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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
【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。
【Abstract】 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.
- 【文献出处】 安徽地质 ,GEOLOGY OF ANHUI , 编辑部邮箱 ,1999年04期
- 【分类号】P546
- 【被引频次】10
- 【下载频次】106