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- W2390263621 abstract "The Mega Basin is a typical intermountain fault basin constained by the faulting around the basin. The study of the Mega ancient lake shows that the formation, development and collapse of the lake are closely related to those of the Mega Basin. The faulting, northern and southern differential uplifting, palaeoclimatic changes and fluvial erosion from the Holocene onwards resulted in the evolution of the basin according to the (evolutionary) path of river-swamp-river-swamp-lake-swamp-lake-river. The Mega ancient lake has a (total) (thickness) of sediments of 20.5 m and an average depositional rate of more than (2.81 mm/a), which are much higher than those of the middle Pleistocene Lanong Lake in the same area. This implies that for the Mega Basin, the (subsidence) rates during the Holocene are much higher than those during the middle Pleistocene." @default.
- W2390263621 created "2016-06-24" @default.
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- W2390263621 date "2004-01-01" @default.
- W2390263621 modified "2023-09-22" @default.
- W2390263621 title "The formation and evolution of the Mega ancient lake in the middle part of the Gangdise Mountain Ranges, Xizang" @default.
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