摘要
从收集整理勘查资料入手,阐述了区内构造分布特征,总结出地质构造发育的一般规律,即短轴褶曲多为北西向、断层均为北东向正断层,提出了构造形迹形成的机制为局部内应力反弹释放,对今后勘查工作有一定的指导意义。
Based on the collected survey data,elaborated the features of structural distribution,summarized the general rule of geological structural development,that the short axis folds are mostly the NW strike,faults are all normal fault strike NE,put forward the forming mechanism of structural features,which is local internal stress rebound release,having certain guiding significance for future prospecting work.
出处
《吉林地质》
2012年第2期58-60,共3页
Jilin Geology
关键词
褶曲
断层
构造特征
骆驼河子区
珲春煤田
fold
fault
structural features
Luotuohezi area
Hunchun coalfield