朱大岗等.念青唐古拉山西布冰川区的冰碛层.地球学报,2002,23(4):343-348
伍光和.祁连山的第四纪冰期问题.见:中国科学院兰州冰川冻土研究所编辑.中国科学院兰州冰川冻土研究所集刊第5号——祁连山冰川变化及利用.北京:科学出版社,1985.116-123
伍光和.祁连山新冰期的初步观察.冰川冻土,1984,6(2):53-60
伍永秋,崔之久,刘耕年等.昆仑山垭口地区的冰期系列.冰川冻土,1999,21(1):71-76
徐道明,沈永平.青藏高原的泛冰盖遗迹与冰期.冰川冻土,1995,17(3):213-229
许刘兵,周尚哲,崔建新等.稻城冰帽区更新世冰川测年研究.冰川冻土,2004,26(5):528-534
阎顺,陈亚宁.西藏南迦巴瓦峰地区第四纪环境探讨.山地研究,1992,10(3):167-171
杨怀仁.岷江峡谷地理之初步观察.地理学报.1946,12:11-29
杨建强,崔之久,易朝路等.云南点苍山全新世以来的冰川湖泊沉积.地理学报,2004,59(4):525-533
杨建强,崔之久 云南点苍山冰川地貌特征水土保持研究2003 10(3):90-94
杨威,周尚哲,王杰,王孝理,孙爱芝,许刘兵,韩海涛.波堆藏布谷地冰碛丘陵形成机制及其环境意义.冰川冻土,2005,(2):220-225.
杨逸畴,李炳元,尹泽生等.西藏地貌.北京:科学出版社,1985:1-266
杨逸畴,高登义,李渤生.雅鲁藏布江下游河谷水汽通道初探.中国科学(B辑),1987,(8):893-902
杨逸畴.记南迦巴瓦峰科学考察.山地研究,1983,1(1):41-47
杨逸畴.徒步穿越考察世界第一大峡谷最新成果.山地学报,1999,17(3):200-206
杨逸畴.再记南迦巴瓦峰科学考察.山地研究,1984,2(1):43-48
杨逸畴.再论南迦巴瓦峰地区的地貌.山地研究,1985,3(4):237-233
姚檀栋,Thomp son L G,施雅风等.古里雅冰芯中末次间冰期以来气候变化记录研究.中国科学(D辑),1997,27(5):447-452
姚檀栋,谢自楚,武筱舲等.敦德冰帽中的小冰期气候记录.中国科学(B辑),1990,20(11):1196.1201
姚檀栋,上田丰,大哲夫等.1989年中日青藏高原冰川联合考察研究.冰川冻土,1991,13(1):1-8
姚檀栋.古里雅冰芯氧同位素地层学.第四纪研究,2000,20(2):165-170
姚小峰,郭正堂,赵希涛.玉龙山东麓古红壤的发现及其对青藏高原抬升的指示意义.科学通报,2000,45(15):1671-1676
易朝路,焦克勤,刘克新等.冰碛物ESR测年与天山乌鲁木齐河源末次冰期系列.冰川冻土,2001,23(4):389-393
易朝路,刘克新,崔之久.天山乌鲁木齐河河源末次冰期以来冰川沉积物AMS测年及其意义.科学通报,1998,43(6):655-656
易朝路,崔之久,熊黑钢.中国第四纪冰期数值年表初步划分.第四纪研究,2005,(5).609-619
易朝路,焦克勤,刘克新等.冰碛物ESR测年与天山乌鲁木齐河源末次冰期系列.冰川冻土,2001,23(4):389-393
易朝路,李孝泽,屈建军.青藏高原现代最大冰原区第四纪冰川作用.冰川冻土,2003,(5):491-497.
