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- W2373607577 abstract "Jiezechaka Lake is located in the northwest part of the lacustrine basin area in the tableland of North Tibet, southwest of the juncture of the Kalakunlun and Kunlun mountains. The lake formed at the link position of Bangong Lake-Nu river and the Hongqilapu-Double river. The altitude of the lake surface is 4 525 m. There is a distinctive perch lake shoreline at 325 m above the lake. From this shoreline to the lake-surface, there occurs a lacustrine deposit terrace and numerous lake shore banks, lake erosion grooves, lake erosion poles and lake erosion mesas which are all well preserved. U system ages of the lacustrine sediments at different altitudes are: (14.2±1.2) ka B.P.(T2)、(38.0±3.5) ka B.P.(T4) and (41.6±3.2) ka B.P.(T5). According the extent of the lake surface descend, it reckons that the forming The age of the Jiezechaka lacustrine sediments is estimated to be about 110 ka~120 ka B.P from the rate the lake surface has descended. Since the Late Pleistocence, the Jiezechaka Lake is a block out evolvement system. The dropping lake level is related to an arid climate and lack of rain. The descent of the lake surface (325 m) is larger than Namucuo Lake (139.2 m). The speed of the descent of the lake surface is approximately 3.31 mm/a. In the initial stages of the Late Pleistocence the lake existed as a high lake surface in the Qingzang Altiplano. About 100 ka B.P, the flooding period of the Qingzang Altiplano gradually ceased from west to east. The climate also changed, becoming dryer from west to east." @default.
- W2373607577 created "2016-06-24" @default.
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- W2373607577 date "2005-01-01" @default.
- W2373607577 modified "2023-09-23" @default.
- W2373607577 title "EVOLUTION OF JIEZECHAKA LAKE AND THE CLIMATIC ENVIRONMENT OF THE LATE PLEISTOCENCE IN NORTHWEST TIBET" @default.
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