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- W2365431734 abstract "Lacustrine deposits and two steps of lake terraces are developed in the Pagri area, southern Tibet. Divergent views exist as to the age of terrace II. Thermoluminescence (TL) dating shows that: terrace II formed at 89-58 ka and the terrace I at 4 ka. According to the distribution, characteristics and dating of the lacustrine deposits, the lake development in the Pagri area may fall into three stages: Pagri Lake stage (89-58 ka), overflow lake stage (23-10 ka) and Dogen Co stage (10-2.5ka). Terrace II corresponds to the Pagri Lake stage. The outflow lake stage, which is characterized by tills, occurred in the late glacial interval of the Last Glacial Maximum, when the watershed of the main ridge zone of the Himalayas shifted northward to the location of present Tangla Mountain. During the Dogen Co stage, large alluvial fans (5.7-5.15 ka) and terrace I formed and the lake surface shrank greatly. After 2.5 ka, the lake area in the Pagri area was reduced and desertification occurred in some places of southern Tibet. Then the area displays the present-day appearance." @default.
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- W2365431734 date "2006-01-01" @default.
- W2365431734 modified "2023-09-23" @default.
- W2365431734 title "Late Pleistocene-Holocene lacustrine deposits and paleolake evolution in the Pagri area, Yadong County, southern Tibet, China" @default.
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