余素华,朱照宇,李炳元等.23万年以来青藏高原甜水海湖岩心铁元素的气候记录刍议.海洋地质与第四纪地质,1998,18(3):63-69
张东启,秦大河,侯书贵等.珠穆朗玛峰东绒布80.36m冰芯δ18O记录的气候意义.中国科学(D辑),2003,33(3):264-270
张文敬,高登义.世界第一大峡谷——雅鲁藏布大峡谷科学考察新进展.山地学报,1999,17(2):99-103
张文敬.南迦巴瓦峰跃动冰川的某些特征.山地研究,1985,3(4):234-238
张祥松,王宗太.西北冰川变化及其趋势.见:施雅风总主编,刘春蓁,张祥松本卷副主编.中国气候与海面变化及其趋势和影响(4)——气候变化对西北华北水资源的影响.济南:山东科学技术出版社,1995.53-78
张振栓.南迦巴瓦峰西北坡末次冰期以来的冰川变化.冰川冻土,1988,10(2):180-188
赵井东,周尚哲,史正涛等.祁连山东段冷龙岭南麓白水河冰碛物ESR测年研究.兰州大学学报(自然科学版),2001,37(4):110-117
赵井东,周尚哲,崔建新,焦克勤,业渝光,许刘兵.乌鲁木齐河源冰碛物的ESR测年研究.冰川冻土,2002,(6):737-743.
赵井东,周尚哲,崔建新,潘小多,许刘兵,张小伟.摆浪河流域的ESR年代学与祁连山第四纪冰期新认识.山地学报,2001,(6):481-488
赵希涛,曲永新,李铁松.玉龙山东麓更新世冰川作用.冰川冻土,1999,21(3):242-248
赵希涛,吴中海,朱大岗等.念青唐古拉山脉西段第四纪冰川作用.第四纪研究,2002,22(5):424-433.
郑本兴,焦克勤,李世杰等.西昆仑山第四纪冰川与环境变化.见:中国第四纪冰川研究中心编.中国西部第四纪冰川与环境.北京:科学出版社,1991:15-23
郑本兴,李世杰,王苏民.若尔盖盆地周围高山第四纪冰川演变历史.见:青藏项目专家委员会编著.青藏高原形成演化、环境变迁与生态系统研究.北京:科学出版社,1995:218-226
郑本兴,马秋华.贡嘎山地区全新世的冰川变化、气候变化与河谷阶地发育.地理学报,1994,49(6):500-508
郑本兴,施雅风.珠穆朗玛峰地区第四纪冰期探讨.见:中国科学院西藏科学考察队编著.珠穆朗玛峰地区科学考察报告(1966-1968):第四纪地质.北京:科学出版社,1976:29-62
郑本兴.贡嘎山东麓第四纪冰川作用与磨西台地成因探讨.冰川冻土,2001,23(3):283-291
郑本兴.云南玉龙雪山第四纪冰期与冰川演化模式.冰川冻土,2000,22(1):53-61
中国科学院青藏高原综合科学考察队编.西藏冰川.北京:科学出版社,1986.117:217-222,226-230,313-327
周尚哲,易朝路,施雅风等.中国西部M IS 12冰期研究.地质力学学报,2001,7(4):321-327
周尚哲,焦克勤,赵井东,张世强,崔建新,许刘兵.乌鲁木齐河河谷地貌与天山第四纪抬升研究.中国科学D辑,2002,(2):157-162.
周尚哲,李吉均,潘保田,张叶春.黄河源区更新世冰盖初步研究.地理学报,1994,(1):64-72.
周尚哲,李吉均.冰期之青藏高原新研究.地学前缘,2001,(1):67-75.
周尚哲,李吉均.第四纪冰川测年研究新进展.冰川冻土,2003,(6):660-660.
周尚哲,许刘兵,崔建新,张小伟,赵井东.沙鲁里山第四纪地貌发育与环境演变.科学通报,2004,(23):660-666.
周尚哲.巴颜喀拉山第四纪冰川序列.冰川冻土,1995,(3):230-240.