| 皖南青弋江、水阳江地区地貌与新构造运动 |
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| 引用本文： | 严庠生.皖南青弋江、水阳江地区地貌与新构造运动[J].南京晓庄学院学报,1999(4). |
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| 作者姓名： | 严庠生 |
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| 摘 要： | 本地区地貌,主要划分为褶断剥蚀低山、侵入构造剥蚀低山、熔岩构造剥蚀低山、褶断剥蚀丘陵、侵入构造剥蚀丘陵、断陷侵蚀──堆积岗地、沉积平原以及两级夷平面、四级阶地、冲积扇群等多种地貌类型。新构造运动的特点是老构造运动的继承和复活,从南到北以掀外运动为主;其发展趋势是上升运动减弱,沉降运动增强,近代普遍为微弱下降的特点。
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| 关 键 词： | 青弋江 水阳江地区 地貌与新构造运动 |
The Landforms of the Area along the Qingyi River and Shuiyang River and the New Crustal Movement |
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| Yan Yangsheng.The Landforms of the Area along the Qingyi River and Shuiyang River and the New Crustal Movement[J].Journal of Nanjing Xiaozhuang College,1999(4). |
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| Authors: | Yan Yangsheng |
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| Abstract: | The landform of this area mainly belongr to the fow broken folded denudation mountains, low intrusive denudation mountalns, low lava denudahon mountains,brokwn folded denudation hills, intrusive denudation hills, edsd faul hibok accumulation, deposit plains, alluvial plains and so on. Its characteristics is the extension and revival of the old structure of the crustal movement. Taking slanting movement as it major tendency from south to north, the ascending movement is weakening while the diseending movement is shengthening. In modern times, the discending is slight. |
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| Keywords: | area along the Qihgyi River and Shuiyang River landform new crustal movement |
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