QUATERNARY GLACIATION SERIES ANDGLACIAL LANDFORM IN GONGWANG MOUNTAINS INNORTHEAST PART OF YUNNAN PROVINCE, CHINA  

作　　者：况明生 

出　　处：《Chinese Geographical Science》1997年第2期180-190,共11页中国地理科学（英文版）

摘　　要：The Gongwang Mountains is situated in the northeast part of Yunnan Plovince. In the mountain, glaciation once occirred above 3100 m a. s. l. in the Quaiernary. The typical glacial remains are mainly concentrated in Jiaozishan - and Yaojingtang - Niudongping area. The glacial landforms were mainly cirque, trough valley and lateral moraine. Glacial type was alpine cirque glacier and according to morphogenetic relation of the glacial landforms, the Quaternary glaciation should be separated into two periods: last glaciation (containing two stages of late and maximum glaciation) and penultimate in the Gongwang Mountain in northeast part of Yunnan Province of China.The Gongwang Mountains is situated in the northeast part of Yunnan Plovince. In the mountain, glaciation once occirred above 3100 m a. s. l. in the Quaiernary. The typical glacial remains are mainly concentrated in Jiaozishan - and Yaojingtang - Niudongping area. The glacial landforms were mainly cirque, trough valley and lateral moraine. Glacial type was alpine cirque glacier and according to morphogenetic relation of the glacial landforms, the Quaternary glaciation should be separated into two periods: last glaciation (containing two stages of late and maximum glaciation) and penultimate in the Gongwang Mountain in northeast part of Yunnan Province of China.

关 键 词：REMAINS of glacier  the QUATERNARY GLACIATION SERIES the Gongwang Mountains  Yunnan Province 

分 类 号：P343.3[天文地球—水文科学]