对长江中下游第四纪冰川发育的新认识  

A NEW IDEA TO QUATERNARY GLACIATION IN THE MIDDLE—LOWER REACHES OF THE CHANGJIANG RIVER

作　　者：徐馨[1,2] 沈志达 何才华[3] 

机构地区：[1]南京大学 [2]贵州省地质矿产局 [3]贵州师范大学

出　　处：《贵州师范大学学报（自然科学版）》1999年第1期1-6,共6页Journal of Guizhou Normal University：Natural Sciences

摘　　要：早在２０世纪３０～４０年代，李四光就已开始对我国长江中下游第四纪冰川发育问题进行研究。本文通过对长江中下游在冰期时的古气候、山体高度及雪线高度的研究，认为气候变冷和高山存在是长江中下游第四纪冰川发育最关键的条件。尤其是后者对发育冰川起着积极和直接的作用。In the 1930's ～1940's, Li Siguang, the famous geologist in the world, had made a initial study on development of Quatornary glaciation in the middle-lower reaches of the Changjaing River.Based on the analysis of paleoclimate, heights of snow line and mountains of his area in Quatornary ice age, the paper concludes that the cold weather and the existence of the high moutains are the most important conditions affecting development of quatemary glacier, especially the high mountains energized the glacier's development.

关 键 词：长江 第四纪 冰川 发育 古气候 

分 类 号：P343.6[天文地球—水文科学] P532[天文地球—地球物理学]