Mega-lakes in the northwestern Tibetan Plateau formed by melting glaciers during the last deglacial
Rapid lake expansions along with intensive glacier loss in the Tibetan Plateau (TP) in recent decades indicate an enhanced hydrological circulation. Well-preserved paleo-shorelines up to ∼200 m above modern levels in the TP attest to much greater lake expansions in the past and serve as analogues fo...
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Published in | Quaternary science reviews Vol. 285; p. 107528 |
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Main Authors | , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.06.2022
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Subjects | |
Online Access | Get full text |
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