[1]杨建强,崔之久.云南点苍山冰川地貌特征[J].水土保持研究,2003,10(03):90-93.
YANG Jian-qiang,CUI Zhi-jiu.Glacial Geomorphology in Diancangshan Mountain in Yunnan Province[J].Research of Soil and Water Conservation,2003,10(03):90-93.
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YANG Jian-qiang,CUI Zhi-jiu.Glacial Geomorphology in Diancangshan Mountain in Yunnan Province[J].Research of Soil and Water Conservation,2003,10(03):90-93.
云南点苍山冰川地貌特征
《水土保持研究》[ISSN:1005-3409/CN:61-1272/P]
卷:
10
期数:
2003年03期
页码:
90-93
栏目:
出版日期:
1900-01-01
- Title:
- Glacial Geomorphology in Diancangshan Mountain in Yunnan Province
- Keywords:
- Diancangshan; Dali Ice Age; glacial geomophology
- 分类号:
- P931.4
- 摘要:
- “大理冰期”的概念被提出以来,其命名地—点苍山的冰川地貌并未经过系统的研究.在对点苍山进行深入细致考察的基础上,基本上确定了冰期发育的规模、范围,统计了各种冰川地貌的数量,并且总结了点苍山冰川地貌的特点,发育比较年轻,断尾冰川,以及冰川发育的多阶段性.
- Abstract:
- In a so long time after the conception of "Dali Ice Age" was put forward,the place where this name came from,Diancangshan,had not been investigated and researched for it’s glacial geomorphology.On the base of thoroughly and particularly field work,the scale,the extension of the glaciaton was confirmed and the number of the glaciers was counted on the whole.The characteristic of the glacier geomorphology was summarized to be very young,tail cut and multi stage.
参考文献/References:
[1] Credner.W,Yannan reise des geographerischer lust der Jun Yatsen University Nitt Geogr,1931,lust sun Yatseh Univ.Bd.1.
[2] H V Wissmann.The Pleistocene glaciation in China[J].Bulletin of the Geological Society of China,1937,145-168.
[3] 陈钦峦,赵维成.从航片上观察点仓山冰川地貌[J].云南地理环境研究,1997,9(2):6673.
[4] S Iwata,H Yagi,et al.Glacial extent and ELAs during the Last Glacial period in Yunnan province,China[A].Proceedings of International Symposium on Paleoenvironmental Change in Tropical-subtropical Monsoon Asia[C].Special Publication,1995(24):113-123.
备注/Memo
收稿日期:2003-4-25。
基金项目:国家自然科学基金(批准号:40071015);云南大理州城建局专项资助.
作者简介:杨建强(1975- ),男,地貌与第四纪地质学专业博士研究生.
更新日期/Last Update:
1900-01-01