摘要
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。
By means of analysis of the archaeological data in the New Stone Age combined with the varieties of thickness of Holoene strata and the crustal deformation data, the present authors expounded the foutures of the subsidence of Taihu plain, and the differential uplifting and sagging movement of the eastern part of the plain, and the activity of the EW trending Fengxian-Nanhui and Kunshan-Jiading fault zones.
出处
《地震学刊》
CSCD
1989年第3期28-33,共6页
Journal of Seismology