通过岩石磁学、磁清洗和剩磁组分分离 ,结合野外地质实际 ,对宁镇山脉湖山地区晚泥盆世五通组、早石炭世高郦山组岩石作了剩磁分析与剩磁年代的探讨 ,确定了三组磁组分 :特征剩磁、印支期和燕山期重磁化组分 .从古地磁偏角数据 ,确认了古生代局部旋转运动的存在 ,并进一步讨论了下扬子板块晚古生代以来的运动学特征和构造演化的若干规律 Through the analysis of rock magnetism, magnetic cleaning and residual magnetism component, combined with the field geological practice, the residual magnetism and residual magnetism of the Late Devonian Wutong Formation and the Early Carboniferous Gaogangshan Formation rocks in Hushan, Ningzhen Mountains were discussed , Three sets of magnetic components were identified: remanent magnetism, Indosinian and Yanshanian remanent magnetization.From the paleomagnetic declination data, the existence of local rotation of the Paleozoic was confirmed, Kinematics and tectonic evolution of a number of laws