摘要
本文首先给出利用航磁异常反演壳内磁化强度的方法和汾渭断陷带壳内磁化强度分布图。以此探讨了汾渭断陷盆地的磁性结构构造与地震活动的关系及其深部地质含义。
At first, the method of inversing apparent magnetic intensity in crust by using aeromagnetic anomaly and the sections of magnetic structure in Fen-Wei downfaulted belt are showed in this paper. Then,based on those information the deep-seated structure and the distribution of magnetic substance in Fen-Wei downfaulted belt,and its relations to the seismicity and its deep-seated geological meaning are discussed.
出处
《中国地震》
CSCD
北大核心
1992年第3期69-73,共5页
Earthquake Research in China
