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- W2350424106 abstract "The research on geomorphological development and palaeo glacier is an important field in geomorphology and quaternary study. Through the detailed field expedition and the analysis of geological and geomorphological profiles, the geomorphological development of the Diancangshan mountain is studied, while the plaeo glaciations of the Luopingshan mountain in Lijiang epoch is probed. The basic conclusions are as follows: 1) The landform of the Diancanghshan mountain is characterized by its multielement, multi-layer and compound features. Its geomorpjological development processes from the mountain top to the foot are: The disintegration process of palaeo plantation surface(3800～4000m); Palaeo glacier and glacier marginal process(3700～3900m); Alluvial action process(2300～3700m);Mixed accumulation process caused by fluvial, debris flow and water flow actions(2100～2300m); Terraces of pediments and lake shore plain action at the mountain foot(1900～2100m). 2) The Diancangshan mountain has developed two-time glaciations which are Dali glacier epoch and Lijiang glacier epoch. They are located at the southernmost limits of the continental glaciers in China.3) Lijiang glacier epoch ever developed on the Luopingshan mountain, which is 800m lower than the Diancangshan mountain, and there a couple of compound mountain glaciers have been found." @default.
- W2350424106 created "2016-06-24" @default.
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- W2350424106 date "2003-01-01" @default.
- W2350424106 modified "2023-09-25" @default.
- W2350424106 title "A STUDY ON GEOMORPHOLOGICAL DEVELOPMENT AND QUATERNARY PALAEO GLACIATION OF THE DIANCANGSHAN-LUOPINGSHAN MOINTAIN IN WESTERNS YUNNAN" @default.
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