Discovery of quaternary glacial evidence of Snow Mountain in Taiwan, China

被引:12
作者
Cui, ZJ [1 ]
Yang, JF
Liu, GG
Wang, X
Song, GC
机构
[1] Peking Univ, Dept Geog, Beijing 100871, Peoples R China
[2] Taiwan Natl Univ, Dept Geog, Taibei, Taiwan
[3] Chenggong Univ, Dept Earth Sci, Tainan, Taiwan
来源
CHINESE SCIENCE BULLETIN | 2000年 / 45卷 / 06期
基金
中国国家自然科学基金;
关键词
Snow Mountain peak; last glaciation; three glacier remains; evidence;
D O I
10.1007/BF02887108
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
There are glacial remains of three different periods on the main peak of Snow Mountain in Taiwan province, including cirque lake, crosswall, polished surface, striation, moraine etc, These three different periods were called, respectively, Shanzhuang ((44.25 +/- 3.72) kaBP), Shuiyuan ((18.26 +/- 1.52) kaBP), and Xueshan glacial stages (the late period of last glaciation). It is characterized by the earlier glacier broad in scale.
引用
收藏
页码:566 / 571
页数:6
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