De vorming van China’s grote woestijnen: Verantwoording van de geraadpleegde bronnen
Door: Joost Terwindt
Geologische ontwikeling van het Tarim Bekken
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change.
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basin sediments at Oytag (Wuyitake) in the Tarim Basin, (west China).
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Klimaatsverandering en verwoestijning van het Tarim Bekken
Abels, H.A. et al. (2011): Step-wise change of Asian interior climate, preceding the Eocene-Oligocene Transition.
Palaeogeography, Palaeoclimatology, Palaeoecology, 299: 399-412.
Dupont-Nivet, G. et al. (2007): Tibetan plateau aridification linked to global cooling at the Eocene-Oligocene transition.
Nature, 445: 635-638.
Sun, J. et al. (2010): Late Oligocene-Miocene mid-latitude aridification and wind patterns in the Asian interior.
Geology, 38,6:515-518.
Vandenberghe, J. et al. (2006): Penetration of Atlantic westerly winds into Central and East Asia.
Quarternary Science Reviews, 25:2380-2389.
Zeng, H. et al. (2003): Late Neogene loess deposition in the southern Tarim Basin: tectonic and palaeoenvironmental implications.
Tectonophysics, 375:49-59.
Glaciaties
Owen, L. (2009): Latest Pleisocenen and Holocene glacier fluctuations in the Himalaya and Tibet.
Quarternary Science Reviews, 28: 2150-2164.
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Quarternary International 138-139: 55-78.
Seong, Y.B. et al. (2009): Geomorphology of anomalously high glaciated mountains at the northwestern end of Tibet: Muztag Ata and
Kongur Shan.
Geomorphology, 103:227-250.
Stroeven, A.P. et al. (2009): Landscape analysis of the Huang He headwaters, NE Tibetan Plateau-Patterns of glacial and fluvial erosion.
Geomorphology, 103:212-226.
Yang, X. et al. (2004): The evolution of dry lands in northern China and the Republic of Mongolia since the Last Glacial Maximum.
Quarternary International, 118:69-85.
Yang, X, et al. (2006): Late Quarternary environmental changes in the Taklamakan Desert, western China, inferred from OSL-dated
lacustrine and aeolian deposits.
Quarternary Science Reviews, 25:923-932.
Zech, R. (2005): Late Quarternary glacial and climatic history of the Pamir Mountains derived from cosmogenic 10Be exposure ages.
Quarternary Research, 64: 212-220.
Duinen Taklamakan
Dong, Z., Wang, X. & Chen, G. (2000): Monitoring sand dune advance in the Taklamakan Desert.
Geomorphology, 35: 219-231.
Yang, X. and Scuderi, L.A. (2010): Hydrological and climatic changes in deserts of China since the late Pleistocene.
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Yang, X. (2001): The Oases along the Keriya River in the Taklamakan Desert, China, and their evolution since the end of the last glaciation.
Environmental Geology, 41:314-320.
Wang, X. et al.(2004): The evolution of dry lands in northern China and the Republic of Mongolia since the Last Glacial Maximum.
Quarternary International, 118:69-85.
Yang, X. et al. (2002): Geomorphology of sand dunes in the Northeast Taklamakan Desert.
Geomorphology, 42,: 183-195.
Wang, X. et al. (2003): Grain size characteristics of dune sands in the central Taklamakan Sand Sea.
Sedimentary Geology, 161 :1-14.
Wang, X. et al. (2004): Formation of complex linear dunes in the cebtral Taklamakan Sand Sea.
Earth Surface Processes and Landforms, 29:677-686.
Zu, R. et al.(2008): Characteristics of near-surface wind regimes in the Taklamakan Desert, China.
Geomorphology, 96: 39-47.