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Exposed sediments of 50m thickness were investigated in the 120,000km 2 Qaidam Basin at the northern margin of the Tibetan Plateau. Fine-grained silty sediments constitute most of the section and were accumulated in a lake. Intercalated beds of aeolian sand, and of fluvial or littoral origin, show that the lake experienced periods of desiccation and shallow water levels at the section site...
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