中国东南大陆和陆缘地带板内构造界带的地磁异常场响应  

ABNORMAL GEOMAGNETIC FIELD RESPONSE AT INTRAPLATE TECTONIC BOUNDARY IN CONTINENT AND CONTINENTAL MARGIN IN SOUTHEASTERN CHINA

作　　者：滕吉文[1] 闫雅芬[1] 

机构地区：[1]中国科学院地质与地球物理研究所,北京100029

出　　处：《大地构造与成矿学》2004年第2期105-117,共13页Geotectonica et Metallogenia

基　　金：国家自然科学基金项目 ( 4 0 0 740 2 0 );专项基金项目 ( 4 0 2 42 0 0 4)

摘　　要：利用中国东南大陆与陆缘地带的地面磁场观测资料 ,通过适配滤波、谱分析、位场延拓等技术进行数据处理 ,获得了该区的地磁场分布 ;并在网格化数据的基础上进行反演 ,求得了不同深度层面的磁场分布及磁性结构。新的研究结果表明 :1 .扬子、华夏、康滇、秦岭—大别各陆块的磁异常特征无论在水平方向或垂直方向都存在很大差异 ,且具有明显的分区特征。 2 .郯庐深大断裂跨过长江后可能经东西向局部错动继续沿赣江断裂、吴川—四会断裂延伸并潜入海域。 3.扬子与华夏陆块的界带 ,东端起始于杭州湾 ,沿江绍断裂向西南方向延伸 ,经南昌、至长沙 ,再沿雪峰山向南经桂林西并沿钦州湾入海。4 .华南EW向大型隐伏构造带形迹 ,基本沿 2 4 .5°～ 2We used matched filter, spectrum analysis, and continuation methods of potential field for data processing and obtained the geomagnetic field distribution about the continent and continental margin in southeast China. On the basis of grid data, inversion was conducted and magnetic field distribution and magnetic structure on bedding of different depths were obtained. The new results show that: 1. The magnetic field characteristics are largely different in horizontal and vertical directions and it can be divided into zones according to the continental blocks of Yangtze, Cathaysia, Kangdian (Sichuan-Yunnan) and Qinling-Dabie. 2. The Tanlu fault extends southward along the Ganjiang and Wuchuan-Sihui faults after it crossed over the Yangtze River and was offset locally in the east-west direction. The Tanlu fault finally slips into the South China Sea at Hainan Island. 3. The boundary between Yangtze and Cathaysia blocks starts from Hangzhou Bay in the east, extends along Jiangshao fault and passes through Nanchang, Changsha, and Guilin, and finally enters the sea at Qinzhou, Guangxi. 4. The distribution of buried structure zone is located at 24.5°～26° N.

关 键 词：地磁场 陆块 边界场效应 深层过程 板内构造界带 

分 类 号：P318[天文地球—固体地球物理学]