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Titlebook: Lakes of Mongolia; Geomorphology, Geoch Alexander Orkhonselenge,Munkhjargal Uuganzaya,Tuya Book 2022 The Editor(s) (if applicable) and The

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Lake Studies in Mongolia: An Overviewia were studied in the context of physical geography. Physiographic conditions and geneses of lakes were presented with documentation of their geographical locations, and evolutionary history and paleogeography of lake basins were hypothesized based on paleoterraces and paleoshorelines. In the early
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Formation and Evolution of Lakes in Mongolia lake formation in Mongolia. Lakes of Mongolia began to form during the early Paleozoic Era. The lake formation of the late Ordovician and Silurian coincided with the presence of a paleooceanic environment. Many lakes formed during the Mesozoic and Cenozoic Eras due to neotectonics, and they evolved
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Genesis of Lakes in Mongoliaearly Paleozoic Era (see Chap. .), lakes of Mongolia have experienced diverse paths of evolution (e.g., dominant presence in the Triassic, maximum sizes in the Cretaceous, decrease in size since the Paleogene, stabilization of existence in the Neogene reaching the present conditions since the late P
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Lake KhukhMongolia for inferring the regional landform evolution and reconstructing the impact of the East Asian Winter Monsoon on the Quaternary climate change over geological time scales. Lake Khukh, the second largest lake in eastern Mongolia, provides valuable surface water resources in the Dornod plain.
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Landscape, Lake Distribution, and Evolution in Southern Mongolialimate changes over geological time scales. In southern Mongolia, the number of lakes is second in the country (24.7%), and they are mainly aeolian, volcanic, and tectonic lakes. Lakes in the Govi are important and useful archives for reconstructing paleoclimate and paleoenvironmental changes in sou
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