IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
Alternative TitleThe Landforms of the Quaternary Glacial Periods in Western China
刘淑珍; 王明龙
Source Publication横断山研究文集
Publication Place成都
Keyword第四纪冰川 地貌 侵蚀 堆积 横断山区


Other Abstract

The area of western China, in this paper, incude Qing-Xizang plateau and the wide Significant Heng Duan moutains. It's an area of the most all of Quaternary glacial developing period-times, and of the most old traces in China. This paper introduced cmphasizely mant new informations  whick were obtained by author and other researcher in the area Surveying during recent five years, espcially the information of C-14 isotopic ages was most less obtained first in Qinghai-Xizang areas, then progressively develop toward Heng Duan mountains. This late phenomenon of the area Characters have a difference of geological period.
The various glacial periods are divided by fromold to new as follows:
1. Xixiabangma Ice Age (Q~1^1);
2. Nie  Niexiongai Ice Age (Q~2^1);
3. Tilougsi phase in Ximalaya Ice Age (Q~3^1);
4. Rongbusi phase in Ximalaya Ice Age (Q~3^2);
5. Holocene epoch neoglaction  (Q~4^3).
Theactive range of Quaternary old glacids in western China had extended toward South to North at 26°N line.

Document Type专著章节文集论文
Recommended Citation
GB/T 7714
刘淑珍,王明龙. 横断山区第四纪冰川地貌. 横断山研究文集. 成都:四川科学技术出版社,1989:25-49.
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