摘要
太湖及其附近地区自晚更新世末期以来,由于内外营力共同作用的结果,经历着一个由沟谷切割的滨海平原景观,演变为蝶形洼地的泻湖地貌形态,其后由于出入口通道的变化,泻湖演变为太湖,并经历面积大小的伸缩演变过程。
In the area around Tai Lake（太湖）, since late Pleistocene epoch（晚更新世）, uue to the endogenetic agent and external agent, a process of the landscape forming from a landscape of gulch-cut littoral plain to a lagoon landscape of papilionaceous depression has been taken place. And then the lagoon had developed into Tai Lake due to the changing of incoming and outcoming watercourse with continuous zooming of its area
出处
《中国历史地理论丛》
CSSCI
北大核心
2009年第1期5-12,共8页
Journal of Chinese Historical Geography
基金
国家自然科学基金项目(40771056)
关键词
太湖
演变
过程
Tai Lake
developing
process
