合肥及其以东地区新构造运动特征  

THE FEATURES OF NEOTECTONIC MOVEMENT IN HEFEI AND EAST BEYOND

作　　者：许卫[1] 王有生[1] 童劲松[1] 陈秀其[1] 邢润华[1] 

机构地区：[1]安徽地质调查院,安徽合肥230001

出　　处：《安徽地质》1999年第4期250-254,共5页Geology of Anhui

摘　　要：通过对合肥及其以东地区第四纪地层发育特征、地貌特征、地震等特征分析，认为合肥至浮槎山西麓为相对下降区，位于江淮分水岭南缘的梁园一带为现代上升区，浮槎山东部至巢湖一带为相对上升区。新构造运动表现有四次活动。An analysis on the development character,geomorphic feature, seismic signature,etc of the Quaternary strata suggests that the area from Hefei to the west foot of the Fuchachan Mt is a relatively downcast zone,the area around Liangyuan town on the south margin of the Jianghuai watershed a modern upcast zone, and the area from the eastern Fuchashan Mt to Chaohu a relatively upcast zone.The neotectonic movement displays four stages of activity.

关 键 词：第四纪 新构造运动 合肥及其以东地区 

分 类 号：P546[天文地球—构造地质学]