庐山新构造运动初步研究

本文认为庐山新构造运动活跃。中山低地对照极其鲜明、断层崖悬崖峭壁、温泉地震、谷地形态悬殊、多级裂点瀑布和岬湾曲折湖岸是庐山新构造运动主要迹象;而地垒、地堑、断(?)、掀斜则是主要类型。庐山新构造运动具有运动普遍、继承明显、间歇显著的特征。而且新构造运动经历了轻度—强烈—轻度等断块升降时期,从而控制地貌发育过程。

ELEMENTARY RESEARCH OF THE NEW TECTONIC MOVEMENT OF LU SHAN

The article shows that the new tectonic movement of Lu Shan is very active. The main phenomena are that the middlemountain is instriking contract with the plain; fault-cliffs tower; the valleys differ greatly in form and there are also many hot springs, earthquakes, multistage water falls and knick points, fjords and the winding lake banks. The main types of the new tectonic movement are horsts, grabens, faults and tilted faults. So the new tectonic movement is characterized by its widespread movement, obvious inheritance and evident intermittent. It experienced the stages of weak-strong-weak block-elevation which control the development of the land form.