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Titlebook: Karst in China; Its Geomorphology an Marjorie M. Sweeting Book 1995 Springer-Verlag Berlin Heidelberg 1995 China.Europe.Geomorphologie.Geom

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The Cone Karsts of Guizhou,y between 1000–2000 m. The plateau extends into the neighbouring provinces of Yunnan, Hunan, Hebei and Sichuan (Fig. 2). It is part of the second great topographic step of China and falls to the E to neighbouring Guangxi. The plateau slopes generally from W to E. It is drained to the N by major trib
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The Karsts of Yunnan,estern sectors of the Yangtse platform with folds generally NE-SW and NNE-SSW. However, from Kunming, the capital of Yunnan, westwards, the structure lines are N-S or NNW-SSE (Figs. 3 and 4). Western Yunnan is the region where the eastern Himalayas and the mountains of Assam and Burma impinge on the
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The Karsts of North China,covered or buried; their outcrops are much more isolated than in S China. Limestones outcrop widely in North China (Fig. 50), though not as continuously as in the south. The most continuous area is in Shanxi province where the Cambro-Ordovician limestones form an extensive plateau, but are covered b
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The Karst of Tibet and Other Parts of Chinese Central Asia,and Figs. 4 and 61). It is almost half the total area of China. Limestones occur over much of this western tectonic megaregion, particularly in Tibet, where about one-fifth of the terrain is karstic (Fig. 1). All this vast area is arid, with an aridity index of one or more (Yuan Daoxian et al. 1991)
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Karst Hydrogeology and Chemical Characteristics of the Karst Water,pter gives a summary review of the karst hydrogeology and the characteristics of the karst waters, particularly in relation to the geomorphology. Both this and the concluding chapter review the contributions of Chinese karst to world karst geomorphology, and its position in general world karst studi
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chaft zu einer Informations-und Wissensgesellschaft: vielmehr findet eine grundlegende Neubewertung der Art und Weise statt, wie wir die Welt und uns selbst sehen und verstehen. Seit der Aufklärung wurde unser Weltbild durch das Projekt der Moderne geformt. Die Kernprämisse dieses Projekts — kontinu
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