摘要
通过确定河北迁安矿区宫店子向形的岩石磁组构,分析了褶皱的磁组构特征,并用磁组构对向形构造做了一些简单的地质解释。
The characteristics of magnetic fabric of fold rocks has been analyed through determining the synform of magnetic fabric of rocks in Gongdianzi mining area, Qian An of Hebei Province. A simple geological interpretaion of synform structure is made by use of the characteristics of magnetic fabric of rocks.
出处
《地震地质》
EI
CSCD
北大核心
1993年第2期167-173,共7页
Seismology and Geology
关键词
磁组构
褶皱
宫店子向形
河北
岩石
Magnetic fabric, Fold, Gongdianzi synform, Hebei Province
