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关于福建及邻近地区地壳深部场源磁异常的研究
引用本文:任国泰,阎雅芬.关于福建及邻近地区地壳深部场源磁异常的研究[J].地球物理学报,1985,28(6):608-617.
作者姓名:任国泰  阎雅芬
作者单位:中国科学院地球物理研究所
摘    要:本文利用大量实际资料和多项式方法,以全国地磁正常场为背景场,提取反映福建及邻近地区的地壳深部场源磁异常信息;并对它们的空间变化特征,以及与地震带的分布,区域重力场和深部地质构造等的关系进行了对比分析,取得了有用的结果.

关 键 词:磁异常  场源  邻近地区  地壳深部  正异常  零值线  戴云山  负异常  北北东  地壳结构  
收稿时间:1982-11-19

A STUDY ABOUT THE MAGNETIC ANOMALY DUE TO THE SOURCE WITHIN THE DEEPER EARTH'S CRUST IN PROVINCE FUJIAN AND ITS NEAR REGION
BEN GUO-TAI,YAN YA-FEN.A STUDY ABOUT THE MAGNETIC ANOMALY DUE TO THE SOURCE WITHIN THE DEEPER EARTH'S CRUST IN PROVINCE FUJIAN AND ITS NEAR REGION[J].Chinese Journal of Geophysics,1985,28(6):608-617.
Authors:BEN GUO-TAI  YAN YA-FEN
Institution:Institute of Geophysics, Academia Sinica
Abstract:By use of a large amount of data on the earth's surface, we obtained informations which reflect the magnetic anomaly due to. the source within the deeper earth's crust by filter method. We have analysed the features of the anomaly's spatial variation, and compared them with the regional gravity anomaly, distribution of seismic belt and deep geological structure in the earth's crust and obtained useful results.
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