| 合肥及其以东地区新构造运动特征 |
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| 引用本文： | 许卫,王有生,童劲松,陈秀其,邢润华.合肥及其以东地区新构造运动特征[J].安徽地质,1999(4). |
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| 作者姓名： | 许卫 王有生 童劲松 陈秀其 邢润华 |
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| 作者单位： | 安徽地质调查院!安徽合肥230001 |
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| 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。
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| 关 键 词： | 第四纪 新构造运动 合肥及其以东地区 |
THE FEATURES OF NEOTECTONIC MOVEMENT IN HEFEI AND EAST BEYOND |
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| Xu Wei,Wang Yousheng,Tong Jingsong,Chen Xiuqi,Xing Runhua.THE FEATURES OF NEOTECTONIC MOVEMENT IN HEFEI AND EAST BEYOND[J].Geology of Anhui,1999(4). |
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| Authors: | Xu Wei Wang Yousheng Tong Jingsong Chen Xiuqi Xing Runhua |
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| 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. |
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| Keywords: | Quaternary neotectonic movement Hefei and east beyond |
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