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作者从新石器时代考古资料分析入手,结合全新世地层厚度变化、水准测量资料等阐述了太湖平原的沉降、太湖平原东部地区的差异沉降活动和奉贤南汇断裂、昆山—嘉定东西向断裂带的活动表现。
Based on the analysis of Neolithic archeological data, the author expounds the sedimentation of the Taihu Lake plain, the differential settlement in the eastern Taihu Lake plain and the activities of Fengxian Nanhui fault and Kunshan-Jiading east-west fault zone in the light of Holocene strata thickness variation and leveling data .