摘要
记述了湖的基本特征，讨论了全新世镇江海侵对湖的影响，根据全新世各时期沉积物的分布，阐明了湖湖岸的变化；依据古生物与人类活动遗迹资料，指出湖演化发展可分为３个阶段，即距今１００００ａ～６０００ａ为雏形阶段，距今６０００ａ～２０００ａ为发展阶段，距今２０００ａ以来为现代湖成形阶段。究其成因为新构造活动—河道淤塞—人工改造而成。
Located in the west edge of Yangtze delta, Gehu Lake is a second largest fresh lake in South Jiangsu. The author state the basic features of Gehu Lake and explain the effect of Holocene ingression on Gehu lake. The changes of Gehu Lake have been showed on the basis of the distribution of Holocene sediments. According to the traces of paleontological and Man′s activities, the evolution and development of Gehu Lake fall into three stages:1.Incipient stage of about 10 000a～6 000a ago; 2.Development stage of about 6 000a～2 000a ago; 3.Formation stage of modern Gehu Lake since 2 000a. The origin of Gehu Lake is deduced as neotectonism blocked channel artificial reformation through the survey of strata, geology and tectonics as well as paleontology.
出处
《江苏地质》
1999年第1期30-33,共4页
Jiangsu Geology
